Sample records for gujarat india earthquake

  1. Dewatering Effects from the Gujarat earthquake

    NASA Image and Video Library

    2003-02-05

    On January 26, 2001, when India Republic Day is normally celebrated, a devastating earthquake hit the state of Gujarat. These two false-color images were acquired by NASA Terra spacecraft before and after the event, on January 15 and 31.

  2. India: Gujarat

    Atmospheric Science Data Center

    2013-04-16

    ... Gujarat), and in areas close to the earthquake epicenter.  Research uses the unique capabilities of the Multi-angle Imaging ... Indo-Pakistani border, which were not easily accessible to survey teams on the ground. Changes in reflection at different view angles ...

  3. Wind Resource Assessment of Gujarat (India)

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Draxl, C.; Purkayastha, A.; Parker, Z.

    India is one of the largest wind energy markets in the world. In 1986 Gujarat was the first Indian state to install a wind power project. In February 2013, the installed wind capacity in Gujarat was 3,093 MW. Due to the uncertainty around existing wind energy assessments in India, this analysis uses the Weather Research and Forecasting (WRF) model to simulate the wind at current hub heights for one year to provide more precise estimates of wind resources in Gujarat. The WRF model allows for accurate simulations of winds near the surface and at heights important for wind energy purposes.more » While previous resource assessments published wind power density, we focus on average wind speeds, which can be converted to wind power densities by the user with methods of their choice. The wind resource estimates in this study show regions with average annual wind speeds of more than 8 m/s.« less

  4. East Meets West: An Earthquake in India Helps Hazard Assessment in the Central United States

    USGS Publications Warehouse

    ,

    2002-01-01

    Although geographically distant, the State of Gujarat in India bears many geological similarities to the Mississippi Valley in the Central United States. The Mississippi Valley contains the New Madrid seismic zone that, during the winter of 1811-1812, produced the three largest historical earthquakes ever in the continental United States and remains the most seismically active region east of the Rocky Mountains. Large damaging earthquakes are rare in ‘intraplate’ settings like New Madrid and Gujarat, far from the boundaries of the world’s great tectonic plates. Long-lasting evidence left by these earthquakes is subtle (fig. 1). Thus, each intraplate earthquake provides unique opportunities to make huge advances in our ability to assess and understand the hazards posed by such events.

  5. Seismological evidence for monsoon induced micro to moderate earthquake sequence beneath the 2011 Talala, Saurashtra earthquake, Gujarat, India

    NASA Astrophysics Data System (ADS)

    Singh, A. P.; Mishra, O. P.

    2015-10-01

    In order to understand the processes involved in the genesis of monsoon induced micro to moderate earthquakes after heavy rainfall during the Indian summer monsoon period beneath the 2011 Talala, Saurashtra earthquake (Mw 5.1) source zone, we assimilated 3-D microstructures of the sub-surface rock materials using a data set recorded by the Seismic Network of Gujarat (SeisNetG), India. Crack attributes in terms of crack density (ε), the saturation rate (ξ) and porosity parameter (ψ) were determined from the estimated 3-D sub-surface velocities (Vp, Vs) and Poisson's ratio (σ) structures of the area at varying depths. We distinctly imaged high-ε, high-ξ and low-ψ anomalies at shallow depths, extending up to 9-15 km. We infer that the existence of sub-surface fractured rock matrix connected to the surface from the source zone may have contributed to the changes in differential strain deep down to the crust due to the infiltration of rainwater, which in turn induced micro to moderate earthquake sequence beneath Talala source zone. Infiltration of rainwater during the Indian summer monsoon might have hastened the failure of the rock by perturbing the crustal volume strain of the causative source rock matrix associated with the changes in the seismic moment release beneath the surface. Analyses of crack attributes suggest that the fractured volume of the rock matrix with high porosity and lowered seismic strength beneath the source zone might have considerable influence on the style of fault displacements due to seismo-hydraulic fluid flows. Localized zone of micro-cracks diagnosed within the causative rock matrix connected to the water table and their association with shallow crustal faults might have acted as a conduit for infiltrating the precipitation down to the shallow crustal layers following the fault suction mechanism of pore pressure diffusion, triggering the monsoon induced earthquake sequence beneath the source zone.

  6. High-Resolution Attenuation Model for Gujarat: State of Western India

    NASA Astrophysics Data System (ADS)

    Jaiswal, N.; Singh, C.; Prajapati, S.

    2016-12-01

    In India, Gujarat belongs to the highest seismicity zone other than Himalayan belts. It has suffered from great economic and social loss due to many large magnitude earthquakes in the past. Thus the area needs a special attention from the seismic hazard point of view. It is the state of intraplate earthquakes similar to New Madrid Seismic zone in the United States. In the present study we have prepared a Lg attenuation tomographic model for Gujarat. The study also employs the other complementary information to get a detailed understanding into the mechanisms of attenuation. It will be useful in seismic hazard risk study and in estimating the source parameters of earthquakes. The amplitude of Lg wave is sensitive to different tectonic structures like faults, mountains and ocean basins. It travels predominantly through the continental crust but does not travel across ocean basins. Fifteen earthquakes of Mb >5 recorded at 40 stations operated in the region are chosen for the initial LgQ measurement using the standard two-station method. Finally, 5 events with 70 high-quality inter-station paths are selected from 117 possible pairs that are (1) aligned approximately with the source and (2) separated enough to permit the use of the standard two-station method for LgQ estimation. By using these values of Q0 (1 Hz LgQ) as input, an inversion is performed to have a Lg Q model for the region. A drastic spatial variation in Q0 has been noticed across our study region. Kutch, Jamnagar area are characterized by lowest Q0 values (<50) and south-east region of Saurashtra peninsula shows high Q0 (>300). These variations could be correlated with thermal effects, petrophysical properties and heterogeneity present in the crust.

  7. Crustal seismic structure beneath the Deccan Traps area (Gujarat, India), from local travel-time tomography

    NASA Astrophysics Data System (ADS)

    Prajapati, Srichand; Kukarina, Ekaterina; Mishra, Santosh

    2016-03-01

    The Gujarat region in western India is known for its intra-plate seismic activity, including the Mw 7.7 Bhuj earthquake, a reverse-faulting event that reactivated normal faults of the Mesozoic Kachchh rift zone. The Late Cretaceous Deccan Traps, one of the largest igneous provinces on the Earth, cover the southern part of Gujarat. This study is aimed at bringing light to the crustal rift zone structure and likely origin of the Traps based on the velocity structure of the crust beneath Gujarat. Tomographic inversion of the Gujarat region was done using the non-linear, passive-source tomographic algorithm, LOTOS. We use high-quality arrival times of 22,280 P and 22,040 S waves from 3555 events recorded from August 2006 to May 2011 at 83 permanent and temporary stations installed in Gujarat state by the Institute of Seismological Research (ISR). We conclude that the resulting high-velocity anomalies, which reach down to the Moho, are most likely related to intrusives associated with the Deccan Traps. Low velocity anomalies are found in sediment-filled Mesozoic rift basins and are related to weakened zones of faults and fracturing. A low-velocity anomaly in the north of the region coincides with the seismogenic zone of the reactivated Kachchh rift system, which is apparently associated with the channel of the outpouring of Deccan basalt.

  8. India: Kachchh

    Atmospheric Science Data Center

    2013-04-16

    ... show the Kachchh region in the Gujarat province of western India. On January 26, 2001, a magnitude 7.7 earthquake devastated this area, ... for the earthquake are related to the collision of India with Asia and the resulting rise of the Himalayas to the northeast. ...

  9. Gujarat, Western India

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Extremely high sediment loads are delivered to the Arabian Sea along the coast of Pakistan (upper left) and western India. In the case of the Indus River (far upper left) this sedimentation, containing large quantities of desert sand, combines with wave action to create a large sand-bar like delta. In the arid environment, the delta lacks much vegetation, but contains numerous mangrove-lined channels. This true-color image from May 2001 shows the transition from India's arid northwest to the wetter regions farther south along the coast. The increase in vegetation along the coast is brought about by the moisture trapping effect of the Western Ghats Mountain Range that runs north-south along the coast. Heavy sediment is visible in the Gulf of Kachchh (north) and the Gulf of Khambhat(south), which surround the Gujarat Peninsula.

  10. Sensitivity analysis of seismic hazard for the northwestern portion of the state of Gujarat, India

    USGS Publications Warehouse

    Petersen, M.D.; Rastogi, B.K.; Schweig, E.S.; Harmsen, S.C.; Gomberg, J.S.

    2004-01-01

    We test the sensitivity of seismic hazard to three fault source models for the northwestern portion of Gujarat, India. The models incorporate different characteristic earthquake magnitudes on three faults with individual recurrence intervals of either 800 or 1600 years. These recurrence intervals imply that large earthquakes occur on one of these faults every 266-533 years, similar to the rate of historic large earthquakes in this region during the past two centuries and for earthquakes in intraplate environments like the New Madrid region in the central United States. If one assumes a recurrence interval of 800 years for large earthquakes on each of three local faults, the peak ground accelerations (PGA; horizontal) and 1-Hz spectral acceleration ground motions (5% damping) are greater than 1 g over a broad region for a 2% probability of exceedance in 50 years' hazard level. These probabilistic PGAs at this hazard level are similar to median deterministic ground motions. The PGAs for 10% in 50 years' hazard level are considerably lower, generally ranging between 0.2 g and 0.7 g across northwestern Gujarat. Ground motions calculated from our models that consider fault interevent times of 800 years are considerably higher than other published models even though they imply similar recurrence intervals. These higher ground motions are mainly caused by the application of intraplate attenuation relations, which account for less severe attenuation of seismic waves when compared to the crustal interplate relations used in these previous studies. For sites in Bhuj and Ahmedabad, magnitude (M) 7 3/4 earthquakes contribute most to the PGA and the 0.2- and 1-s spectral acceleration ground motion maps at the two considered hazard levels. ?? 2004 Elsevier B.V. All rights reserved.

  11. Assessment of intelligence quotient among schoolchildren of fishermen community of Kutch, Gujarat, India.

    PubMed

    Asawa, Kailash; Pujara, Piyush; Thakkar, Jigar P; Pandya, Bindi Gajjar; Sharma, Anant Raghav; Pareek, Sonia; Tak, Aniruddh; Tak, Mridula; Maniar, Ronak

    2014-01-01

    The aim of the study was to assess the intelligence quotient of fishermen school children of Kutch, Gujarat, India. A descriptive cross-sectional study was conducted among 8 to 10 years old school children living in Kutch District, Gujarat, India, from January to February 2013. Seguin Form Board Test was used to assess the intelligence quotient (IQ) level of children. Means of groups were compared by independent student t-test. Stepwise multiple linear regression was used to identify predictors for IQ. The mean average timing taken by fishermen school children to complete the test was 30.64 ± 4.97. Males had significantly lower mean timing scores than females (p < 0.05). Participants with severe dental fluorosis, low socio-economic status (SES), lower education level of both mother and father and those who were overweight had significantly higher mean timing scores for average category. The present study suggested a low IQ among fishermen school children community of Kutch, Gujarat, India. The major factors which influenced their IQ were dental fluorosis, low SES, low education level of parents and high body mass index.

  12. A survey of plants in Gujarat, India, for alkaloids, saponins, and tannins

    Treesearch

    Basalingappa L. Hungund; Chandravadan H. Pathak; Chandravadan H. Pathak

    1971-01-01

    A floristic and phytochemical survey of forests in Gujarat State, India, is being undertaken to identify sources of alkaloids, saponins, and tannins. This note is a report on the results of screening 105 plant species collected from that region.

  13. Liquefaction Effects from the Bhuj earthquake

    NASA Image and Video Library

    2001-04-25

    This image from NASA Terra satellite shows the Kachchh region in the Gujarat province of western India. On January 26, 2001, a magnitude 7.7 earthquake devastated this area, killing 20,000 people and destroying buildings, dams, and port facilities.

  14. Injury epidemiology after the 2001 Gujarat earthquake in India: a retrospective analysis of injuries treated at a rural hospital in the Kutch district immediately after the disaster

    PubMed Central

    Phalkey, Revati; Reinhardt, Jan D.; Marx, Michael

    2011-01-01

    Background The number of injured far exceeds those dead and the average injury to mortality ratio in earthquakes stands at 3:1. Immediate effective medical response significantly influences injury outcomes and thus the overall health impact of earthquakes. Inadequate or mismanagement of injuries may lead to disabilities. The lack of precise data from immediate aftermath is seen as a remarkable weak point in disaster epidemiology and warrants evidence generation. Objective To analyze the epidemiology of injuries and the treatment imparted at a secondary rural hospital in the Kutch district, Gujarat, India following the January 26, 2001 earthquake. Design/Methods Discharge reports of patients admitted to the hospital over 10 weeks were analyzed retrospectively for earthquake-related injuries. Results Orthopedic injuries, (particularly fractures of the lower limbs) were predominant and serious injuries like head, chest, abdominal, and crush syndrome were minimal. Wound infections were reported in almost 20% of the admitted cases. Surgical procedures were more common than conservative treatment. The most frequently performed surgical procedures were open reduction with internal fixation and cleaning and debridement of contaminated wounds. Four secondary deaths and 102 transfers to tertiary care due to complications were reported. Conclusion The injury epidemiology reported in this study is in general agreement with most other studies reporting injury epidemiology except higher incidence of distal orthopedic injuries particularly to the lower extremities. We also found that young males were more prone to sustaining injuries. These results warrant further research. Inconsistent data reporting procedures against the backdrop of inherent disaster data incompleteness calls for urgent standardization of reporting earthquake injuries for evidence-based response policy planning. PMID:21799668

  15. Diabetes knowledge and self-efficacy among rural women in Gujarat, India.

    PubMed

    Mehta, Naaman V; Trivedi, Mayur; Maldonado, Luis E; Saxena, Deepak; Humphries, Debbie L

    2016-01-01

    Type II diabetes has risen dramatically among rural women in India, specifically in the states of Gujarat, Karnataka, Tamil Nadu and Uttar Pradesh. Recent studies suggest that rural Indian women's low level of self-efficacy, or confidence in their ability to carry out tasks, such as managing diabetes, is a key reason for this increase. Therefore, this study utilizes the Health Belief Model to analyze whether increased awareness of diabetes leads to a positive increase in levels of self-efficacy among diabetic women in two rural villages of Gujarat. A cross-sectional study of 126 known cases of women with diabetes was carried out in the villages of Rajpur and Valam in the Mehsana District in the state of Gujarat, India, to assess the relationship between diabetes knowledge and self-efficacy. The instrument was adapted from the Michigan Diabetes Research and Training Center's Diabetes Empowerment Scale-Short Form and Knowledge, Attitudes and Practices Assessment of the Indian Institute of Public Health Gandhinagar. Participants' mean knowledge score was 10.77±2.86 out of a possible 24 points, for a mean percentage of 45%. The median self-efficacy score for the women was 7 with an interquartile range of 3. The age-adjusted multiple regression analysis demonstrated a significant positive correlation between knowledge and self-efficacy (p<0.001). The observations of this study suggest a positive correlation between diabetes knowledge and self-efficacy. Future diabetes educational interventions in India should place a greater emphasis on increasing knowledge among rural women. Specifically, these interventions should emphasize the major gaps in knowledge regarding causes of diabetes, complications and treatment procedures. Educational interventions that are catered more towards rural women will be critical for improving their self-efficacy.

  16. Concentrating Solar Power Projects - Gujarat Solar One | Concentrating

    Science.gov Websites

    Solar Power | NREL Gujarat Solar One This page provides information on Gujarat Solar One, a configuration. Status Date: February 12, 2014 Project Overview Project Name: Gujarat Solar One Country: India

  17. Policy development in disaster preparedness and management: lessons learned from the January 2001 earthquake in Gujarat, India.

    PubMed

    Bremer, Rannveig

    2003-01-01

    During the last decades, several humanitarian emergencies have occurred, with an increasing number of humanitarian organizations taking part in providing assistance. However, need assessments, medical intelligence, and coordination of the aid often are sparse, resulting in the provision of ineffective and expensive assistance. When an earthquake with the strength of 7.7 on the Richter scale struck the state of Gujarat, India, during the early morning on 26 January 2001, nearly 20,000 persons were killed, nearly 170,000 were injured, and 600,000 were rendered homeless. This study identifies how assigned indicators to measure the level of health care may improve disaster preparedness and management, thus, reducing human suffering. During a two-week mission in the disaster area, the disaster relief provided to the disaster-affected population of Gujarat was evaluated. Vulnerability due to climate, geography, culture, religion, gender, politics, and economy, as each affected the outcome, was studied. By assigning indicators to the eight ELEMENTS of the Primary Health Care System as advocated by the World Health Organization (WHO), the level of public health and healthcare services were estimated, an evaluation of the impact of the disaster was conducted, and possible methods for improving disaster management are suggested. Representatives of the major relief organizations involved were interviewed on their relief policies. Strategies to improve disaster relief, such as policy development in the different aspects of public health/primary health care, were sought. Evaluation of the pre-event status of the affected society revealed a complex situation in a vulnerable society with substantial deficiencies in the existing health system that added to the severity of the disaster. Most of the civilian hospitals had collapsed, and army field hospitals provided medical care to most of the patients under primitive conditions using tents. When the foreign field hospitals arrived

  18. Is Institutional Delivery Protective Against Neonatal Mortality Among Poor or Tribal Women? A Cohort Study From Gujarat, India.

    PubMed

    Altman, Rebecca; Sidney, Kristi; De Costa, Ayesha; Vora, Kranti; Salazar, Mariano

    2017-05-01

    Objectives In low-income settings, neonatal mortality rates (NMR) are higher among socioeconomically disadvantaged groups. Institutional deliveries have been shown to be protective against neonatal mortality. In Gujarat, India, the access of disadvantaged women to institutional deliveries has increased. However, the impact of increased institutional delivery on NMR has not been studied here. This paper examined if institutional childbirth is associated with lower NMR among disadvantaged women in Gujarat, India. Methods A community-based prospective cohort of pregnant women was followed in three districts in Gujarat, India (July 2013-November 2014). Two thousand nine hundred and nineteen live births to disadvantaged women (tribal or below poverty line) were included in the study. Data was analyzed using multivariable logistic regression. Results The overall NMR was 25 deaths per 1000 live births. Multivariable analysis showed that institutional childbirth was protective against neonatal mortality only among disadvantaged women with obstetric complications during delivery. Among mothers with obstetric complications during delivery, those who gave birth in a private or public facility had significantly lower odds of having a neonatal death than women delivering at home (AOR 0.07 95% CI 0.01-0.45 and AOR 0.03, 95% CI 0.00-0.33 respectively). Conclusions for Practice Our findings highlight the crucial role of institutional delivery to prevent neonatal deaths among those born to disadvantaged women with complications during delivery in this setting. Efforts to improve disadvantaged women's access to good quality obstetric care must continue in order to further reduce the NMR in Gujarat, India.

  19. Social Stratification and Mobility in a Rural Community (Mahi) in Gujarat, India.

    ERIC Educational Resources Information Center

    Panchanadikar, K. C.; Panchanadikar, J.

    Analyzing the interaction between factors that are stable and factors that initiate change re: promotion of social mobility or crystalization of existing social stratification, this paper presents a case study of Mahi, a rural village in Gujarat, India. Utilizing data derived from two field studies (1961-1962 and March 1967-June 1967), the stable…

  20. Maternal health in Gujarat, India: a case study.

    PubMed

    Mavalankar, Dileep V; Vora, Kranti S; Ramani, K V; Raman, Parvathy; Sharma, Bharati; Upadhyaya, Mudita

    2009-04-01

    Gujarat state of India has come a long way in improving the health indicators since independence, but progress in reducing maternal mortality has been slow and largely unmeasured or documented. This case study identified several challenges for reducing the maternal mortality ratio, including lack of the managerial capacity, shortage of skilled human resources, non-availability of blood in rural areas, and infrastructural and supply bottlenecks. The Gujarat Government has taken several initiatives to improve maternal health services, such as partnership with private obstetricians to provide delivery care to poor women, a relatively-short training of medical officers and nurses to provide emergency obstetric care (EmOC), and an improved emergency transport system. However, several challenges still remain. Recommendations are made for expanding the management capacity for maternal health, operationalization of health facilities, and ensuring EmOC on 24/7 (24 hours a day, seven days a week) basis by posting nurse-midwives and trained medical officers for skilled care, ensuring availability of blood, and improving the registration and auditing of all maternal deaths. However, all these interventions can only take place if there are substantially-increased political will and social awareness.

  1. Maternal Health in Gujarat, India: A Case Study

    PubMed Central

    Vora, Kranti S.; Ramani, K.V.; Raman, Parvathy; Sharma, Bharati; Upadhyaya, Mudita

    2009-01-01

    Gujarat state of India has come a long way in improving the health indicators since independence, but progress in reducing maternal mortality has been slow and largely unmeasured or documented. This case study identified several challenges for reducing the maternal mortality ratio, including lack of the managerial capacity, shortage of skilled human resources, non-availability of blood in rural areas, and infrastructural and supply bottlenecks. The Gujarat Government has taken several initiatives to improve maternal health services, such as partnership with private obstetricians to provide delivery care to poor women, a relatively-short training of medical officers and nurses to provide emergency obstetric care (EmOC), and an improved emergency transport system. However, several challenges still remain. Recommendations are made for expanding the management capacity for maternal health, operationalization of health facilities, and ensuring EmOC on 24/7 (24 hours a day, seven days a week) basis by posting nurse-midwives and trained medical officers for skilled care, ensuring availability of blood, and improving the registration and auditing of all maternal deaths. However, all these interventions can only take place if there are substantially-increased political will and social awareness. PMID:19489418

  2. Indian social safety net programs as platforms for introducing wheat flour fortification: a case study of Gujarat, India.

    PubMed

    Fiedler, John L; Babu, Sunil; Smitz, Marc-Francois; Lividini, Keith; Bermudez, Odilia

    2012-03-01

    Micronutrient deficiencies exact an enormous health burden on India. The release of the National Family Health Survey results--showing the relatively wealthy state of Gujarat having deficiency levels exceeding national averages--prompted Gujarat officials to introduce fortified wheat flour in their social safety net programs (SSNPs). To provide a case study of the introduction of fortified wheat flour in Gujarat's Public Distribution System (PDS), Integrated Child Development Scheme (ICDS), and Mid-Day Meal (MDM) Programme to assess the coverage, costs, impact, and cost-effectiveness of the initiative. India's 2004/05 National Sample Survey data were used to identify beneficiaries of each of Gujarat's three SSNPs and to estimate usual intake levels of vitamin A, iron, and zinc. Comparing age- and sex-specific usual intakes to Estimated Average Requirements, the proportion of the population with inadequate intakes was estimated. Postfortification intake levels and reductions in inadequate intake were estimated. The incremental cost of fortifying wheat flour and the cost-effectiveness of each program were estimated. When each program was assessed independently, the proportion of the population with inadequate vitamin A intakes was reduced by 34% and 74% among MDM and ICDS beneficiaries, respectively. Both programs effectively eliminated inadequate intakes of both iron and zinc. Among PDS beneficiaries, the proportion with inadequate iron intakes was reduced by 94%. CONCLUSIONS. Gujarat's substitution of fortified wheat flour for wheat grain is dramatically increasing the intake of micronutrients among its SSNP beneficiaries. The incremental cost of introducing fortification in each of the programs is low, and, according to World Health Organization criteria, each program is "highly cost-effective." The introduction of similar reforms throughout India would largely eliminate the inadequate iron intake among persons participating in any of the three SSNPs and would

  3. Prevalence of skeletal fluorosis in fisherman from Kutch coast, Gujarat, India.

    PubMed

    John, Jacob; Hariharan, Madhu; Remy, Vimal; Haleem, Shaista; Thajuraj, Pathinettam Kandathil; Deepak, Baby; Rajeev, Kundaningattu Govindan; Devang Divakar, Darshan

    2015-01-01

    In health terms, consuming fluoride is well recognised to be a double-edged sword. Consumption of optimal amounts is beneficial to health, however an excess constitutes a health hazard. To assess the prevalence of skeletal fluorosis in fishermen from the Kutch coast, Gujarat, India. A descriptive cross-sectional survey was conducted on 653 fishermen from the Kutch District, Gujarat, India, from October 2014 to December 2014. Clinical skeletal fluorosis was assessed using three diagnostic tests. Drinking water fluoride concentrations in different regions of the study area were determined. General information regarding age, gender and adverse habits were also collected. The Chi square test was used for comparisons and the confidence level and critical p-value were set at 95% and 5% respectively. Fluoride concentrations in water from the study area ranged between 3.4-6.9 ppm. The prevalence of skeletal fluorosis was 30.3%, out of which, the majority of the subjects had mild skeletal fluorosis (18.4%). This condition was found to be significantly associated with age and gender along with tobacco and alcohol consumption; depending on the habit's duration. Being a public health problem in the fishermen community, skeletal fluorosis requires a-priori attention. Measures for preventing this disease should be undertaken on a communitywide basis.

  4. Shoreline changes and Coastal Flooding impacts: South Gujarat coast (India)

    NASA Astrophysics Data System (ADS)

    Parihar, S. B.

    2016-12-01

    South Gujarat coast (India) is experiencing increased coastal inundation and erosion caused by sea-level rise affecting the population, infrastructure, and environment. The area falls under low elevation coastal zone (LEZ) and its topography of the area is also making coast highly susceptible to flooding, especially at high tides and during the rainy season. As part of studies on shoreline changes field trip carried on the coastal taluka's of South Gujarat coast i.e. Surat, Navsari and Valsad shows various temporal changes is taking place at coastal belt. There are ample of studies on coastal dynamics and impacts. The study focus on spatial temporal analysis shows the vulnerable zones covering various physical elements at risk. These coastal areas are attractive in nature for all kind of economic development and growth because of availability of the water & fertile land for house hold use, fishing and transportation. On the contrary, South Gujarat coast being tectonically active; makes this region high vulnerable for any kind of infrastructure development. The region had also witnessed loss of life and property, disruptions to transport & power and incidences of epidemics during the floods of 2006 in Surat. Coastal flooding would, under these scenarios, threaten region that are home of 370,000 approx (Census, 2011) people in seven coastal taluka's of Surat, Navsari and Valsad district. Among the people residing in the region, the most vulnerable communities are fishermen, farmer and industrial labours. The wide range of infrastructure such as roads, hospitals, schools, power plants, industries and port will also be at risk. Shoreline changes are inevitably changing the characteristics of south Gujarat coast; practices and policies should be put in place to mitigate the potentially adverse impacts on environment and human settlements. Key words: sea level rise, LEZ, vulnerable, erosion, inundation, spatial temporal analysis, landuse changes.

  5. Infection control in delivery care units, Gujarat state, India: A needs assessment

    PubMed Central

    2011-01-01

    Background Increasingly, women in India attend health facilities for childbirth, partly due to incentives paid under government programs. Increased use of health facilities can alleviate the risks of infections contracted in unhygienic home deliveries, but poor infection control practices in labour and delivery units also cause puerperal sepsis and other infections of childbirth. A needs assessment was conducted to provide information on procedures and practices related to infection control in labour and delivery units in Gujarat state, India. Methods Twenty health care facilities, including private and public primary health centres and referral hospitals, were sampled from two districts in Gujarat state, India. Three pre-tested tools for interviewing and for observation were used. Data collection was based on existing infection control guidelines for clean practices, clean equipment, clean environment and availability of diagnostics and treatment. The study was carried out from April to May 2009. Results Seventy percent of respondents said that standard infection control procedures were followed, but a written procedure was only available in 5% of facilities. Alcohol rubs were not used for hand cleaning and surgical gloves were reused in over 70% of facilities, especially for vaginal examinations in the labour room. Most types of equipment and supplies were available but a third of facilities did not have wash basins with "hands-free" taps. Only 15% of facilities reported that wiping of surfaces was done immediately after each delivery in labour rooms. Blood culture services were available in 25% of facilities and antibiotics are widely given to women after normal delivery. A few facilities had data on infections and reported rates of 3% to 5%. Conclusions This study of current infection control procedures and practices during labour and delivery in health facilities in Gujarat revealed a need for improved information systems, protocols and procedures, and for

  6. Seismotectonic Models of the Three Recent Devastating SCR Earthquakes in India

    NASA Astrophysics Data System (ADS)

    Mooney, W. D.; Kayal, J.

    2007-12-01

    During the last decade, three devastating earthquakes, the Killari 1993 (Mb 6.3), Jabalpur 1997 (Mb 6.0) and the Bhuj 2001 (Mw 7.7) occurred in the Stable Continental Region (SCR), Peninsular India. First, the September 30, 1993 Killari earthquake (Mb 6.3) occurred in the Deccan province of central India, in the Latur district of Maharashtra state. The local geology in the area is obscured by the late Cretaceous-Eocene basalt flows, referred to as the Deccan traps. This makes it difficult to recognize the geological surface faults that could be associated with the Killari earthquake. The epicentre was reported at 18.090N and 76.620E, and the focal depth at 7 +/- 1 km was precisely estimated by waveform inversion (Chen and Kao, 1995). The maximum intensity reached to VIII and the earthquake caused a loss of about 10,000 lives and severe damage to property. The May 22, 1997 Jabalpur earthquake (Mb 6.0), epicentre at 23.080N and 80.060E, is a well studied earthquake in the Son-Narmada-Tapti (SONATA) seismic zone. A notable aspects of this earthquake is that it was the first significant event in India to be recorded by 10 broadband seismic stations which were established in 1996 by the India Meteorological Department (IMD). The focal depth was well estimated using the "converted phases" of the broadband seismograms. The focal depth was given in the lower crust at a depth of 35 +/- 1 km, similar to the moderate earthquakes reported from the Amazona ancient rift system in SCR of South America. Maximum MSK intensity of the Jabalpur earthquake reached to VIII in the MSK scale and this earthquake killed about 50 people in the Jabalpur area. Finally, the Bhuj earthquake (MW 7.7) of January 26, 2001 in the Gujarat state, northwestern India, was felt across the whole country, and killed about 20,000 people. The maximum intensity level reached X. The epicenter of the earthquake is reported at 23.400N and 70.280E, and the well estimated focal depth at 25 km. A total of about

  7. Political ecology of groundwater: the contrasting case of water-abundant West Bengal and water-scarce Gujarat, India

    NASA Astrophysics Data System (ADS)

    Mukherji, Aditi

    2006-03-01

    Three apparently disparate themes (groundwater, farmers and politics) interweave in this account of how groundwater-related policies in India have very little to do with the scarcity, depletion or quality of groundwater, and more to do with rural politics manifested, among other things, in terms of the presence or absence of farmer lobbies. Examples from two states of India, the water-abundant state of West Bengal and water-scarce state of Gujarat, were investigated using readily available data, analysis of the literature, interviews and fieldwork. In the case of West Bengal, although there is no pressing groundwater crisis, the government of West Bengal (GOWB) was able to successfully implement strict groundwater regulations along with a drastic increase in electricity tariff. More importantly, GOWB was able to implement these without any form of visible farmer protest, though these measures negatively affected farmer incomes. On the other hand, in Gujarat, where there is a real and grave groundwater crisis, the government of Gujarat has neither been able to implement strict groundwater regulations, nor has it been able to increase electricity tariff substantially. Thus, through the lens of ‘political ecology’ the contrasting case of these two Indian states is explained.

  8. Serosurvey of Crimean-Congo hemorrhagic fever virus in domestic animals, Gujarat, India, 2013.

    PubMed

    Mourya, Devendra T; Yadav, Pragya D; Shete, Anita; Majumdar, Triparna D; Kanani, Amit; Kapadia, Dhirendra; Chandra, Vartika; Kachhiapatel, Anantdevesh J; Joshi, Pravinchandra T; Upadhyay, Kamalesh J; Dave, Paresh; Raval, Dinkar

    2014-09-01

    Crimean-Congo hemorrhagic fever (CCHF) is a tick-borne viral disease that causes a fatal hemorrhagic illness in humans. This disease is asymptomatic in animals. CCHF was first confirmed in a nosocomial outbreak in 2011 in Gujarat State. Another notifiable outbreak occurred in July, 2013, in Karyana Village, Amreli district, Gujarat State. Anti-CCHF virus (CCHFV) immunoglobulin G (IgG) antibodies were detected in domestic animals from the adjoining villages of the affected area, indicating a considerable amount of positivity against domestic animals. The present serosurvey was carried out to determine the prevalence of CCHFV among bovine, sheep, and goat populations from 15 districts of Gujarat State, India. A total of 1226 serum samples from domestic animals were screened for IgG antibodies using a CCHF animal IgG enzyme-linked immunosorbent assay (ELISA) kit from the Centers for Disease Control and Prevention. Antibodies were detected in all the 15 districts surveyed; with positivity of 12.09%, 41.21%, and 33.62% in bovine, sheep, and goat respectively. This necessitates the surveillance of CCHFV IgG antibodies in animals and hemorrhagic fever cases in human.

  9. Emergence of Crimean-Congo hemorrhagic fever in Amreli District of Gujarat State, India, June to July 2013.

    PubMed

    Yadav, Pragya D; Gurav, Yogesh K; Mistry, Madhulika; Shete, Anita M; Sarkale, Prasad; Deoshatwar, Avinash R; Unadkat, Vishwa B; Kokate, Prasad; Patil, Deepak Y; Raval, Dinkar K; Mourya, Devendra T

    2014-01-01

    Crimean-Congo hemorrhagic fever virus (CCHFV) etiology was detected in a family cluster (nine cases, including two deaths) in the village of Karyana, Amreli District, and also a fatal case in the village of Undra, Patan District, in Gujarat State, India. Anti-CCHFV IgG antibodies were detected in domestic animals from Karyana and adjoining villages. Hyalomma ticks from households were found to be positive for CCHF viral RNA. This confirms the emergence of CCHFV in new areas and the wide spread of this disease in Gujarat State. Copyright © 2013 The Authors. Published by Elsevier Ltd.. All rights reserved.

  10. Duchenne/Becker muscular dystrophy: A report on clinical, biochemical, and genetic study in Gujarat population, India.

    PubMed

    Rao, Mandava V; Sindhav, Gaurang M; Mehta, Jitendra J

    2014-07-01

    In India, various groups have studied different regions to find out deletion pattern of dystrophin gene. We have investigated its deletion pattern among Duchenne/Becker muscular dystrophy (D/BMD) patients across Gujarat. Moreover, in this study we also correlate the same with reading frame rule. However, we too consider various clinicopathological features to establish as adjunct indices when deletion detection fails. In this pilot study, a total of 88 D/BMD patients consulting at our centers in Gujarat, India were included. All patients were reviewed on basis of their clinical characteristics, tested by three primer sets of 10-plex, 9-plex, and 7-plex polymerase chain reaction (PCR) for genetic analysis; whereas, biochemical indices were measured using automated biochemical analyzers. The diagnosis of D/BMD was confirmed by multiplex-PCR (M-PCR) in D/BMD patients. A number of 65 (73.86%) out of 88 patients showed deletion in dystrophin gene. The exon 50 (58.46%) was the most frequent deletion found in our study. The mean age of onset of DMD and BMD was 4.09 ± 0.15 and 7.14 ± 0.55 years, respectively. In patients, mean creatine phosphokinase (CPK), lactate dehydrogenase (LDH), and myoglobin levels were elevated significantly (P < 0.05) in comparison to controls. Addition to CPK, LDH and myoglobin are good adjunct when deletion detection failed. These data are further in accordance with world literature when correlated with frame rule. The analysis has been carried out for the first time for a total of 88 D/BMD patients particularly from Gujarat, India. More research is essential to elucidate specific mutation pattern in association with management and therapies of proband.

  11. Mucormycosis at a tertiary care centre in Gujarat, India.

    PubMed

    Patel, Atul K; Patel, Ketan K; Patel, Kamlesh; Gohel, Swati; Chakrabarti, Arunaloke

    2017-06-01

    The prevalence of mucormycosis is reportedly high in India, although the studies are mainly from north and south India only. We analysed the mucormycosis cases at tertiary care centres of West India. We retrieved the clinical details of all the patients with probable and proven mucormycosis diagnosed at Sterling Hospital and ID clinic at Ahmedabad, Gujarat over the period from 1 January 2013 through 30 April 2015. The data were analysed to determine demography, risk factors, underlying diseases, site of infection and outcome of these patients. A total of 27 patients with the median age of 50 (16-65) years were diagnosed with mucormycosis during the period. Rhino-orbital-cerebral mucormycosis was the most common (51.9%) presentation. Majority (55.6%) of the patients had uncontrolled diabetes with or without ketoacidosis; 25.9% patients had no underlying disease and most of them (85.7%) had cutaneous mucormycosis. In this group, the mortality was 25.9% and an equal percentage of patients were lost to follow up; 14 (51.9%) patients could complete 6 weeks of amphotericin B therapy. All patients who completed antifungal therapy survived except one. Like other parts of India, uncontrolled diabetes was the predominant risk factor for mucormycosis in our group. Patients completing 6 weeks of amphotericin B treatment were likely to survive. © 2017 Blackwell Verlag GmbH.

  12. Knowledge and opinion about smoke-free laws and second-hand smoke among hospitality venue managers in Gujarat and Andhra Pradesh, India.

    PubMed

    Gupta, Vinay K; Arora, Monika; Sharma, Indrani; Nazar, Gaurang P; Modi, Bhavesh; Singh, Deepti; Millett, Christopher; Reddy, K Srinath

    2013-01-01

    India's Smoke-Free Law (SFL) was implemented in 2004 and reinforced on 2nd October 2008. This research attempts to understand the knowledge and opinion of hospitality venue (HV) managers about second-hand smoke (SHS) and SFL as well as self-reported compliance with SFL in two Indian states. A survey was conducted among 804 randomly sampled HVs from project STEPS (Strengthening of tobacco control efforts through innovative partnerships and strategies) in Gujarat and Andhra Pradesh, India. Four hundred and three HVs from two districts in Gujarat and 401 HVs from six districts in Andhra Pradesh were selected. The owner, manager or supervisor of each HV was interviewed using a pre-tested structured interview schedule. Association of opinion scales with respondents' background characteristics was assessed through the analysis of variance (ANOVA) method. Out of the 403 respondents in Gujarat and 401 in Andhra Pradesh, 56.1% and 84.3% had knowledge about SFL respectively. Compliance of HVs with SFL was 21.8% in Gujarat and 31.2% in Andhra Pradesh as reported by the managers. Knowledge about SHS was noted among 39.7% of respondents in Gujarat and 25.4% in Andhra Pradesh. Bivariate results indicated that more educated HV managers showed higher support for smoke-free public places (P < 0.001) and were more concerned about the health effects of SHS exposure (P = 0.002). Complete self-reported compliance with, and knowledge of SFL as well as SHS was not found in Gujarat and Andhra Pradesh. The education level of HV managers is an important determinant to ensure compliance with SFL in public places.

  13. Study of Blood-transfusion Services in Maharashtra and Gujarat States, India

    PubMed Central

    Ramani, K.V.; Govil, Dipti

    2009-01-01

    Blood-transfusion services are vital to maternal health because haemorrhage and anaemia are major causes of maternal death in South Asia. Unfortunately, due to continued governmental negligence, blood-transfusion services in India are a highly-fragmented mix of competing independent and hospital-based blood-banks, serving the needs of urban populations. This paper aims to understand the existing systems of blood-transfusion services in India focusing on Maharashtra and Gujarat states. A mix of methodologies, including literature review (including government documents), analysis of management information system data, and interviews with key officials was used. Results of analysis showed that there are many managerial challenges in blood-transfusion services, which calls for strengthening the planning and monitoring of these services. Maharashtra provides a good model for improvement. Unless this is done, access to blood in rural areas may remain poor. PMID:19489420

  14. Duchenne/Becker muscular dystrophy: A report on clinical, biochemical, and genetic study in Gujarat population, India

    PubMed Central

    Rao, Mandava V.; Sindhav, Gaurang M.; Mehta, Jitendra J.

    2014-01-01

    Objective: In India, various groups have studied different regions to find out deletion pattern of dystrophin gene. We have investigated its deletion pattern among Duchenne/Becker muscular dystrophy (D/BMD) patients across Gujarat. Moreover, in this study we also correlate the same with reading frame rule. However, we too consider various clinicopathological features to establish as adjunct indices when deletion detection fails. Materials and Methods: In this pilot study, a total of 88 D/BMD patients consulting at our centers in Gujarat, India were included. All patients were reviewed on basis of their clinical characteristics, tested by three primer sets of 10-plex, 9-plex, and 7-plex polymerase chain reaction (PCR) for genetic analysis; whereas, biochemical indices were measured using automated biochemical analyzers. Results: The diagnosis of D/BMD was confirmed by multiplex-PCR (M-PCR) in D/BMD patients. A number of 65 (73.86%) out of 88 patients showed deletion in dystrophin gene. The exon 50 (58.46%) was the most frequent deletion found in our study. The mean age of onset of DMD and BMD was 4.09 ± 0.15 and 7.14 ± 0.55 years, respectively. In patients, mean creatine phosphokinase (CPK), lactate dehydrogenase (LDH), and myoglobin levels were elevated significantly (P < 0.05) in comparison to controls. Addition to CPK, LDH and myoglobin are good adjunct when deletion detection failed. These data are further in accordance with world literature when correlated with frame rule. Conclusion: The analysis has been carried out for the first time for a total of 88 D/BMD patients particularly from Gujarat, India. More research is essential to elucidate specific mutation pattern in association with management and therapies of proband. PMID:25221400

  15. SRTM Radar Image with Color as Height: Kachchh, Gujarat, India

    NASA Image and Video Library

    2001-04-05

    This image shows the area around the January 26, 2001, earthquake in western India, the deadliest in the country history with some 20,000 fatalities. The epicenter of the magnitude 7.6 earthquake was just to the left of the center of the image.

  16. Y Chromosome Haplogroup Distribution in Indo-European Speaking Tribes of Gujarat, Western India

    PubMed Central

    Aggarwal, Aastha; Mitra, Siuli; Italia, Yazdi M.; Saraswathy, Kallur N.; Chandrasekar, Adimoolam

    2014-01-01

    The present study was carried out in the Indo-European speaking tribal population groups of Southern Gujarat, India to investigate and reconstruct their paternal population structure and population histories. The role of language, ethnicity and geography in determining the observed pattern of Y haplogroup clustering in the study populations was also examined. A set of 48 bi-allelic markers on the non-recombining region of Y chromosome (NRY) were analysed in 284 males; representing nine Indo-European speaking tribal populations. The genetic structure of the populations revealed that none of these groups was overtly admixed or completely isolated. However, elevated haplogroup diversity and FST value point towards greater diversity and differentiation which suggests the possibility of early demographic expansion of the study groups. The phylogenetic analysis revealed 13 paternal lineages, of which six haplogroups: C5, H1a*, H2, J2, R1a1* and R2 accounted for a major portion of the Y chromosome diversity. The higher frequency of the six haplogroups and the pattern of clustering in the populations indicated overlapping of haplogroups with West and Central Asian populations. Other analyses undertaken on the population affiliations revealed that the Indo-European speaking populations along with the Dravidian speaking groups of southern India have an influence on the tribal groups of Gujarat. The vital role of geography in determining the distribution of Y lineages was also noticed. This implies that although language plays a vital role in determining the distribution of Y lineages, the present day linguistic affiliation of any population in India for reconstructing the demographic history of the country should be considered with caution. PMID:24614885

  17. Y chromosome haplogroup distribution in Indo-European speaking tribes of Gujarat, western India.

    PubMed

    Khurana, Priyanka; Aggarwal, Aastha; Mitra, Siuli; Italia, Yazdi M; Saraswathy, Kallur N; Chandrasekar, Adimoolam; Kshatriya, Gautam K

    2014-01-01

    The present study was carried out in the Indo-European speaking tribal population groups of Southern Gujarat, India to investigate and reconstruct their paternal population structure and population histories. The role of language, ethnicity and geography in determining the observed pattern of Y haplogroup clustering in the study populations was also examined. A set of 48 bi-allelic markers on the non-recombining region of Y chromosome (NRY) were analysed in 284 males; representing nine Indo-European speaking tribal populations. The genetic structure of the populations revealed that none of these groups was overtly admixed or completely isolated. However, elevated haplogroup diversity and FST value point towards greater diversity and differentiation which suggests the possibility of early demographic expansion of the study groups. The phylogenetic analysis revealed 13 paternal lineages, of which six haplogroups: C5, H1a*, H2, J2, R1a1* and R2 accounted for a major portion of the Y chromosome diversity. The higher frequency of the six haplogroups and the pattern of clustering in the populations indicated overlapping of haplogroups with West and Central Asian populations. Other analyses undertaken on the population affiliations revealed that the Indo-European speaking populations along with the Dravidian speaking groups of southern India have an influence on the tribal groups of Gujarat. The vital role of geography in determining the distribution of Y lineages was also noticed. This implies that although language plays a vital role in determining the distribution of Y lineages, the present day linguistic affiliation of any population in India for reconstructing the demographic history of the country should be considered with caution.

  18. Using an emergency response infrastructure to help women who experience gender-based violence in Gujarat, India.

    PubMed

    Newberry, Jennifer A; Mahadevan, Swaminatha; Gohil, Narendrasinh; Jamshed, Roma; Prajapati, Jashvant; Rao, Gv Ramana; Strehlow, Matthew

    2016-05-01

    Many women who experience gender-based violence may never seek any formal help because they do not feel safe or confident that they will receive help if they try. A public-private-academic partnership in Gujarat, India, established a toll-free telephone helpline - called 181 Abhayam - for women experiencing gender-based violence. The partnership used existing emergency response service infrastructure to link women to phone counselling, nongovernmental organizations (NGOs) and government programmes. In India, the lifetime prevalence of gender-based violence is 37.2%, but less than 1% of women will ever seek help beyond their family or friends. Before implementation of the helpline, there were no toll-free helplines or centralized coordinating systems for government programmes, NGOs and emergency response services. In February 2014, the helpline was launched across Gujarat. In the first 10 months, the helpline assisted 9767 individuals, of which 8654 identified themselves as women. Of all calls, 79% (7694) required an intervention by phone or in person on the day they called and 43% (4190) of calls were by or for women experiencing violence. Despite previous data that showed women experiencing gender-based violence rarely sought help from formal sources, women in Gujarat did use the helpline for concerns across the spectrum of gender-based violence. However, for evaluating the impact of the helpline, the operational definitions of concern categories need to be further clarified. The initial triage system for incoming calls was advantageous for handling high call volumes, but may have contributed to dropped calls.

  19. Genome Sequence of Salt-Tolerant Bacillus safensis Strain VK, Isolated from Saline Desert Area of Gujarat, India.

    PubMed

    Kothari, V V; Kothari, R K; Kothari, C R; Bhatt, V D; Nathani, N M; Koringa, P G; Joshi, C G; Vyas, B R M

    2013-09-05

    Bacillus safensis strain VK was isolated from the rhizosphere of a cumin plant growing in the saline desert of Radhanpar, Gujarat, India. Here, we provide the 3.68-Mb draft genome sequence of B. safensis VK, which might provide information about the salt tolerance and genes encoding enzymes for the strain's plant growth-promoting potential.

  20. Towards a Managed Aquifer Recharge strategy for Gujarat, India: An economist’s dialogue with hydro-geologists

    NASA Astrophysics Data System (ADS)

    Shah, Tushaar

    2014-10-01

    Gujarat state in Western India exemplifies all challenges of an agrarian economy founded on groundwater overexploitation sustained over decades by perverse energy subsidies. Major consequences are: secular decline in groundwater levels, deterioration of groundwater quality, rising energy cost of pumping, soaring carbon footprint of agriculture and growing financial burden of energy subsidies. In 2009, Government of Gujarat asked the present author, an economist, to chair a Taskforce of senior hydro-geologists and civil engineers to develop and recommend a Managed Aquifer Recharge (MAR) strategy for the state. This paper summarizes the recommended strategy and its underlying logic. It also describes the imperfect fusion of socio-economic and hydro-geologic perspectives that occurred in course of the working of the Taskforce and highlights the need for trans-disciplinary perspectives on groundwater governance.

  1. Knowledge, attitudes, and practices of private sector immunization service providers in Gujarat, India.

    PubMed

    Hagan, José E; Gaonkar, Narayan; Doshi, Vikas; Patni, Anas; Vyas, Shailee; Mazumdar, Vihang; Kosambiya, J K; Gupta, Satish; Watkins, Margaret

    2018-01-02

    India is responsible for 30% of the annual global cohort of unvaccinated children worldwide. Private practitioners provide an estimated 21% of vaccinations in urban centers of India, and are important partners in achieving high vaccination coverage. We used an in-person questionnaire and on-site observation to assess knowledge, attitudes, and practices of private immunization service providers regarding delivery of immunization services in the urban settings of Surat and Baroda, in Gujarat, India. We constructed a comprehensive sampling frame of all private physician providers of immunization services in Surat and Baroda cities, by consulting vaccine distributors, local branches of physician associations, and published lists of private medical practitioners. All providers were contacted and asked to participate in the study if they provided immunization services. Data were collected using an in-person structured questionnaire and directly observing practices; one provider in each practice setting was interviewed. The response rate was 82% (121/147) in Surat, and 91% (137/151) in Baroda. Of 258 participants 195 (76%) were pediatricians, and 63 (24%) were general practitioners. Practices that were potential missed opportunities for vaccination (MOV) included not strictly following vaccination schedules if there were concerns about ability to pay (45% of practitioners), and not administering more than two injections in the same visit (60%). Only 22% of respondents used a vaccination register to record vaccine doses, and 31% reported vaccine doses administered to the government. Of 237 randomly selected vaccine vials, 18% had expired vaccine vial monitors. Quality of immunization services in Gujarat can be strengthened by providing training and support to private immunization service providers to reduce MOVs and improve quality and safety; other more context specific strategies that should be evaluated may involve giving feedback to providers on quality of services

  2. Neo-deterministic definition of earthquake hazard scenarios: a multiscale application to India

    NASA Astrophysics Data System (ADS)

    Peresan, Antonella; Magrin, Andrea; Parvez, Imtiyaz A.; Rastogi, Bal K.; Vaccari, Franco; Cozzini, Stefano; Bisignano, Davide; Romanelli, Fabio; Panza, Giuliano F.; Ashish, Mr; Mir, Ramees R.

    2014-05-01

    performed to understand the influence of the model characteristics on the computed ground shaking scenarios. For massive parametric tests, or for the repeated generation of large scale hazard maps, the methodology can take advantage of more advanced computational platforms, ranging from GRID computing infrastructures to HPC dedicated clusters up to Cloud computing. In such a way, scientists can deal efficiently with the variety and complexity of the potential earthquake sources, and perform parametric studies to characterize the related uncertainties. NDSHA provides realistic time series of expected ground motion readily applicable for seismic engineering analysis and other mitigation actions. The methodology has been successfully applied to strategic buildings, lifelines and cultural heritage sites, and for the purpose of seismic microzoning in several urban areas worldwide. A web application is currently being developed that facilitates the access to the NDSHA methodology and the related outputs by end-users, who are interested in reliable territorial planning and in the design and construction of buildings and infrastructures in seismic areas. At the same, the web application is also shaping up as an advanced educational tool to explore interactively how seismic waves are generated at the source, propagate inside structural models, and build up ground shaking scenarios. We illustrate the preliminary results obtained from a multiscale application of NDSHA approach to the territory of India, zooming from large scale hazard maps of ground shaking at bedrock, to the definition of local scale earthquake scenarios for selected sites in the Gujarat state (NW India). The study aims to provide the community (e.g. authorities and engineers) with advanced information for earthquake risk mitigation, which is particularly relevant to Gujarat in view of the rapid development and urbanization of the region.

  3. Knowledge of and attitudes toward clinical depression among health providers in Gujarat, India.

    PubMed

    Almanzar, Santiago; Shah, Nirsarg; Vithalani, Suril; Shah, Sandip; Squires, James; Appasani, Raghu; Katz, Craig L

    2014-01-01

    Clinical depression is a major leading cause of morbidity and mortality but it is oftentimes overlooked and undertreated. The negative perception and lack of understanding of this condition prevents millions of people from seeking appropriate and on-time medical help, leading to distress and increased burden for affected people and their families. The implementation of public education campaigns and training of non-psychiatric health professionals on mental health and clinical depression has been neglected in several countries, including India, which is the second most populous country in the world with a population of more than 1.2 billion people, almost one-fifth of the world's population. This study sought to explore the knowledge and attitudes toward the diagnosis and treatment of clinical depression in nonpsychiatric health care providers in Vadodara, Gujarat, India. A cross-sectional survey was conducted over a 4-week period In Gujarat, India among resident physicians and community health workers about their knowledge and views on clinical depression. We found considerable stigma and misinformation about depression especially among health care workers in India. Most of the community health workers had a great deal of difficulty when defining clinical depression, and a large majority said that they never heard about depression or its definition and although the overwhelming majority of respondents did not believe that clinical depression results from a punishment from God (82% disagreed or strongly disagreed with this belief) or evil spirits (77.5%), a much smaller proportion disagreed with the assertions that depression was either solely due to difficult circumstances (38.2%) or that sufferers only had themselves to blame (47.2%). Meanwhile, only 32.6% disagreed with the position that clinical depression is a sign of weakness and 39.4% disagreed with the statement that suicide was a sign of weakness. Our findings underscore the considerable public health

  4. The Gujarat earthquake (2001) experience in a seismically unprepared area: community hospital medical response.

    PubMed

    Roy, Nobhojit; Shah, Hemant; Patel, Vikas; Coughlin, R Richard

    2002-01-01

    At 08:53 hours on 26 January 2001, an earthquake measuring 6.9 on the Richter scale devastated a large, drought-affected area of northwestern India, the state of Gujarat. The known number killed by the earthquake is 20,005, with 166,000 injured, of whom 20,717 were "seriously" injured. About 370,000 houses were destroyed, and another 922,000 were damaged. A community health worker using the local language interviewed all of the patients admitted to the Gandhi-Lincoln hospital with an on-site, oral, real-time, Victim Specific Questionnaire (VSQ). The census showed a predominance of women, children, and young adults, with the average age being 28 years. The majority of the patients had other family members who were also injured (84%), but most had not experienced deaths among family members (86%). Most of the patients (91%) had traveled more than 200 kilometers using their family cars, pick-ups, trucks, or buses to reach the buffer zone hospitals. The daily hospital admission rate returned to pre-event levels five days after the event, and all of the hospital services were restored by nine days after the quake. Most of the patients (83%) received definitive treatment in the buffer zone hospitals; 7% were referred to tertiary-care centers; and 9% took discharge against medical advice. The entrapped village folk with their traditional architecture had lesser injuries and a higher rescue rate than did the semi-urban townspeople, who were trapped in collapsed concrete masonry buildings and narrow alleys. However, at the time of crisis, aware townspeople were able to tap the available health resources better than were the poor. There was a low incidence of crush injuries. Volunteer doctors from various backgrounds teamed up to meet the medical crisis. International relief agencies working through local groups were more effective. Local relief groups needed to coordinate better. Disaster tourism by various well-meaning agencies took a toll on the providers. Many surgeries

  5. Oral health status of fishermen and non-fishermen community of Kutch district, Gujarat, India: a comparative study.

    PubMed

    Asawa, Kailash; Pujara, Piyush; Tak, Mridula; Nagarajappa, Ramesh; Aapaliya, Pankaj; Bhanushali, Nikhil; Mishra, Prashant; Sharma, Abhishek

    2014-01-01

    Fishing is one such hazardous occupation, which involves irregular diet, stress, alcoholism, tobacco and pernicious habits. Fishermen have lower socio-economic status and their illiteracy adds to their poor oral hygiene, which may influence general and oral health. The aim of the study was to assess and compare the oral health status of fishermen and non-fishermen population of Kutch District, Gujarat, India. A descriptive cross-sectional survey was conducted to assess and compare the oral health status of the fishermen and non-fishermen community of Mundra taluka of Kutch district, Gujarat, India, from January 2013 to June 2013. Fishermen had significantly higher periodontal disease and dental caries than non-fishermen group (p = 0.001). Malocclusion was significantly higher in non-fishermen group (p = 0.001). Extraction was the most prevalent treatment need among both groups. Occupation and educational status were respectively identified as the best predictors for dental caries and periodontal disease. Findings of the present study suggest that oral health status of the fishermen population was relatively poor, with high caries prevalence and poor periodontal health when compared to the non-fishermen population. In the light of high treatment needs of the study population, health policy that emphasises oral health promotion and prevention would seem more advantageous in addition to traditional curative care.

  6. The Gujarat Earthquake: Mitigations Failures and Lessons learnt for Future Strategies

    NASA Astrophysics Data System (ADS)

    Katuri, A. K.; Mittal, J.; Kumar, K.

    Time and again, the Indian subcontinent has been suffering from diverse natural calamities, ranging from droughts to floods, landslides to earthquakes, and cyclones to spells of famines. Recently, in October 1999, a severe cyclone battered the eastern coast of Orissa affecting millions of people, blowing away homes, damaging buildings, destroying crops and wiping out a huge cattle population. The Gujarat earthquake of January 2001 was another monumental disaster that affected more than 15 million people causing colossal loss of life and property estimated at US 1.30 billion, though actual may be much higher. More than 200 international and domestic voluntary agencies promptly rushed aid to the damaged areas at the shake of the quake-2001. In this crucial rescue phase, teams were scattered across affected villages and urban centers, clueless of precise locations and extent of damage. Problems faced during the relief and rehabilitation were- absence of a comprehensive information system (both spatial and attribute), absence of a nodal agency to disseminate information on the type of relief required, absence of high precision remotely sensed data, appropriate for preparation and implementation of long term reconstruction and rehabilitation plan (Development Plan). Repeated disaster assessments by multiple agencies led to wastage of time and resources. All this led to non-coherence amongst the coordinating agencies, and rescue &relief teams. Spatial and attribute damage assessment could have been easier in the presence of comprehensive geographic and demographic information supported by high precision satellite imageries to compare pre and post disaster situation. Disaster management includes pre-disaster preparedness planning, post- disaster damage assessment, search and rescue, rehabilitation and reconstruction activities. Unlike other disasters, scientific alerts, forecasts and warnings of impending earthquake still require more attention. Disaster Preparedness Plan

  7. Different stages of collision zones on examples of Gujarat province (India) and Caucasus

    NASA Astrophysics Data System (ADS)

    Zabelina, Irina; Koulakov, Ivan; Ranjan Kayal, Jnana; Pratap Singh, Ajay; Kumar, Santosh; Kukarina, Ekaterina; Amanatashvili, Iason

    2016-04-01

    In this study we present seismic structures of the crust and upper mantle beneath two regions: Kachchh Gujarat region (India), and Caucasus that may represent different stages of the collisional processes. In both cases, the 3D seismic models were obtained based on tomography inversion of arrival times of P and S seismic waves from local and regional earthquakes. Collisional processes in the Caucasus region began 35 million years ago with the closure of the Tethys Ocean, and continues to this day. The rate of shortening between the Scythian and the Arabian plate is currently 1-2.2 mm/year. The tomography inversion used the dataset provided by several seismic agencies of the Caucasus region that contained 23,071 P- and 21,598 S-picks from 1374 events. The obtained P and S velocity models clearly delineate major tectonic units in the study area. A high velocity anomaly in Transcaucasian separating the Great and Lesser Caucasus possibly represents a rigid crustal block corresponding to the remnant oceanic lithosphere of Tethys. Another high-velocity pattern coincides with the southern edge of the Scythian Plate. Strongly deformed areas of Great and Lesser Caucasus are mostly associated with low-velocity patterns representing thickened felsic part of the crust and strong fracturing of rocks. Most Cenozoic volcanic centers of Caucasus match to the low-velocity seismic anomalies in the crust. We propose that the mantle part of the Arabian and Eurasian Plates has been delaminated due to the continental collision in the Caucasus region. As a result, overheated asthenosphere appeared nearly the bottom of the crust and facilitated melting of the crustal material that caused the origin of recent volcanism in Great and Lesser Caucasus. The Kachchh province, in contrast to the Caucasus, is far from any boundaries of major lithospheric plates. However, this area is one of the most seismically active in India. It is suggested that it may be a site of the lithosphere rupture and

  8. Influence of meteorological parameters on the soil radon (Rn222) emanation in Kutch, Gujarat, India.

    PubMed

    Sahoo, Sushanta Ku; Katlamudi, Madhusudhanarao; Shaji, Jerin P; Murali Krishna, K S; Udaya Lakshmi, G

    2018-02-02

    The soil radon (Rn 222 ) and thoron (Rn 220 ) concentrations recorded at Badargadh and Desalpar observatories in the Kutch region of Gujarat, India, have been analyzed to study the sources of the radon emissions, earthquake precursors, and the influence of meteorological parameters on radon emission. Radon and meteorological parameters were recorded using Radon Monitor RMT 1688-2 at these two stations. We used the radon data during February 21, 2011 to June 8, 2011, for Badargadh and March 2, 2011 to May 19, 2011, for the Desalpar station with a sampling interval of 10 min. It is observed that the radon concentrations at Desalpar varies between 781 and 4320 Bq m -3 with an average value of 2499 Bq m -3 , whereas thoron varies between 191 and 2017 Bq m -3 with an average value of 1433.69 Bq m -3 . The radon concentration at Badargadh varies between 264 and 2221 Bq m -3 with an average value of 1135.4 Bq m -3 , whereas thoron varies between 97 and 556 Bq m -3 . To understand how the meteorological parameters influence radon emanation, the radon and other meteorological parameters were correlated with linear regression analysis. Here, it was observed that radon and temperature are negatively correlated whereas radon and other two parameters, i.e., humidity and pressure are positively correlated. The cross correlogram also ascertains similar relationships between radon and other parameters. Further, the ratio between radon and thoron has been analyzed to determine the deep or shallow source of the radon emanation in the study area. These results revealed that the ratio radon/thoron enhanced during this period which indicates the deeper source contribution is prominent. Incidentally, all the local earthquakes occurred with a focal depth of 18-25 km at the lower crust in this region. We observed the rise in the concentrations of radon and the ratio radon/thoron at Badargadh station before the occurrence of the local earthquakes on 29th March 2011 (M 3

  9. Assisting community management of groundwater: Irrigator attitudes in two watersheds in Rajasthan and Gujarat, India

    NASA Astrophysics Data System (ADS)

    Varua, M. E.; Ward, J.; Maheshwari, B.; Oza, S.; Purohit, R.; Hakimuddin; Chinnasamy, P.

    2016-06-01

    The absence of either state regulations or markets to coordinate the operation of individual wells has focussed attention on community level institutions as the primary loci for sustainable groundwater management in Rajasthan and Gujarat, India. The reported research relied on theoretical propositions that livelihood strategies, groundwater management and the propensity to cooperate are associated with the attitudinal orientations of well owners in the Meghraj and Dharta watersheds, located in Gujarat and Rajasthan respectively. The research tested the hypothesis that attitudes to groundwater management and farming practices, household income and trust levels of assisting agencies were not consistent across the watersheds, implying that a targeted approach, in contrast to default uniform programs, would assist communities craft rules to manage groundwater across multiple hydro-geological settings. Hierarchical cluster analysis of attitudes held by survey respondents revealed four statistically significant discrete clusters, supporting acceptance of the hypothesis. Further analyses revealed significant differences in farming practices, household wealth and willingness to adapt across the four groundwater management clusters. In conclusion, the need to account for attitudinal diversity is highlighted and a framework to guide the specific design of processes to assist communities craft coordinating instruments to sustainably manage local aquifers described.

  10. An external evaluation of the Diarrhea Alleviation through Zinc and ORS Treatment (DAZT) program in Gujarat and Uttar Pradesh, India.

    PubMed

    Lamberti, Laura M; Taneja, Sunita; Mazumder, Sarmila; LeFevre, Amnesty; Black, Robert E; Walker, Christa L Fischer

    2015-12-01

    To address inadequate coverage of oral rehydration salts (ORS) and zinc supplements for the treatment of diarrhea among children under-five, the Diarrhea Alleviation through Zinc and ORS Treatment (DAZT) program was carried out from 2011-2013 in Gujarat and from 2011-2014 in Uttar Pradesh (UP), India. The program focused on improving the diarrhea treatment practices of public and private sector providers. We conducted cross-sectional household surveys in program districts at baseline and endline and constructed state-specific logistic regression models with generalized estimating equations to assess changes in ORS and zinc treatment during the program period. Between baseline and endline, zinc coverage increased from 2.5% to 22.4% in Gujarat and from 3.1% to 7.0% in UP; ORS coverage increased from 15.3% to 39.6% in Gujarat but did not change in UP. In comparison to baseline, children with diarrhea in the two-weeks preceding the endline survey had higher odds of receiving zinc treatment in both Gujarat (odds ratio, OR = 11.2; 95% confidence interval (CI) 6.4-19.3) and UP (OR = 2.4; 95% CI 1.4-3.9), but the odds of receiving ORS only increased in Gujarat (OR = 3.6; 95% CI 2.7-4.8; UP OR = 0.9; 95% CI 0.7-1.2). Seeking care outside the home, especially from a public sector source, was associated with higher odds of receiving ORS and zinc. During the duration of the DAZT program, there were modest improvements in the treatment of diarrhea among young children. Future programs should build upon and accelerate this trend with continued investment in public and private sector provider training and supply chain sustainability, in addition to targeted caregiver demand generation activities.

  11. Dominance of cyanobacterial and cryptophytic assemblage correlated to CDOM at heavy metal contamination sites of Gujarat, India.

    PubMed

    Patidar, Shailesh Kumar; Chokshi, Kaumeel; George, Basil; Bhattacharya, Sourish; Mishra, Sandhya

    2015-01-01

    Industrial clusters of Gujarat, India, generate high quantity of effluents which are received by aquatic bodies such as estuary and coastal water. In the present study, microalgal assemblage, heavy metals, and physico-chemical variables were studied from different habitats. Principal component analysis revealed that biovolume of cyanobacterial and cryptophytic community positively correlated with the heavy metal concentration (Hg, As, Zn, Fe, Mo, Ni, and Co) and chromophoric dissolved organic matter (CDOM) under hypoxic environment. Green algae and diatoms dominated at comparatively lower nitrate concentration which was positively associated with Pb and Mn.

  12. Establishing the reference value for “timed up-and-go” test in healthy adults of Gujarat, India

    PubMed Central

    Khant, Nency; Dani, Vyoma Bharat; Patel, Purvi; Rathod, Rachana

    2018-01-01

    CONTEXT: Timed up-and-go (TUG) test is a valid, reliable, and an objective test for quantifying functional mobility and assessing the fall risk in all age groups. The analysis of patient scores on TUG test is limited by lack of data, having a wide range of performance scores among people without disabilities. AIM: The objective of the study was to provide the reference value for TUG test in healthy individuals of Gujarat, India. SUBJECTS AND METHODS: It was a cross-sectional observational study. Five hundred and twenty healthy individuals, aged 40–70 years, were recruited from various regions of Gujarat based on convenient sampling. All the participants were made to perform TUG test in a controlled environment in community. Three readings of the actual test were obtained and averaged. RESULTS: Data were analyzed with mean, standard deviation, confidence intervals (CIs 95%) and Pearson's correlation coefficient (r) with α = 0.05 by age groups (40–50, 51–60, and 61–70 years) and gender. The mean (CI 95%) TUG time for healthy adults of Gujarat was 8.46 (8.35–8.57) s and demonstrated age-related decline for both male and female participants. TUG time also demonstrated strong correlation with the height of individuals. CONCLUSION: This preliminary data can be used as a reference only for specific population with specific age groups due to variability in test results among the different population due to age, gender, anthropometric measures such as height, weight, and body mass index, geographical variation, nutritional support, and cognitive status.

  13. Barriers to Real-Time Medical Direction via Cellular Communication for Prehospital Emergency Care Providers in Gujarat, India.

    PubMed

    Lindquist, Benjamin; Strehlow, Matthew C; Rao, G V Ramana; Newberry, Jennifer A

    2016-07-08

    Many low- and middle-income countries depend on emergency medical technicians (EMTs), nurses, midwives, and layperson community health workers with limited training to provide a majority of emergency medical, trauma, and obstetric care in the prehospital setting. To improve timely patient care and expand provider scope of practice, nations leverage cellular phones and call centers for real-time online medical direction. However, there exist several barriers to adequate communication that impact the provision of emergency care. We sought to identify obstacles in the cellular communication process among GVK Emergency Management and Research Institute (GVK EMRI) EMTs in Gujarat, India. A convenience sample of practicing EMTs in Gujarat, India were surveyed regarding the barriers to call initiation and completion. 108 EMTs completed the survey. Overall, ninety-seven (89.8%) EMTs responded that the most common reason they did not initiate a call with the call center physician was insufficient time. Forty-six (42%) EMTs reported that they were unable to call the physician one or more times during a typical workweek (approximately 5-6 twelve-hour shifts/week) due to their hands being occupied performing direct patient care. Fifty-eight (54%) EMTs reported that they were unable to reach the call center physician, despite attempts, at least once a week. This study identified multiple barriers to communication, including insufficient time to call for advice and inability to reach call center physicians. Identification of simple interventions and best practices may improve communication and ensure timely and appropriate prehospital care.

  14. Metagenomic sequence of saline desert microbiota from wild ass sanctuary, Little Rann of Kutch, Gujarat, India.

    PubMed

    Patel, Rajesh; Mevada, Vishal; Prajapati, Dhaval; Dudhagara, Pravin; Koringa, Prakash; Joshi, C G

    2015-03-01

    We report Metagenome from the saline desert soil sample of Little Rann of Kutch, Gujarat State, India. Metagenome consisted of 633,760 sequences with size 141,307,202 bp and 56% G + C content. Metagenome sequence data are available at EBI under EBI Metagenomics database with accession no. ERP005612. Community metagenomics revealed total 1802 species belonged to 43 different phyla with dominating Marinobacter (48.7%) and Halobacterium (4.6%) genus in bacterial and archaeal domain respectively. Remarkably, 18.2% sequences in a poorly characterized group and 4% gene for various stress responses along with versatile presence of commercial enzyme were evident in a functional metagenome analysis.

  15. First Report of Microfaunal Remains from Lignitic Sequences of Bhavnagar Lignite Mine (khadsaliya Formation), Gujarat, India: Implication to Depositional Environments and Age

    NASA Astrophysics Data System (ADS)

    Maurya, A. S.

    2016-12-01

    FIRST REPORT OF MICROFAUNAL REMAINS FROM LIGNITIC SEQUENCES OF BHAVNAGAR LIGNITE MINE (KHADSALIYA FORMATION), GUJARAT, INDIA: IMPLICATION TO DEPOSITIONAL ENVIRONMENTS AND AGEABHAYANAND SINGH MAURYA1*, SANJAY KUMAR VERMA1, PRAGYA PANDEY11Department of Earth Sciences, Indian Institute of Technology Roorkee, Roorkee Moderately preserved fish otoliths, fish vertebra, bivalves, pteropods, ostracods and foraminifereral remains were recovered from the grey to greenish-grey clays of Khadsaliya Formation, Bhavnagar Lignite Mine (western India) and quantitatively analyzed to understand the depositional environment. The bio-facies assemblage is diverse and dominated by fauna Fishes, Bivalve, Pteropods and with rare occurrences of Ostracoda and Foraminifera. Fish fauna includes otoliths represented by Ambassidarum, Apogonidarum, Percoideorum and Gobiidarum vastani, out of which Gobiidarum vastani is possibly representing Ypresian (early Eocene). The Globanomalina ovalis a smaller planktic foraminifer is known to be a very short ranged species corresponds to Planktic Foranimiferal Zone 5 to 6 (P5-P6) i.e late Thanetian to early Yepresian. Presence of both fresh water (Lepisosteus, Osteoglossidae), fresh water (Cypridopsis) ostracods and shallow marine fauna (Enchodus, Egertonia and Stephanodus) of fish vertebra; (Cardita) bivalve, , marine water (Globanomalina, Eggrella, Pyrulinoides) foraminifer suggests that Bhavnagar lignite mine have an assemblage of admixed fauna and rocks of Khaldsiya formation at Bhavnagar Lignite mine deposited under marine transgressive-regressive cycles. Some of the microfauna from Bhavnagar lignite mine show close affinities with microfaunal assemblages of the Vastan lignite mine of Gujarat, India which is stated to be of Ypresian (early Eocene).

  16. Communal violence in Gujarat, India: impact of sexual violence and responsibilities of the health care system.

    PubMed

    Khanna, Renu

    2008-05-01

    Situations of chronic conflict across the globe make it imperative to draw attention to its gendered health consequences, particularly the violation of women's reproductive and sexual rights. Since early 2002 in Gujarat, western India, the worst kind of state-sponsored violence against Muslims has been perpetrated, which continues to this day. This paper describes the history of that violence and highlights the mental and physical consequences of sexual and gender-based violence and the issues that need to be addressed by the police, the health care system and civil society. It draws upon several reports, including from the International Initiative for Justice and the Medico Friend Circle, which documented the reproductive, sexual and mental health consequences of the violence in Gujarat, and the lacunae in the responses of the health system. The paper calls for non-discrimination to be demonstrated by health personnel in the context of conflict and social unrest. Their training should include conflict as a public health problem, their roles and responsibilities in prevention, treatment and documentation of this "disease", and focus on relevant medico-legal methodology and principles, the psychological impact of sexual assault on victims, and the legal significance of medical evidence in these cases.

  17. Mafic/Ultramafic xenoliths from Saurashtra peninsula of Gujarat; northwestern Deccan Trap, India

    NASA Astrophysics Data System (ADS)

    Naushad, M.; Behera, J. R.; Chakra, M.; Murthy, P. V.

    2017-12-01

    The crustal growth forming processes at the crust-mantle interface or within the crust due to magma underplating is important for the formation and emplacement of continental flood basalt and large igneous provinces. Mafic/ultramafic xenoliths from lower crust or upper mantle provide clue to characterize the underplated material and magmatic processes. Earlier study of ultramafic xenoliths suggested magma underplating and crustal growth in Kuchchh, Gujarat, northwestern Deccan Trap (NWDT). Absence of such xenoliths in Saurashtra peninsula (SP) of NWDT however could not supplement this. Here, we report the mafic/ultramafic xenoliths entrained in high MgO basaltic lava flows of NWDT of SP in Rajkot district of Gujarat, India. The xenoliths are medium to coarse grained, meso - to melanocratic, elongated to angular pyroxenite (Type-I), two pyroxenes gabbro (Type-II) and anorthosite (Type-III) showing sharp contact with host basalt flows. Type-I xenoliths dominated by clinopyroxene (cpx) (Wo49-45 En49-38) with olivine (ol) (Fo84-78), exhibit cumulate texture, Type-II composed of cpx (core-Wo49-48 En42-41), orthopyroxene (opx) (core- En77-76 Fs23-22) and plagioclase (plag) (Ab35-28 An71-64) and Type-III, composed dominantly of plag (Ab67-29 An68-28) with minor opx (En78-76 Fs20-18) and a grain of hercynite (Al2O3=59%) in close association with plag. The basaltic lavas are porphyritic containing ol (Fo88-75), cpx (Wo50-48 En39-37), plag (Ab43-26 An74-54) and opaques. Whole rock geochemical data of xenolith entrained lava flows indicates high MgO (10-11 wt%) with high Ni (421-430 ppm) and Cr (795-1076 ppm). The equilibration temperature calculated from cpx - opx (adjacent grain of cpx and opx, pair-A; inclusion of cpx within opx, pair-B) for Type-II xenolith indicates 778°C and 789°C (pair-A) and 821°C and 832°C (pair-B) at 5 kbar and 10 kbar pressure respectively. Present study suggests that the possibility of magma underplating at crust-mantle interface or presence

  18. Issues and challenges in recruitment for government doctors in Gujarat, India.

    PubMed

    Purohit, Bhaskar; Martineau, Tim

    2016-07-19

    India faces a critical shortage of government doctors in rural and underserved areas. Several measures have been introduced to address the shortage, but significant problems still remain. The main aim of the current research was to understand the existing recruitment-related policies and systems in place for government doctors in Gujarat and to identify issues that prevent effective recruitment of doctors that could have implications for doctors' shortage in the state. The research also aims to fill the knowledge gap in the existing literature on why recruitment in civil services is an important HR function to address the shortage of doctors. The study aimed at identifying the existing recruitment policies and practices for government Medical Officers (MOs) from Gujarat state in India. The analysis is based on document review to understand the existing policies, 19 in-depth interviews with MOs to understand the systems in place for recruitment of MOs, construction of job histories from interviews to understand various nuances in the recruitment system and five interviews with Key Informants to understand recruitment policies and their actual implementation. Thematic framework approach was used to analyse qualitative data using NVivo. While the state has general recruitment guidelines called the Recruitment Rules (RRs), these rules are very wide-ranging and fragmented. The MOs were neither briefed about them nor received copies of the rules at any time during the service suggesting that RRs were not transparent. The recruitment system was considered to be slow and very sporadic having possible implications for attraction and retention of MOs. The study results indicate several other system inefficiencies such as a long time taken by the health department to provide salary benefits and service regularization that has a negative effect over MOs' motivation. The study also found unequal opportunities presented to different categories of MOs in relation to job security

  19. Golden roots to golden fruits of mental health in Gujarat.

    PubMed

    Mehta, Ritambhara; Shah, Anil; Vankar, G K; Chauhan, Ajay; Bakre, Ravindra

    2018-02-01

    Through the behavioral descriptions in age-old texts it is obvious that Mental Health problems exist since the existence of Homo Sapiens and humanity, with ever changing norms, contexts, definitions and hence their management. Gujarat state of India is one of the oldest land plateaus existing. It has been inhabited, ruled and governed by many different people, races, kings; and invaded through its longest sea-coast by Dutch, Portuguese, British. Even after freedom of India in 1947, Gujarat emerged as a separate state in 1960 only. The history of Mental Health, before being a separate state, could be summed up in 2 Mental Hospitals started by British governance and 2 very unique institutions. Post NMHP, there has been a tremendous growth in the sector, supported by many leaders in the governance. This is an attempt to review some documented and some gathered information from dependable sources, from pre-independence colonial era, post-independence and post-statehood contemporary period.

  20. The Mw 7.7 Bhuj earthquake: Global lessons for earthquake hazard in intra-plate regions

    USGS Publications Warehouse

    Schweig, E.; Gomberg, J.; Petersen, M.; Ellis, M.; Bodin, P.; Mayrose, L.; Rastogi, B.K.

    2003-01-01

    The Mw 7.7 Bhuj earthquake occurred in the Kachchh District of the State of Gujarat, India on 26 January 2001, and was one of the most damaging intraplate earthquakes ever recorded. This earthquake is in many ways similar to the three great New Madrid earthquakes that occurred in the central United States in 1811-1812, An Indo-US team is studying the similarities and differences of these sequences in order to learn lessons for earthquake hazard in intraplate regions. Herein we present some preliminary conclusions from that study. Both the Kutch and New Madrid regions have rift type geotectonic setting. In both regions the strain rates are of the order of 10-9/yr and attenuation of seismic waves as inferred from observations of intensity and liquefaction are low. These strain rates predict recurrence intervals for Bhuj or New Madrid sized earthquakes of several thousand years or more. In contrast, intervals estimated from paleoseismic studies and from other independent data are significantly shorter, probably hundreds of years. All these observations together may suggest that earthquakes relax high ambient stresses that are locally concentrated by rheologic heterogeneities, rather than loading by plate-tectonic forces. The latter model generally underlies basic assumptions made in earthquake hazard assessment, that the long-term average rate of energy released by earthquakes is determined by the tectonic loading rate, which thus implies an inherent average periodicity of earthquake occurrence. Interpreting the observations in terms of the former model therefore may require re-examining the basic assumptions of hazard assessment.

  1. Effect of Chiranjeevi Yojana on institutional deliveries and neonatal and maternal outcomes in Gujarat, India: a difference-in-differences analysis.

    PubMed

    Mohanan, Manoj; Bauhoff, Sebastian; La Forgia, Gerard; Babiarz, Kimberly Singer; Singh, Kultar; Miller, Grant

    2014-03-01

    To evaluate the effect of the Chiranjeevi Yojana programme, a public-private partnership to improve maternal and neonatal health in Gujarat, India. A household survey (n = 5597 households) was conducted in Gujarat to collect retrospective data on births within the preceding 5 years. In an observational study using a difference-in-differences design, the relationship between the Chiranjeevi Yojana programme and the probability of delivery in health-care institutions, the probability of obstetric complications and mean household expenditure for deliveries was subsequently examined. In multivariate regressions, individual and household characteristics as well as district and year fixed effects were controlled for. Data from the most recent District Level Household and Facility Survey (DLHS-3) wave conducted in Gujarat (n = 6484 households) were used in parallel analyses. Between 2005 and 2010, the Chiranjeevi Yojana programme was not associated with a statistically significant change in the probability of institutional delivery (2.42 percentage points; 95% confidence interval, CI: -5.90 to 10.74) or of birth-related complications (6.16 percentage points; 95% CI: -2.63 to 14.95). Estimates using DLHS-3 data were similar. Analyses of household expenditures indicated that mean household expenditure for private-sector deliveries had either not fallen or had fallen very little under the Chiranjeevi Yojana programme. The Chiranjeevi Yojana programme appears to have had no significant impact on institutional delivery rates or maternal health outcomes. The absence of estimated reductions in household spending for private-sector deliveries deserves further study.

  2. Faculty perceptions of the strengths, weaknesses and future prospects of the current medical undergraduate experimental physiology curriculum in Gujarat, India.

    PubMed

    Paralikar, Swapnil; Shah, Chinmay

    2015-01-01

    Over the past several years, an opinion has emerged in India that the current practical curricula in medical schools fail to meet many of the objectives for which they were instituted. Hence, this study has assessed the perception of physiology faculty members regarding the current experimental physiology curriculum in one Indian state, Gujarat. The faculty were of the opinion that many of the topics currently taught in experimental physiology (amphibian nerve-muscle and heart muscle experiments) were outdated and clinically irrelevant: Therefore, the faculty advocated that duration of teaching time devoted to some of these topics should be reduced and topics with clinical relevance should be introduced at the undergraduate level. The faculty also felt that more emphasis should be laid on highlighting the clinical aspect related to each concept taught in experimental physiology . Moreover, a majority of faculty members were in favour of replacing the current practice in Gujarat of teaching experimental physiology only by explanation of graphs obtained from experiments conducted in the previous years, with computer assisted learning in small groups.

  3. Earthquake Damage Assessment Using Very High Resolution Satelliteimagery

    NASA Astrophysics Data System (ADS)

    Chiroiu, L.; André, G.; Bahoken, F.; Guillande, R.

    Various studies using satellite imagery were applied in the last years in order to assess natural hazard damages, most of them analyzing the case of floods, hurricanes or landslides. For the case of earthquakes, the medium or small spatial resolution data available in the recent past did not allow a reliable identification of damages, due to the size of the elements (e.g. buildings or other structures), too small compared with the pixel size. The recent progresses of remote sensing in terms of spatial resolution and data processing makes possible a reliable damage detection to the elements at risk. Remote sensing techniques applied to IKONOS (1 meter resolution) and IRS (5 meters resolution) imagery were used in order to evaluate seismic vulnerability and post earthquake damages. A fast estimation of losses was performed using a multidisciplinary approach based on earthquake engineering and geospatial analysis. The results, integrated into a GIS database, could be transferred via satellite networks to the rescue teams deployed on the affected zone, in order to better coordinate the emergency operations. The methodology was applied to the city of Bhuj and Anjar after the 2001 Gujarat (India) Earthquake.

  4. Perceptions regarding barriers and facilitators to combination antiretroviral therapy adherence among people living with HIV/AIDS in Gujarat, India: A qualitative study

    PubMed Central

    Patel, Sangita; Baxi, Rajendra K.; Patel, Shilpa N.; Golin, Carol E; Mehta, Mansi; Bakshi, Harsh; Shingrapure, Kalpita; Modi, Ekta; Coonor, Priyanka; Mehta, Kedar

    2012-01-01

    Objectives: To know the perceptions regarding barriers and facilitators to cART adherence among people living with HIV/AIDS Materials and Methods: To adapt U.S. based SAFETALK “prevention with positives” intervention to be culturally relevant in Gujarat, India in assisting PLWHA, a formative study was conducted. We conducted 30 in-depth interviews with PLWHA in the local language, assessing the experiences, perceived barriers, and facilitators to combination antiretroviral therapy (cART) among PLWHA in Gujarat. PLWHA were selected from the Voluntary Counseling and Testing Centre (VCTC) in Gujarat. To triangulate interview findings, we conducted two focus group discussions (FGDs) with medical and non-medical providers, respectively. Results: Travel and commuting to clinic, fear of possible physical reactions, high cost of ART from private practitioners, CD4 count being in normal limits and resistance to medication acted as barriers to cART adherence. Initiation of cART was facilitated by family members′ suggestion, advice of treating doctors and counselors, appropriate counseling before starting cART, belief that cART would aid in living a better and longer life and due to lowering of the CD4 count. Interpretation and Conclusions: Our study suggests that several issues need to be considered when providing cART. Further research is needed to study interactions between patients and their health care providers. PMID:23188935

  5. Inequity in maternal health care service utilization in Gujarat: analyses of district-level health survey data

    PubMed Central

    Saxena, Deepak; Vangani, Ruchi; Mavalankar, Dileep V.; Thomsen, Sarah

    2013-01-01

    Background Two decades after the launch of the Safe Motherhood campaign, India still accounts for at least a quarter of maternal death globally. Gujarat is one of the most economically developed states of India, but progress in the social sector has not been commensurate with economic growth. The purpose of this study was to use district-level data to gain a better understanding of equity in access to maternal health care and to draw the attention of the policy planers to monitor equity in maternal care. Methods Secondary data analyses were performed among 7,534 ever-married women who delivered since January 2004 in the District Level Household and Facility Survey (DLHS-3) carried out during 2007–2008 in Gujarat, India. Based on the conceptual framework designed by the Commission on the Social Determinants of Health, associations were assessed between three outcomes – Institutional delivery, antenatal care (ANC), and use of modern contraception – and selected intermediary and structural determinants of health using multiple logistic regression. Results Inequities in maternal health care utilization persist in Gujarat. Structural determinants like caste group, wealth, and education were all significantly associated with access to the minimum three antenatal care visits, institutional deliveries, and use of any modern method of contraceptive. There is a significant relationship between being poor and access to less utilization of ANC services independent of caste category or residence. Discussion and conclusions Poverty is the most important determinant of non-use of maternal health services in Gujarat. In addition, social position (i.e. caste) has a strong independent effect on maternal health service use. More focused and targeted efforts towards these disadvantaged groups needs to be taken at policy level in order to achieve targets and goals laid out as per the MDGs. In particular, the Government of Gujarat should invest more in basic education and

  6. Inequity in maternal health care service utilization in Gujarat: analyses of district-level health survey data.

    PubMed

    Saxena, Deepak; Vangani, Ruchi; Mavalankar, Dileep V; Thomsen, Sarah

    2013-03-06

    Two decades after the launch of the Safe Motherhood campaign, India still accounts for at least a quarter of maternal death globally. Gujarat is one of the most economically developed states of India, but progress in the social sector has not been commensurate with economic growth. The purpose of this study was to use district-level data to gain a better understanding of equity in access to maternal health care and to draw the attention of the policy planers to monitor equity in maternal care. Secondary data analyses were performed among 7,534 ever-married women who delivered since January 2004 in the District Level Household and Facility Survey (DLHS-3) carried out during 2007-2008 in Gujarat, India. Based on the conceptual framework designed by the Commission on the Social Determinants of Health, associations were assessed between three outcomes - Institutional delivery, antenatal care (ANC), and use of modern contraception - and selected intermediary and structural determinants of health using multiple logistic regression. Inequities in maternal health care utilization persist in Gujarat. Structural determinants like caste group, wealth, and education were all significantly associated with access to the minimum three antenatal care visits, institutional deliveries, and use of any modern method of contraceptive. There is a significant relationship between being poor and access to less utilization of ANC services independent of caste category or residence. Poverty is the most important determinant of non-use of maternal health services in Gujarat. In addition, social position (i.e. caste) has a strong independent effect on maternal health service use. More focused and targeted efforts towards these disadvantaged groups needs to be taken at policy level in order to achieve targets and goals laid out as per the MDGs. In particular, the Government of Gujarat should invest more in basic education and infrastructural development to begin to remove the structural causes

  7. Seismic Velocity Assessment In The Kachchh Region, India, From Multiple Waveform Functionals

    NASA Astrophysics Data System (ADS)

    Ghosh, R.; Sen, M. K.; Mandal, P.; Pulliam, J.; Agrawal, M.

    2014-12-01

    The primary goal of this study is to estimate well constrained crust and upper mantle seismic velocity structure in the Kachchh region of Gujarat, India - an area of active interest for earthquake monitoring purposes. Several models based on 'stand-alone' surface wave dispersion and receiver function modeling exist in this area. Here we jointly model the receiver function, surface wave dispersion and, S and shear-coupled PL wavetrains using broadband seismograms of deep (150-700 km), moderate to-large magnitude (5.5-6.8) earthquakes recorded teleseismically at semi-permanent seismograph stations in the Kachchh region, Gujarat, India. While surface wave dispersion and receiver function modeling is computationally fast, full waveform modeling makes use of reflectivity synthetic seismograms. An objective function that measures misfit between all three data is minimized using a very fast simulated annealing (VFSA) approach. Surface wave and receiver function data help reduce the model search space which is explored extensively for detailed waveform fitting. Our estimated crustal and lithospheric thicknesses in this region vary from 32 to 41 km and 70 to 80 km, respectively, while crustal P and S velocities from surface to Moho discontinuity vary from 4.7 to 7.0 km/s and 2.7 to 4.1 km/s, respectively. Our modeling clearly reveals a zone of crustal as well as an asthenospheric upwarping underlying the Kachchh rift zone relative to the surrounding unrifted area. We believe that this feature plays a key role in the seismogenesis of lower crustal earthquakes occurring in the region through the emanation of volatile CO2 into the hypocentral zones liberating from the crystallization of carbonatite melts in the asthenosphere. Such a crust-mantle structure might be related to the plume-lithosphere interaction during the Deccan/Reunion plume episode (~65 Ma).

  8. Diarrhea no more: does zinc help the poor? Evidence on the effectiveness of programmatic efforts to reach poorest in delivering zinc and ORS at scale in UP and Gujarat, India.

    PubMed

    LeFevre, Amnesty E; Mohan, Diwakar; Mazumder, Sarmila; Lamberti, Laura L; Taneja, Sunita; Black, Robert E; Fischer-Walker, Christa L

    2016-12-01

    India has the greatest burden of diarrhea in children under 5 years globally. The Diarrhea Alleviation through zinc and oral rehydration salts (ORS) Therapy program (2010-2014) sought to improve access to and utilization of zinc and ORS among children 2-59 months in Gujarat and Uttar Pradesh (UP), India, through public and private sector delivery channels. In this analysis, we present findings on program's effect in reducing child-health inequities. Data from cross-sectional baseline and endline surveys were used to assess disparities in key outcomes across six dimensions: socioeconomic strata, gender, caregiver education, ethnicity and geography. Careseeking outside the home for children under 5 years with diarrhea did not increase significantly in UP or Gujarat across socioeconomic strata. Declines in private sector careseeking were observed in both sites along with concurrent increases in public sector careseeking. Zinc, ORS, zinc+ORS use did not increase significantly in UP across socioeconomic strata. In Gujarat, increases in zinc use (20% overall; 33% in the Quintile 5 (Q5) strata) and zinc+ORS (18% overall; 30% in the Q5 strata) were disproportionately observed in the high income strata, among members of the most advantaged caste, and among children whose mothers had ≥1 year of schooling. ORS use increased significantly across all socioeconomic strata for children in Gujarat with diarrhea (23% overall; 33% in Q5 strata) and those with dehydration + diarrhea (33% overall; 38% in Q5 strata). The magnitude of increase in ORS receipt from the public sector was nearly twice that observed in the private sector. In Gujarat, while out of pocket spending for diarrhea was significantly higher for male children, overall costs to users declined by a mean of US$ 2; largely due to significant reductions in wages lost (-US$ 0.79; P  < 0.003), and transportation costs (-US$ 0.44; P  < 0.00). While significant improvements in diarrhea treatment were achieved in

  9. Health system capacity: maternal health policy implementation in the state of Gujarat, India

    PubMed Central

    Sanneving, Linda; Kulane, Asli; Iyer, Aditi; Ahgren, Bengt

    2013-01-01

    Introduction The Government of Gujarat has for the past couple of decades continuously initiated several interventions to improve access to care for pregnant and delivering women within the state. Data from the last District Family Heath survey in Gujarat in 2007–2008 show that 56.4% of women had institutional deliveries and 71.5% had at least one antenatal check-up, indicating that challenges remain in increasing use of and access to maternal health care services. Objective To explore the perceptions of high-level stakeholders on the process of implementing maternal health interventions in Gujarat. Method Using the policy triangle framework developed by Walt and Gilson, the process of implementation was approached using in-depth interviews and qualitative content analysis. Result Based on the analysis, three themes were developed: lack of continuity; the complexity of coordination; and lack of confidence and underutilization of the monitoring system. The findings suggest that decisions made and actions advocated and taken are more dependent on individual actors than on sustainable structures. The findings also indicate that the context in which interventions are implemented is challenged in terms of weak coordination and monitoring systems that are not used to evaluate and develop interventions on maternal health. Conclusions The implementation of interventions on maternal health is dependent on the capacity of the health system to implement evidence-based policies. The capacity of the health system in Gujarat to facilitate implementation of maternal health interventions needs to be improved, both in terms of the role of actors and in terms of structures and processes. PMID:23522352

  10. Role stress among auxiliary nurses midwives in Gujarat, India.

    PubMed

    Purohit, Bhaskar; Vasava, Paul

    2017-01-23

    Understanding Role Stress is important as health service providers, especially nurses experience high levels of Role Stress which is linked to burnout, poor quality of care and high turnover. The current study explicates the concept of Role Stress and assesses the Role Stress experienced by the Auxiliary Nurse Midwives (ANMs) working with rural government health centres from Gujarat, India. The study included 84 ANMs working with government health centres from one district in India. A structured instrument with established reliability and validity was used to measure 10 dimensions of Role Stress namely: Inter-role distance, role stagnation, role expectation conflict, role erosion: role overload, role isolation, personal inadequacy, self-role distance, role ambiguity and resource inadequacy. The study instrument was based on 5 point Likert rating scale that contained 50 unidirectional negative statements, 5 for each dimension. Kolmogorov-Smirnov and Shapiro-Wilk test were carried out to assess if the data were normally distributed. Cronbach's alpha test was carried out to assess reliability of the instrument. The study data was analyzed using descriptive statistics mainly using mean scores with higher scores indicating higher Role Stress and vice versa. The data was analyzed using SPSS version 19. Kolmogorov-Smirnov and Shapiro-Wilk test indicated that the data were normally distributed. Cronbach's alpha test indicated values of 0.852 suggesting high reliability of the tool. The highest Role Stress among ANMs was experienced for resource inadequacy. Role overload, role stagnation and inter-role distance were among the other important role stressors for ANMs. The study results suggests that ANMs frequently feel that: they do not have adequate amount of resources, facilities and financial support from the high levels authorities; people have too many expectations from their roles and as result they are overloaded with work and have very limited opportunities for

  11. Assessment of water quality index of bore well water samples from some selected locations of South Gujarat, India.

    PubMed

    Tripathi, S; Patel, H M; Srivastava, P K; Bafna, A M

    2013-10-01

    The present study calculates the water quality index (WQI) of some selected sites from South Gujarat (India) and assesses the impact of industries, agriculture and human activities. Chemical parameters were monitored for the calculation of WQI of some selected bore well samples. The results revealed that the WQI of the some bore well samples exceeded acceptable levels due to the dumping of wastes from municipal, industrial and domestic sources and agricultural runoff as well. Inverse Distance Weighting (IDW) was implemented for interpolation of each water quality parameter (pH, EC, alkalinity, total hardness, chloride, nitrate and sulphate) for the entire sampled area. The bore water is unsuitable for drinking and if the present state of affairs continues for long, it may soon become an ecologically dead bore.

  12. SRTM Stereo Pair: Bhuj, India, Two Weeks After Earthquake

    NASA Image and Video Library

    2001-04-05

    On January 26, 2001, the city of Bhuj suffered the most deadly earthquake in India history. This stereoscopic image was generated from NASA Landsat satellite and data from Shuttle Radar Topography Mission SRTM.

  13. Intimate partner violence and physical and mental health among women utilizing community health services in Gujarat, India.

    PubMed

    Kamimura, Akiko; Ganta, Vikas; Myers, Kyl; Thomas, Tomi

    2014-10-16

    Intimate partner violence (IPV) is a significant public health threat which causes injury and acute and chronic physical and mental health problems. In India, a high percentage of women experience IPV. The purposes of this study include 1) to describe the lifetime prevalence of IPV, and 2) to examine the association between IPV and physical and mental health well-being, among women utilizing community health services for the economically disadvantaged in India. Women utilizing community health services (N = 219) aged between 18 and 62 years completed a self-administered survey in Gujarat, India. Standardized instruments were used to measure perceived physical and mental health well-being. In addition, participants were asked about their lifetime experience with IPV, and socio-demographic questions. Analysis was restricted to the ever-married participants who completed the questions on IPV (N = 167). Participants with a lifetime history of IPV were more likely to have reported poorer physical and mental health compared to those without a lifetime history of IPV. More than half of the participants with an IPV history experienced multiple types of IPV (physical, sexual and/or emotional IPV). While being in the highest caste was a significant positive factor associated with better health, caste and other socio-demographic factors were not associated with IPV. Women in India face risk of IPV. Yet those experiencing IPV do not seek help or rely on informal help sources. Community health organizations may take a role in IPV prevention and intervention. Diversity of intervention options would be important to encourage more women with IPV experience to seek help.

  14. Initial posting-a critical stage in the employment cycle: lessons from the experience of government doctors in Gujarat, India.

    PubMed

    Purohit, Bhaskar; Martineau, Tim

    2016-07-11

    With the critical shortage of government doctors serving in rural health centers in India, understanding the initial posting policies, processes, and practices become important from a retention point of view. The initial posting is a very critical stage of an employment cycle and could play an important role in influencing the key human resource for health outcomes such as turnover and performance. The current study aimed at exploring a rather unknown phenomenon of the initial posting-related processes, practices, and perceptions of Medical Officers working with the Public Health Department in Gujarat, India. This was an exploratory study carried out in the state of Gujarat, India, that used qualitative methods first to document the extant initial posting policy with the help of document review and five Key Informant interviews; next, 19 in-depth interviews were carried out with Medical Officers to assess implementation of policies as well as processes and systems related to the initial posting of Medical Officers. A thematic framework approach was used to analyze qualitative data using NVIVO. The results indicate that there is no formal published or written initial posting policy in the state, and in the absence of a written and formal policy, the overall posting systems were perceived to be arbitrary by the study respondents. In the absence of any policy, the state has some unwritten informal practices such as posting the Medical Officers at their native places. Although this practice reflects a concern towards the Medical Officer's needs, such practices are not consistently applied indicating some inequity and possible implications over Medical Officers' retention and motivation. Initial posting is a critical aspect of an employment cycle, and the perceptions and experiences of MOs regarding the processes and practices involved in their initial posting can be crucial in influencing their performance and turnover rates. If long-term solutions are to be sought in

  15. Maternal healthcare financing: Gujarat's Chiranjeevi Scheme and its beneficiaries.

    PubMed

    Bhat, Ramesh; Mavalankar, Dileep V; Singh, Prabal V; Singh, Neelu

    2009-04-01

    Maternal mortality is an important public-health issue in India, specifically in Gujarat. Contributing factors are the Government's inability to operationalize the First Referral Units and to provide an adequate level of skilled birth attendants, especially to the poor. In response, the Gujarat state has developed a unique public-private partnership called the Chiranjeevi Scheme. This scheme focuses on institutional delivery, specifically emergency obstetric care for the poor. The objective of the study was to explore the targeting of the scheme, its coverage, and socioeconomic profile of the beneficiaries and to assess financial protection offered by the scheme, if any, in Dahod, one of the initial pilot districts of Gujarat. A household-level survey of beneficiaries (n=262) and non-users (n=394) indicated that the scheme is well-targeted to the poor but many poor people do not use the services. The beneficiaries saved more than Rs 3000 (US$ 75) in delivery-related expenses and were generally satisfied with the scheme. The study provided insights on how to improve the scheme further. Such a financing scheme could be replicated in other states and countries to address the cost barrier, especially in areas where high numbers of private specialists are available.

  16. Multifractal analysis of 2001 Mw 7 . 7 Bhuj earthquake sequence in Gujarat, Western India

    NASA Astrophysics Data System (ADS)

    Aggarwal, Sandeep Kumar; Pastén, Denisse; Khan, Prosanta Kumar

    2017-12-01

    The 2001 Mw 7 . 7 Bhuj mainshock seismic sequence in the Kachchh area, occurring during 2001 to 2012, has been analyzed using mono-fractal and multi-fractal dimension spectrum analysis technique. This region was characterized by frequent moderate shocks of Mw ≥ 5 . 0 for more than a decade since the occurrence of 2001 Bhuj earthquake. The present study is therefore important for precursory analysis using this sequence. The selected long-sequence has been investigated first time for completeness magnitude Mc 3.0 using the maximum curvature method. Multi-fractal Dq spectrum (Dq ∼ q) analysis was carried out using effective window-length of 200 earthquakes with a moving window of 20 events overlapped by 180 events. The robustness of the analysis has been tested by considering the magnitude completeness correction term of 0.2 to Mc 3.0 as Mc 3.2 and we have tested the error in the calculus of Dq for each magnitude threshold. On the other hand, the stability of the analysis has been investigated down to the minimum magnitude of Mw ≥ 2 . 6 in the sequence. The analysis shows the multi-fractal dimension spectrum Dq decreases with increasing of clustering of events with time before a moderate magnitude earthquake in the sequence, which alternatively accounts for non-randomness in the spatial distribution of epicenters and its self-organized criticality. Similar behavior is ubiquitous elsewhere around the globe, and warns for proximity of a damaging seismic event in an area. OS: Please confirm math roman or italics in abs.

  17. Sociodemographic Correlates of Tobacco Consumption in Rural Gujarat, India

    PubMed Central

    Kahar, Payal; Misra, Ranjita; Patel, Thakor G.

    2016-01-01

    Background. The purpose of this study was to examine occupation-, education-, and gender-specific patterns of tobacco use and knowledge of its health effects among 23,953 rural Asian Indians ≥18 years in Gujarat. Methodology. A statewide, community-based, cross-sectional survey was conducted in 26 districts of Gujarat (December 2010–May 2015), using face-to-face interviews by trained community health workers called SEVAKS. Results. Mean age was 39.8 ± 15.2 years. Eighteen percent of respondents used tobacco in various forms. Tobacco consumption was significantly higher among males (32%), 18–34 years' age group (35%), those who were self-employed (72%), and those with elementary education (40%). The prevalence was 11 times higher among males than females (95% CI = 9.78, 13.13). Adjusted ORs for tobacco use showed strong gradient by age and educational level; consumption was lower among the illiterates and higher for older participants (≥55 years). Tobacco consumption also varied by occupation; that is, those who were self-employed and employed for wages were more likely to use tobacco than those who were unemployed. Knowledge of health effects of tobacco lowered the odds of consumption by 30–40%. Conclusions. Effective educational programs should be tailored by gender, to improve knowledge of health risks and dispel myths on perceived benefits of tobacco. PMID:27127788

  18. Socio-economic, Biophysical, and Perceptional Factors Associated with Agricultural Adaptation of Smallholder Farmers in Gujarat, Northwest India

    NASA Astrophysics Data System (ADS)

    Jain, M.; DeFries, R. S.

    2012-12-01

    Climate change is predicted to negatively impact many agricultural communities across the globe, particularly smallholder farmers who often do not have access to appropriate technologies to reduce their vulnerability. To better predict which farmers will be most impacted by future climate change at a regional scale, we use remote sensing and agricultural census data to examine how cropping intensity and crop type have shifted based on rainfall variability across Gujarat, India from 1990 to 2010. Using household-level interviews, we then identify the socio-economic, biophysical, perceptional, and psychological factors associated with smallholder farmers who are the most impacted and the least able to adapt to contemporaneous rainfall variability. We interviewed 750 farmers in 2011 and 2012 that span a rainfall, irrigation, socio-economic, and caste gradient across central Gujarat. Our results show that farmers shift cropping practices in several ways based on monsoon onset, which farmers state is the main observable rainfall signal influencing cropping decisions during the monsoon season. When monsoon onset is delayed, farmers opt to plant more drought-tolerant crops, push back the date of sowing, and increase the number of irrigations used. Comparing self-reported income and yields, we find that switching crops does not improve agricultural income, shifting planting date does not influence crop yield, yet increasing the number of irrigations significantly increases yield. Future work will identify which social (e.g. social networks), psychological (e.g. risk preference), and knowledge (e.g. information sources) factors are associated with farmers who are best able to adapt to rainfall variability.

  19. Post-Earthquake Reconstruction — in Context of Housing

    NASA Astrophysics Data System (ADS)

    Sarkar, Raju

    Comprehensive rescue and relief operations are always launched with no loss of time with active participation of the Army, Governmental agencies, Donor agencies, NGOs, and other Voluntary organizations after each Natural Disaster. There are several natural disasters occurring throughout the world round the year and one of them is Earthquake. More than any other natural catastrophe, an earthquake represents the undoing of our most basic pre-conceptions of the earth as the source of stability or the first distressing factor due to earthquake is the collapse of our dwelling units. Earthquake has affected buildings since people began constructing them. So after each earthquake a reconstruction of housing program is very much essential since housing is referred to as shelter satisfying one of the so-called basic needs next to food and clothing. It is a well-known fact that resettlement (after an earthquake) is often accompanied by the creation of ghettos and ensuing problems in the provision of infrastructure and employment. In fact a housing project after Bhuj earthquake in Gujarat, India, illustrates all the negative aspects of resettlement in the context of reconstruction. The main theme of this paper is to consider few issues associated with post-earthquake reconstruction in context of housing, all of which are significant to communities that have had to rebuild after catastrophe or that will face such a need in the future. Few of them are as follows: (1) Why rebuilding opportunities are time consuming? (2) What are the causes of failure in post-earthquake resettlement? (3) How can holistic planning after an earthquake be planned? (4) What are the criteria to be checked for sustainable building materials? (5) What are the criteria for success in post-earthquake resettlement? (6) How mitigation in post-earthquake housing can be made using appropriate repair, restoration, and strengthening concepts?

  20. Variability of Power from Large-Scale Solar Photovoltaic Scenarios in the State of Gujarat: Preprint

    DOE Office of Scientific and Technical Information (OSTI.GOV)

    Parsons, B.; Hummon, M.; Cochran, J.

    2014-04-01

    India has ambitious goals for high utilization of variable renewable power from wind and solar, and deployment has been proceeding at a rapid pace. The western state of Gujarat currently has the largest amount of solar generation of any Indian state, with over 855 Megawatts direct current (MWDC). Combined with over 3,240 MW of wind, variable generation renewables comprise nearly 18% of the electric-generating capacity in the state. A new historic 10-kilometer (km) gridded solar radiation data set capturing hourly insolation values for 2002-2011 is available for India. We apply an established method for downscaling hourly irradiance data to one-minutemore » irradiance data at potential PV power production locations for one year, 2006. The objective of this report is to characterize the intra-hour variability of existing and planned photovoltaic solar power generation in the state of Gujarat (a total of 1.9 gigawatts direct current (GWDC)), and of five possible expansion scenarios of solar generation that reflect a range of geographic diversity (each scenario totals 500-1,000 MW of additional solar capacity). The report statistically analyzes one year's worth of power variability data, applied to both the baseline and expansion scenarios, to evaluate diurnal and seasonal power fluctuations, different timescales of variability (e.g., from one to 15 minutes), the magnitude of variability (both total megawatts and relative to installed solar capacity), and the extent to which the variability can be anticipated in advance. The paper also examines how Gujarat Energy Transmission Corporation (GETCO) and the Gujarat State Load Dispatch Centre (SLDC) could make use of the solar variability profiles in grid operations and planning.« less

  1. Has Chiranjeevi Yojana changed the geographic availability of free comprehensive emergency obstetric care services in Gujarat, India?

    PubMed Central

    Vora, Kranti Suresh; Yasobant, Sandul; Patel, Amit; Upadhyay, Ashish; Mavalankar, Dileep V.

    2015-01-01

    Background The high rate of maternal mortality in India is of grave concern. Poor rural Indian women are most vulnerable to preventable maternal deaths primarily because they have limited availability of affordable emergency obstetric care (EmOC) within reasonable geographic proximity. Scarcity of obstetricians in the public sector combined with financial barriers to accessing private sector obstetrician services preclude this underserved population from availing lifesaving functions of comprehensive EmOC such as C-section. In order to overcome this limitation, Government of Gujarat initiated a unique public–private partnership program called Chiranjeevi Yojana (CY) in 2005. The program envisaged leveraging private sector providers to increase availability and thereby accessibility of EmOC care for vulnerable sections of society. Under CY, private sector providers render obstetric care services to poor women at no cost to patients. This paper examines the CY's effectiveness in improving availability of CEmOC services between 2006 and 2012 in three districts of Gujarat, India. Methods Primary data on facility locations, EmOC functionality, and obstetric bed availability were collected in the years 2012 and 2013 in three study districts. Secondary data from Census 2001 and 2011 were used along with required geographic information from Topo sheets and Google Earth maps. ArcGIS version 10 was used to analyze the availability of services using two-step floating catchment area (2SFCA) method. Results Our analysis suggests that the availability of CEmOC services within reasonable travel distance has greatly improved in all three study districts as a result of CY. We also show that the declining participation of the private sector did not result in an increase in distance to the nearest facility, but the extent of availability of providers for several villages was reduced. Spatial and temporal analyses in this paper provide a comprehensive understanding of trends in the

  2. Has Chiranjeevi Yojana changed the geographic availability of free comprehensive emergency obstetric care services in Gujarat, India?

    PubMed

    Vora, Kranti Suresh; Yasobant, Sandul; Patel, Amit; Upadhyay, Ashish; Mavalankar, Dileep V

    2015-01-01

    The high rate of maternal mortality in India is of grave concern. Poor rural Indian women are most vulnerable to preventable maternal deaths primarily because they have limited availability of affordable emergency obstetric care (EmOC) within reasonable geographic proximity. Scarcity of obstetricians in the public sector combined with financial barriers to accessing private sector obstetrician services preclude this underserved population from availing lifesaving functions of comprehensive EmOC such as C-section. In order to overcome this limitation, Government of Gujarat initiated a unique public-private partnership program called Chiranjeevi Yojana (CY) in 2005. The program envisaged leveraging private sector providers to increase availability and thereby accessibility of EmOC care for vulnerable sections of society. Under CY, private sector providers render obstetric care services to poor women at no cost to patients. This paper examines the CY's effectiveness in improving availability of CEmOC services between 2006 and 2012 in three districts of Gujarat, India. Primary data on facility locations, EmOC functionality, and obstetric bed availability were collected in the years 2012 and 2013 in three study districts. Secondary data from Census 2001 and 2011 were used along with required geographic information from Topo sheets and Google Earth maps. ArcGIS version 10 was used to analyze the availability of services using two-step floating catchment area (2SFCA) method. Our analysis suggests that the availability of CEmOC services within reasonable travel distance has greatly improved in all three study districts as a result of CY. We also show that the declining participation of the private sector did not result in an increase in distance to the nearest facility, but the extent of availability of providers for several villages was reduced. Spatial and temporal analyses in this paper provide a comprehensive understanding of trends in the availability of EmOC services

  3. Preliminary observations from the 3 January 2017, MW 5.6 Manu, Tripura (India) earthquake

    NASA Astrophysics Data System (ADS)

    Debbarma, Jimmi; Martin, Stacey S.; Suresh, G.; Ahsan, Aktarul; Gahalaut, Vineet K.

    2017-10-01

    On 3 January 2017, a MW 5.6 earthquake occurred in Dhalai district in Tripura (India), at 14:39:03 IST (09:09:03 UTC) with an epicentre at 24.018°N ± 4.9 km and 91.964°E ± 4.4 km, and a focal depth of 31 ± 6.0 km. The focal mechanism solution determined after evaluating data from seismological observatories in India indicated a predominantly strike-slip motion on a steeply dipping plane. The estimated focal depth and focal mechanism solution places this earthquake in the Indian plate that lies beneath the overlying Indo-Burmese wedge. As in the 2016 Manipur earthquake, a strong motion record from Shillong, India, appears to suggest site amplification possibly due to topographic effects. In the epicentral region in Tripura, damage assessed from a field survey and from media reports indicated that the macroseismic intensity approached 6-7 EMS with damage also reported in adjacent parts of Bangladesh. A striking feature of this earthquake were the numerous reports of liquefaction that were forthcoming from fluvial locales in the epicentral region in Tripura, and at anomalous distances farther north in Bangladesh. The occurrence of the 2017 Manu earthquake emphasises the hazard posed by intraplate earthquakes in Tripura and in the neighbouring Bengal basin region where records of past earthquakes are scanty or vague, and where the presence of unconsolidated deltaic sediments and poor implementation of building codes pose a significant societal and economic threat during larger earthquakes in the future.

  4. Geographic smoothing of solar PV: Results from Gujarat

    DOE PAGES

    Klima, Kelly; Apt, Jay

    2015-09-24

    We examine the potential for geographic smoothing of solar photovoltaic (PV) electricity generation using 13 months of observed power production from utility-scale plants in Gujarat, India. To our knowledge, this is the first published analysis of geographic smoothing of solar PV using actual generation data at high time resolution from utility-scale solar PV plants. We use geographic correlation and Fourier transform estimates of the power spectral density (PSD) to characterize the observed variability of operating solar PV plants as a function of time scale. Most plants show a spectrum that is linear in the log–log domain at high frequencies f,more » ranging from f -1.23 to f -1.56 (slopes of -1.23 and -1.56), thus exhibiting more relative variability at high frequencies than exhibited by wind plants. PSDs for large PV plants have a steeper slope than those for small plants, hence more smoothing at short time scales. Interconnecting 20 Gujarat plants yields a f -1.66 spectrum, reducing fluctuations at frequencies corresponding to 6 h and 1 h by 23% and 45%, respectively. Half of this smoothing can be obtained through connecting 4-5 plants; reaching marginal improvement of 1% per added plant occurs at 12-14 plants. The largest plant (322 MW) showed an f -1.76 spectrum. Furthermore, this suggests that in Gujarat the potential for smoothing is limited to that obtained by one large plant.« less

  5. Prevalence of hysterectomy among rural and urban women with and without health insurance in Gujarat, India.

    PubMed

    Desai, Sapna; Sinha, Tara; Mahal, Ajay

    2011-05-01

    This paper presents findings on hysterectomy prevalence from a 2010 cross-sectional household survey of 2,214 rural and 1,641 urban, insured and uninsured women in low-income households in Ahmedabad city and district in Gujarat, India. The study investigated why hysterectomy was a leading reason for use of health insurance by women insured by SEWA, a women's organisation that operates a community-based health insurance scheme. Of insured women, 9.8% of rural women and 5.3% of urban women had had a hysterectomy, compared to 7.2% and 4.0%, respectively, of uninsured women. Approximately one-third of all hysterectomies were in women younger than 35 years of age. Rural women used the private sector more often for hysterectomy, while urban use was almost evenly split between the public and private sectors. SEWA's community health workers suggested that such young women underwent hysterectomies due to difficulties with menstruation and a range of gynaecological morbidities. The extent of these and of unnecessary hysterectomy, as well as providers' attitudes, require further investigation. We recommend the provision of information on hysterectomy as part of community health education for women, and better provision of basic gynaecological care as areas for advocacy and action by SEWA and the public health community in India. Copyright © 2011 Reproductive Health Matters. Published by Elsevier Ltd. All rights reserved.

  6. Anomalous soil radon fluctuations - signal of earthquakes in Nepal and eastern India regions

    NASA Astrophysics Data System (ADS)

    Deb, Argha; Gazi, Mahasin; Barman, Chiranjib

    2016-12-01

    The present paper deals with pre-seismic soil radon-222 recorded at two different locations 200 m apart, at Jadavpur University main campus, Kolkata, India. Solid state nuclear track detector method is used for detection of the radioactive radon gas. Two simultaneous 4-month long time series data have been analysed. Anomalous fluctuations in the radon datasets have been observed prior to recent earthquakes in Nepal and eastern India during the monitoring period, mainly, the massive 25th April 7.8 M Nepal earthquake. The simultaneous measurements assist in identifying seismogenic radon precursor efficiently.

  7. Addressing semen loss concerns: towards culturally appropriate HIV/AIDS interventions in Gujarat, India.

    PubMed

    Lakhani, A; Gandhi, K; Collumbien, M

    2001-11-01

    A situation analysis of sexual networking and sexual health in an industrial area of Gujarat, India, identified anxiety about masturbation and other semen loss concerns as major preoccupations among young men. This paper describes how the Deepak Charitable Trust addressed these concerns in their HIV prevention programme for young men aged 15 to 30. Flowcharts were used as participatory learning tools and to obtain data on the perceived consequences of masturbation, both before and after intervention activities. Research was also done on the relation between semen-related anxieties and sexual risk behaviour by DCT and two other NGOs among young men engaging in unsafe sexual behaviour. DCT advocates addressing masturbation and other semen loss concerns in all sexual health campaigns in South Asia, based on the magnitude of these concerns, their potential to confound syndromic management of STIs and their significance as an idiom of psychosocial distress. Masturbation and associated anxieties about sexual performance are seen as health issues and discussed as such by the programme. There is immediate identification among young men, whether or not they are already sexually active, and it provides an excellent entry point for sexual health and safer sex education. The community response to these efforts has been entirely positive.

  8. Association of tomato leaf curl Gujarat virus and tomato leaf curl Bangladesh betasatellite on papaya showing typical leaf curl symptoms in North India.

    PubMed

    Varun, Priyanka; Saxena, Sangeeta

    2018-05-01

    Papaya leaf curl is an economically important disease occurring in papaya growing tropical and subtropical areas. Papaya leaf curl virus, a begomovirus, is the main causative agent for the disease, but many other begomoviruses as well as betasatellites have also been reported on papaya leaf curl disease. Rapidly evolving host range of begomoviruses is a major issue for developing successful resistance strategies against begomoviral infection considering their expanding host range and mixed infection. In our study, we have identified the presence of begomovirus and associated satellite molecule on papaya showing severe leaf curl symptoms in Lucknow, India. Analysis of complete DNA-A component of this isolate (MG757245) revealed the highest similarity (91%) with tomato leaf curl Gujarat virus (ToLCuGuV), while sequence data of betasatellite (MG478451) showed maximum (89%) identity with tomato leaf curl Bangladesh betasatellite (ToLCuBB). This is the first report on identification of ToLCuGuV and ToLCuBB coinfecting papaya plants in Lucknow, Uttar Pradesh (India).

  9. Providing skilled birth attendants and emergency obstetric care to the poor through partnership with private sector obstetricians in Gujarat, India.

    PubMed

    Singh, Amarjit; Mavalankar, Dileep V; Bhat, Ramesh; Desai, Ajesh; Patel, S R; Singh, Prabal V; Singh, Neelu

    2009-12-01

    India has the world's largest number of maternal deaths estimated at 117,000 per year. Past efforts to provide skilled birth attendants and emergency obstetric care in rural areas have not succeeded because obstetricians are not willing to be posted in government hospitals at subdistrict level. We have documented an innovative public-private partnership scheme between the Government of Gujarat, in India, and private obstetricians practising in rural areas to provide delivery care to poor women. In April 2007, the majority of poor women delivered their babies at home without skilled care. More than 800 obstetricians joined the scheme and more than 176,000 poor women delivered in private facilities. We estimate that the coverage of deliveries among poor women under the scheme increased from 27% to 53% between April and October 2007. The programme is considered very successful and shows that these types of social health insurance programmes can be managed by the state health department without help from any insurance company or international donor. At least in some areas of India, it is possible to develop large-scale partnerships with the private sector to provide skilled birth attendants and emergency obstetric care to poor women at a relatively small cost. Poor women will take up the benefit of skilled delivery care rapidly, if they do not have to pay for it.

  10. Heterogeneity in the background and earnings of nurses in India: evidence from a cross-sectional study in Gujarat.

    PubMed

    Seth, Katyayni

    2017-11-01

    It is important to understand the service conditions of nurses because these influence nurses' motivations and ability to provide care. Although nurses are estimated to constitute 30% of India's health workforce, limited empirical information is available about them. This paper attempts to address this gap in research. A cross-sectional survey of 266 nurses in the state of Gujarat was conducted to understand the demographic characteristics, qualifications and employment features of nurses working in India's private and public health sectors. Descriptive and univariate analyses were performed using the collected information. A multivariate regression model was also estimated with monthly earnings as the dependent variable, and workplace, type of employment contract, caste background and years in the nursing workforce as independent variables. The three main findings presented in this article highlight considerable heterogeneity in the background and employment of nurses in India. First, 49% of nurses working in private hospitals and as temporary employees in public facilities belonged to historically disadvantaged social groups (deemed Scheduled Castes and Scheduled Tribes) and were estimated to earn 9% less than similarly qualified and practiced nurses from general caste categories (P = 0.02). Second, 18% of nurses working in private hospitals did not have formal nursing qualifications. Third, nurses working in private hospitals and as temporary employees in public facilities earned less than the minimum wage stipulated by the Government of India. Permanent public sector nurses were estimated to earn 105% more than private sector nurses with the same qualifications, years of work and caste background (P <  0.001). This study finds that the disproportionate presence of women and socially discriminated caste groups in the nursing workforce, coupled with the failure of governmental agencies to regulate the health sector, might help explain the low wages and lack of

  11. Providing skilled birth attendants and emergency obstetric care to the poor through partnership with private sector obstetricians in Gujarat, India

    PubMed Central

    Singh, Amarjit; Bhat, Ramesh; Desai, Ajesh; Patel, SR; Singh, Prabal V; Singh, Neelu

    2009-01-01

    Abstract Problem India has the world’s largest number of maternal deaths estimated at 117 000 per year. Past efforts to provide skilled birth attendants and emergency obstetric care in rural areas have not succeeded because obstetricians are not willing to be posted in government hospitals at subdistrict level. Approach We have documented an innovative public–private partnership scheme between the Government of Gujarat, in India, and private obstetricians practising in rural areas to provide delivery care to poor women. Local setting In April 2007, the majority of poor women delivered their babies at home without skilled care. Relevant changes More than 800 obstetricians joined the scheme and more than 176 000 poor women delivered in private facilities. We estimate that the coverage of deliveries among poor women under the scheme increased from 27% to 53% between April and October 2007. The programme is considered very successful and shows that these types of social health insurance programmes can be managed by the state health department without help from any insurance company or international donor. Lessons learned At least in some areas of India, it is possible to develop large-scale partnerships with the private sector to provide skilled birth attendants and emergency obstetric care to poor women at a relatively small cost. Poor women will take up the benefit of skilled delivery care rapidly, if they do not have to pay for it. PMID:20454488

  12. Incidence and determinants of hysterectomy in a low-income setting in Gujarat, India.

    PubMed

    Desai, Sapna; Campbell, Oona Mr; Sinha, Tara; Mahal, Ajay; Cousens, Simon

    2017-02-01

    Hysterectomy is a leading reason for use of health insurance amongst low-income women in India, but there are limited population-level data available to inform policy. This paper reports on the findings of a mixed-methods study to estimate incidence and identify predictors of hysterectomy in a low-income setting in Gujarat, India. The estimated incidence of hysterectomy, 20.7/1000 woman- years (95% CI: 14.0, 30.8), was considerably higher than reported from other countries, at a relatively low mean age of 36 years. There was strong evidence that among women of reproductive age, those with lower income and at least two children underwent hysterectomy at higher rates. Nearly two-thirds of women undergoing hysterectomy utilized private hospitals, while the remainder used government or other non-profit facilities. Qualitative research suggested that weak sexual and reproductive health services, a widespread perception that the post-reproductive uterus is dispensable and lack of knowledge of side effects have resulted in the normalization of hysterectomy. Hysterectomy appears to be promoted as a first or second-line treatment for menstrual and gynaecological disorders that are actually amenable to less invasive procedures. Most women sought at least two medical opinions prior to hysterectomy, but both public and private providers lacked equipment, skills and motivation to offer alternatives. Profit and training benefits also appeared to play a role in some providers' behaviour. Although women with insecure employment underwent the procedure knowing the financial and physical implications of undergoing a major surgery, the future health and work security afforded by hysterectomy appeared to them to outweigh risks. Findings suggest that sterilization may be associated with an increased risk of hysterectomy, potentially through biological or attitudinal links. Health policy interventions require improved access to sexual and reproductive health services and health

  13. Incidence and determinants of hysterectomy in a low-income setting in Gujarat, India

    PubMed Central

    Desai, Sapna; Campbell, Oona MR; Sinha, Tara; Mahal, Ajay; Cousens, Simon

    2017-01-01

    Abstract Hysterectomy is a leading reason for use of health insurance amongst low-income women in India, but there are limited population-level data available to inform policy. This paper reports on the findings of a mixed-methods study to estimate incidence and identify predictors of hysterectomy in a low-income setting in Gujarat, India. The estimated incidence of hysterectomy, 20.7/1000 woman- years (95% CI: 14.0, 30.8), was considerably higher than reported from other countries, at a relatively low mean age of 36 years. There was strong evidence that among women of reproductive age, those with lower income and at least two children underwent hysterectomy at higher rates. Nearly two-thirds of women undergoing hysterectomy utilized private hospitals, while the remainder used government or other non-profit facilities. Qualitative research suggested that weak sexual and reproductive health services, a widespread perception that the post-reproductive uterus is dispensable and lack of knowledge of side effects have resulted in the normalization of hysterectomy. Hysterectomy appears to be promoted as a first or second-line treatment for menstrual and gynaecological disorders that are actually amenable to less invasive procedures. Most women sought at least two medical opinions prior to hysterectomy, but both public and private providers lacked equipment, skills and motivation to offer alternatives. Profit and training benefits also appeared to play a role in some providers’ behaviour. Although women with insecure employment underwent the procedure knowing the financial and physical implications of undergoing a major surgery, the future health and work security afforded by hysterectomy appeared to them to outweigh risks. Findings suggest that sterilization may be associated with an increased risk of hysterectomy, potentially through biological or attitudinal links. Health policy interventions require improved access to sexual and reproductive health services and

  14. Naphthalene degradation by bacterial consortium (DV-AL) developed from Alang-Sosiya ship breaking yard, Gujarat, India.

    PubMed

    Patel, Vilas; Jain, Siddharth; Madamwar, Datta

    2012-03-01

    Naphthalene degrading bacterial consortium (DV-AL) was developed by enrichment culture technique from sediment collected from the Alang-Sosiya ship breaking yard, Gujarat, India. The 16S rRNA gene based molecular analyzes revealed that the bacterial consortium (DV-AL) consisted of four strains namely, Achromobacter sp. BAB239, Pseudomonas sp. DV-AL2, Enterobacter sp. BAB240 and Pseudomonas sp. BAB241. Consortium DV-AL was able to degrade 1000 ppm of naphthalene in Bushnell Haas medium (BHM) containing peptone (0.1%) as co-substrate with an initial pH of 8.0 at 37°C under shaking conditions (150 rpm) within 24h. Maximum growth rate and naphthalene degradation rate were found to be 0.0389 h(-1) and 80 mg h(-1), respectively. Consortium DV-AL was able to utilize other aromatic and aliphatic hydrocarbons such as benzene, phenol, carbazole, petroleum oil, diesel fuel, and phenanthrene and 2-methyl naphthalene as sole carbon source. Consortium DV-AL was also efficient to degrade naphthalene in the presence of other pollutants such as petroleum hydrocarbons and heavy metals. Copyright © 2011 Elsevier Ltd. All rights reserved.

  15. The dominance of the private sector in the provision of emergency obstetric care: studies from Gujarat, India.

    PubMed

    Salazar, Mariano; Vora, Kranti; De Costa, Ayesha

    2016-07-07

    India has experienced a steep rise in institutional childbirth. The relative contributions of public and private sector facilities to emergency obstetric care (EmOC) has not been studied in this setting. This paper aims to study in three districts of Gujarat state, India:(a) the availability of EmOC facilities in the public and private sectors; (b) the availability and distribution of human resources for birth attendance in the two sectors; and (c) to benchmark the above against 2005 World Health Report benchmarks (WHR2005). A cross-sectional survey of obstetric care facilities reporting 30 or more births in the last three months was conducted (n = 159). Performance of EmOC signal functions and availability of human resources were assessed. EmOC provision was dominated by private facilities (112/159) which were located mainly in district headquarters or small urban towns. The number of basic and comprehensive EmOC facilities was below WHR2005 benchmarks. A high number of private facilities performed C-sections but not all basic signal functions (72/159). Public facilities were the main EmOC providers in rural areas and 40/47 functioned at less than basic EmOC level. The rate of obstetricians per 1000 births was higher in the private sector. The private sector is the dominant EmOC provider in the state. Given the highly skewed distribution of facilities and resources in the private sector, state led partnerships with the private sector so that all women in the state receive care is important alongside strengthening the public sector.

  16. Discriminating satellite IR anomalies associated with the MS 7.1 Yushu earthquake in China

    NASA Astrophysics Data System (ADS)

    Qin, Kai; Wu, Lixin; Zheng, Shuo; Ma, Weiyu

    2018-03-01

    In the process of exploring pre-earthquake thermal anomalies using satellite infrared data, Blackett et al. (2011) found that the previously reported anomalies before the 2001 Mw 7.7 Gujarat earthquake, in India, were related to positive biases caused by data gaps due to cloud cover and mosaicing of neighboring orbits of MODIS satellite data. They supposed that such effects could also be responsible for other cases. We noted a strip-shaped TIR anomaly on March 17th, 2010, 28 days before the Ms. 7.1 Yushu earthquake (Qin et al., 2011). Here we again investigate multi-year infrared satellite data in different bands to discriminate whether the anomaly is associated with the earthquake, or is only bias caused by the data gaps. From the water vapor images, we find lots of clouds that have TIR anomalies. However, on the cloudiness background, there is an obvious strip-shaped gap matching the tectonic faults almost perfectly. In particular, the animation loops of hourly water vapor images show that the cloud kept moving from west to east, while they never covered the strip-shaped gap. We consider that the cloud with this special spatial pattern should have implied the abnormal signals associated with the seismogenic process. Based on current physical models, the satellite IR anomalies both on TIR and water vapor bands can qualitatively be explained using synthetic mechanisms.

  17. Study of earthquakes using a borehole seismic network at Koyna, India

    NASA Astrophysics Data System (ADS)

    Gupta, Harsh; Satyanarayana, Hari VS; Shashidhar, Dodla; Mallika, Kothamasu; Ranjan Mahato, Chitta; Shankar Maity, Bhavani

    2017-04-01

    Koyna, located near the west coast of India, is a classical site of artificial water reservoir triggered earthquakes. Triggered earthquakes started soon after the impoundment of the Koyna Dam in 1962. The activity has continued till now including the largest triggered earthquake of M 6.3 in 1967; 22 earthquakes of M ≥ 5 and several thousands smaller earthquakes. The latest significant earthquake of ML 3.7 occurred on 24th November 2016. In spite of having a network of 23 broad band 3-component seismic stations in the near vicinity of the Koyna earthquake zone, locations of earthquakes had errors of 1 km. The main reason was the presence of 1 km thick very heterogeneous Deccan Traps cover that introduced noise and locations could not be improved. To improve the accuracy of location of earthquakes, a unique network of eight borehole seismic stations surrounding the seismicity was designed. Six of these have been installed at depths varying from 981 m to 1522 m during 2015 and 2016, well below the Deccan Traps cover. During 2016 a total of 2100 earthquakes were located. There has been a significant improvement in the location of earthquakes and the absolute errors of location have come down to ± 300 m. All earthquakes of ML ≥ 0.5 are now located, compared to ML ≥1.0 earlier. Based on seismicity and logistics, a block of 2 km x 2 km area has been chosen for the 3 km deep pilot borehole. The installation of the borehole seismic network has further elucidated the correspondence between rate of water loading/unloading the reservoir and triggered seismicity.

  18. Development and Implementation of South Asia’s First Heat-Health Action Plan in Ahmedabad (Gujarat, India)

    PubMed Central

    Knowlton, Kim; Kulkarni, Suhas P.; Azhar, Gulrez Shah; Mavalankar, Dileep; Jaiswal, Anjali; Connolly, Meredith; Nori-Sarma, Amruta; Rajiva, Ajit; Dutta, Priya; Deol, Bhaskar; Sanchez, Lauren; Khosla, Radhika; Webster, Peter J.; Toma, Violeta E.; Sheffield, Perry; Hess, Jeremy J.

    2014-01-01

    Recurrent heat waves, already a concern in rapidly growing and urbanizing South Asia, will very likely worsen in a warming world. Coordinated adaptation efforts can reduce heat’s adverse health impacts, however. To address this concern in Ahmedabad (Gujarat, India), a coalition has been formed to develop an evidence-based heat preparedness plan and early warning system. This paper describes the group and initial steps in the plan’s development and implementation. Evidence accumulation included extensive literature review, analysis of local temperature and mortality data, surveys with heat-vulnerable populations, focus groups with health care professionals, and expert consultation. The findings and recommendations were encapsulated in policy briefs for key government agencies, health care professionals, outdoor workers, and slum communities, and synthesized in the heat preparedness plan. A 7-day probabilistic weather forecast was also developed and is used to trigger the plan in advance of dangerous heat waves. The pilot plan was implemented in 2013, and public outreach was done through training workshops, hoardings/billboards, pamphlets, and print advertisements. Evaluation activities and continuous improvement efforts are ongoing, along with plans to explore the program’s scalability to other Indian cities, as Ahmedabad is the first South Asian city to address heat-health threats comprehensively. PMID:24670386

  19. New fossils from Tadkeshwar Mine (Gujarat, India) increase primate diversity from the early Eocene Cambay Shale.

    PubMed

    Rose, Kenneth D; Dunn, Rachel H; Kumar, Kishor; Perry, Jonathan M G; Prufrock, Kristen A; Rana, Rajendra S; Smith, Thierry

    2018-06-07

    Several new fossil specimens from the Cambay Shale Formation at Tadkeshwar Lignite Mine in Gujarat document the presence of two previously unknown early Eocene primate species from India. A new species of Asiadapis is named based on a jaw fragment preserving premolars similar in morphology to those of A. cambayensis but substantially larger. Also described is an exceptionally preserved edentulous dentary (designated cf. Asiadapis, unnamed sp. nov.) that is slightly larger and much more robust than previously known Cambay Shale primates. Its anatomy most closely resembles that of Eocene adapoids, and the dental formula is the same as in A. cambayensis. A femur and calcaneus are tentatively allocated to the same taxon. Although the dentition is unknown, exquisite preservation of the dentary of cf. Asiadapis sp. nov. enables an assessment of masticatory musculature, function, and gape adaptations, as well as comparison with an equally well-preserved dentary of the asiadapid Marcgodinotius indicus, also from Tadkeshwar. The new M. indicus specimen shows significant gape adaptations but was probably capable of only weak bite force, whereas cf. Asiadapis sp. nov. probably used relatively smaller gapes but could generate relatively greater bite forces. Copyright © 2018 Elsevier Ltd. All rights reserved.

  20. New euprimate postcrania from the early Eocene of Gujarat, India, and the strepsirrhine-haplorhine divergence.

    PubMed

    Dunn, Rachel H; Rose, Kenneth D; Rana, Rajendra S; Kumar, Kishor; Sahni, Ashok; Smith, Thierry

    2016-10-01

    The oldest primates of modern aspect (euprimates) appear abruptly on the Holarctic continents during a brief episode of global warming known as the Paleocene-Eocene Thermal Maximum, at the beginning of the Eocene (∼56 Ma). When they first appear in the fossil record, they are already divided into two distinct clades, Adapoidea (basal members of Strepsirrhini, which includes extant lemurs, lorises, and bushbabies) and Omomyidae (basal Haplorhini, which comprises living tarsiers, monkeys, and apes). Both groups have recently been discovered in the early Eocene Cambay Shale Formation of Vastan lignite mine, Gujarat, India, where they are known mainly from teeth and jaws. The Vastan fossils are dated at ∼54.5 Myr based on associated dinoflagellates and isotope stratigraphy. Here, we describe new, exquisitely preserved limb bones of these Indian primates that reveal more primitive postcranial characteristics than have been previously documented for either clade, and differences between them are so minor that in many cases we cannot be certain to which group they belong. Nevertheless, the small distinctions observed in some elements foreshadow postcranial traits that distinguish the groups by the middle Eocene, suggesting that the Vastan primates-though slightly younger than the oldest known euprimates-may represent the most primitive known remnants of the divergence between the two great primate clades. Copyright © 2016 Elsevier Ltd. All rights reserved.

  1. Probing reservoir-triggered earthquakes in Koyna, India, through scientific deep drilling

    USGS Publications Warehouse

    Gupta, H.; Nayak, Shailesh; Ellsworth, William L.; Rao, Y. J. B.; Rajan, S.; Bansal, B.K.; Purnachandra Rao, N.; Roy, S.; Arora, K.; Mohan, R.; Tiwari, V. M.; Satyanarayana, H. V. S.; Patro, P. K.; Shashidhar, D.; Mallika, K.

    2014-01-01

    We report here the salient features of the recently concluded International Continental Scientific Drilling Program (ICDP) workshop in Koyna, India. This workshop was a sequel to the earlier held ICDP workshop in Hyderabad and Koyna in 2011. A total of 49 experts (37 from India and 12 from 8 other countries) spent 3 days reviewing the work carried out during the last 3 years based on the recommendations of the 2011 workshop and suggesting the future course of action, including detailed planning for a full deep drilling proposal in Koyna, India. It was unanimously concluded that Koyna is one of the best sites anywhere in the world to investigate genesis of triggered earthquakes from near-field observations. A broad framework of the activities for the next phase leading to deep drilling has been worked out.

  2. Capacity of frontline ICDS functionaries to support caregivers on infant and young child feeding (IYCF) practices in Gujarat, India.

    PubMed

    Chaturvedi, Anuraag; Nakkeeran, N; Doshi, Minal; Patel, Ruchi; Bhagwat, Sadhana

    2014-01-01

    Improved infant and young child feeding practices have the potential to improve child growth and development outcomes in India. Anganwadi Workers, the frontline government functionaries of the national nutrition supplementation programme in India, play a vital role in promoting infant and young child feeding practices in the community. The present study assessed the Anganwadi Workers' knowledge of infant and young child feeding practices, and their ability to counsel and influence caregivers regarding these practices. Eighty Anganwadi Workers from four districts of Gujarat participated in assessment centres designed to evaluate a range of competencies considered necessary for the successful promotion of infant and young child feeding practices. The results of the evaluation showed the Anganwadi Workers possessing more knowledge about infant and young child feeding practices like initiation of breastfeeding, pre-lacteal feeding and colostrum, age of introduction of complementary foods, portion size and feeding frequency than about domains which appear to have a direct bearing on practices. A huge contrast existed between the Anganwadi Workers' knowledge and their ability to apply this in formal counselling sessions with caregivers. Inability to empathetically engage with caregivers, disregard for taking the feeding history of children, poor active listening skills and inability to provide need-based advice were pervasive during counselling. In conclusion, to ensure enhanced interaction between the Anganwadi Workers and caregivers on infant and young child feeding practices, a paradigm shift in training is required, making communication processes and counselling skills central to the training.

  3. The state-led large scale public private partnership 'Chiranjeevi Program' to increase access to institutional delivery among poor women in Gujarat, India: How has it done? What can we learn?

    PubMed

    De Costa, Ayesha; Vora, Kranti S; Ryan, Kayleigh; Sankara Raman, Parvathy; Santacatterina, Michele; Mavalankar, Dileep

    2014-01-01

    Many low-middle income countries have focused on improving access to and quality of obstetric care, as part of promoting a facility based intra-partum care strategy to reduce maternal mortality. The state of Gujarat in India, implements a facility based intra-partum care program through its large for-profit private obstetric sector, under a state-led public-private-partnership, the Chiranjeevi Yojana (CY), under which the state pays accredited private obstetricians to perform deliveries for poor/tribal women. We examine CY performance, its contribution to overall trends in institutional deliveries in Gujarat over the last decade and its effect on private and public sector deliveries there. District level institutional delivery data (public, private, CY), national surveys, poverty estimates, census data were used. Institutional delivery trends in Gujarat 2000-2010 are presented; including contributions of different sectors and CY. Piece-wise regression was used to study the influence of the CY program on public and private sector institutional delivery. Institutional delivery rose from 40.7% (2001) to 89.3% (2010), driven by sharp increases in private sector deliveries. Public sector and CY contributed 25-29% and 13-16% respectively of all deliveries each year. In 2007, 860 of 2000 private obstetricians participated in CY. Since 2007, >600,000 CY deliveries occurred i.e. one-third of births in the target population. Caesareans under CY were 6%, higher than the 2% reported among poor women by the DLHS survey just before CY. CY did not influence the already rising proportion of private sector deliveries in Gujarat. This paper reports a state-led, fully state-funded, large-scale public-private partnership to improve poor women's access to institutional delivery - there have been >600,000 beneficiaries. While caesarean proportions are higher under CY than before, it is uncertain if all beneficiaries who require sections receive these. Other issues to explore include

  4. Pulmonary function test in healthy school children of 8 to 14 years age in south Gujarat region, India

    PubMed Central

    Doctor, Tahera H.; Trivedi, Sangeeta S.; Chudasama, Rajesh K.

    2010-01-01

    Objective: To obtain reference values for FEV1, FVC, FEV1% and PEFR among children aged 8-14 years in south Gujarat region of India. Materials and Methods: This cross-sectional study was conducted among 655 normal healthy school children (408 boys and 247 girls) of Surat city aged 8 to 14 years studying in V to VII standard during November 2007 to April 2008. Height, weight, body surface area were measured. All included children were tested in a sitting position with the head straight after taking written consent from parents. Spirometry was done using the spirometer “Spirolab II” MIR 010. Spirometer used in the study facilitates the total valuation of lung function including forced vital capacity (FVC), forced expiratory volume in one second (FEV1), forced expiratory volume ratio in one second (FEV1%) and peak expiratory flow rate (PEFR). Results: FVC, FEV1 and PEFR were found to be statistically significant in the study groups. For FVC and FEV1, highest correlation was found with age in girls and height in boys. For FEV1%, significant negative correlation was found with age and height in both sexes, but positive correlation was found with surface area. Similarly, PEFR showed highest correlation with surface area in boys and girls. Conclusion: Variables such as FVC, FEV1 and PEFR show good positive correlation with height, age and body surface area in both sexes. There is a need to have regional values for the prediction of normal spirometric parameters in a country like India with considerable diversity. PMID:20931033

  5. Role of deep crustal fluids in the genesis of intraplate earthquakes in the Kachchh region, northwestern India

    NASA Astrophysics Data System (ADS)

    Pavan Kumar, G.; Mahesh, P.; Nagar, Mehul; Mahender, E.; Kumar, Virendhar; Mohan, Kapil; Ravi Kumar, M.

    2017-05-01

    Fluids play a prominent role in the genesis of earthquakes, particularly in intraplate settings. In this study, we present evidence for a highly heterogeneous nature of electrical conductivity in the crust and uppermost mantle beneath the Kachchh rift basin of northwestern India, which is host to large, deadly intraplate earthquakes. We interpret our results of high conductive zones inferred from magnetotelluric and 3-D local earthquake tomography investigations in terms of a fluid reservoir in the upper mantle. The South Wagad Fault (SWF) imaged as a near-vertical north dipping low resistivity zone traversing the entire crust and an elongated south dipping conductor demarcating the North Wagad Fault (NWF) serve as conduits for fluid flow from the reservoir to the middle to lower crustal depths. Importantly, the epicentral zone of the 2001 main shock is characterized as a fluid saturated zone at the rooting of NWF onto the SWF.Plain Language SummaryFluids play a significant role in generation of <span class="hlt">earthquakes</span> in intraplate and interplate settings. However, knowledge of the nature, origin, and localization of crustal fluids in stable continental interiors (intraplate) remains uncertain. The Kachchh rift basin of northwestern <span class="hlt">India</span> is host to large, deadly intraplate <span class="hlt">earthquakes</span> like those in 1819 (Mw7.8) and 2001 (Mw7.7). In the present study we carried out extensive geophysical investigations to understand the cause for seismic activity in the region. The study provides the evidence for the presence of fluids in the seismically active intraplate region of northwest <span class="hlt">India</span>. This study demonstrates that the dynamics of mantle fluids controlled by geological faults could lead to large and moderate-sized <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4006779','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4006779"><span>The State-Led Large Scale Public Private Partnership ‘Chiranjeevi Program’ to Increase Access to Institutional Delivery among Poor Women in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: How Has It Done? What Can We Learn?</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>De Costa, Ayesha; Vora, Kranti S.; Ryan, Kayleigh; Sankara Raman, Parvathy; Santacatterina, Michele; Mavalankar, Dileep</p> <p>2014-01-01</p> <p>Background Many low-middle income countries have focused on improving access to and quality of obstetric care, as part of promoting a facility based intra-partum care strategy to reduce maternal mortality. The state of <span class="hlt">Gujarat</span> in <span class="hlt">India</span>, implements a facility based intra-partum care program through its large for-profit private obstetric sector, under a state-led public-private-partnership, the Chiranjeevi Yojana (CY), under which the state pays accredited private obstetricians to perform deliveries for poor/tribal women. We examine CY performance, its contribution to overall trends in institutional deliveries in <span class="hlt">Gujarat</span> over the last decade and its effect on private and public sector deliveries there. Methods District level institutional delivery data (public, private, CY), national surveys, poverty estimates, census data were used. Institutional delivery trends in <span class="hlt">Gujarat</span> 2000–2010 are presented; including contributions of different sectors and CY. Piece-wise regression was used to study the influence of the CY program on public and private sector institutional delivery. Results Institutional delivery rose from 40.7% (2001) to 89.3% (2010), driven by sharp increases in private sector deliveries. Public sector and CY contributed 25–29% and 13–16% respectively of all deliveries each year. In 2007, 860 of 2000 private obstetricians participated in CY. Since 2007, >600,000 CY deliveries occurred i.e. one-third of births in the target population. Caesareans under CY were 6%, higher than the 2% reported among poor women by the DLHS survey just before CY. CY did not influence the already rising proportion of private sector deliveries in <span class="hlt">Gujarat</span>. Conclusion This paper reports a state-led, fully state-funded, large-scale public-private partnership to improve poor women’s access to institutional delivery - there have been >600,000 beneficiaries. While caesarean proportions are higher under CY than before, it is uncertain if all beneficiaries who require sections</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70168762','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70168762"><span><span class="hlt">Earthquakes</span>, September-October 1991</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1992-01-01</p> <p>There were two major <span class="hlt">earthquakes</span> (7.0-7.9) during this reporting period. the first was in the Solomon Islands on October 14 and the second was in <span class="hlt">India</span> on October 19. <span class="hlt">Earthquake</span>-related deaths were reported in Guatemala and <span class="hlt">India</span>. Htere were no significant <span class="hlt">earthquakes</span> in the United States during the period covered in this report. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015OGeo....7...19R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015OGeo....7...19R"><span>Fluid Inclusion Study of Quartz Xenocrysts in Mafic Dykes from Kawant Area, Chhota Udaipur District, <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Randive, Kirtikumar; Hurai, Vratislav</p> <p>2015-09-01</p> <p>Unusual mafic dykes occur in the proximity of the Ambadongar Carbonatite Complex, Lower Narmada Valley, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. The dykes contain dense population of quartz xenocrysts within the basaltic matrix metasomatised by carbonate-rich fluids. Plagioclase feldspars, relict pyroxenes, chlorite, barite, rutile, magnetite, Fe-Ti oxides and glass were identified in the basaltic matrix. Quartz xenocrysts occur in various shapes and sizes and form an intricate growth pattern with carbonates. The xenocrysts are fractured and contain several types of primary and secondary, single phase and two-phase fluid inclusions. The two-phase inclusions are dominated by aqueous liquid, whereas the monophase inclusions are composed of carbonic gas and the aqueous inclusions homogenize to liquid between 226°C and 361°C. Majority of the inclusions are secondary in origin and are therefore unrelated to the crystallization of quartz. Moreover, the inclusions have mixed carbonic-aqueous compositions that inhibit their direct correlation with the crustal or mantle fluids. The composition of dilute CO2-rich fluids observed in the quartz xenocrysts appear similar to those exsolved during the final stages of evolution of the Amba Dongar carbonatites. However, the carbonates are devoid of fluid inclusions and therefore their genetic relation with the quartz xenocrysts cannot be established.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26825416','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26825416"><span>Predictors of maternal health services utilization by poor, rural women: a comparative study in Indian States of <span class="hlt">Gujarat</span> and Tamil Nadu.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Vora, Kranti Suresh; Koblinsky, Sally A; Koblinsky, Marge A</p> <p>2015-07-31</p> <p><span class="hlt">India</span> leads all nations in numbers of maternal deaths, with poor, rural women contributing disproportionately to the high maternal mortality ratio. In 2005, <span class="hlt">India</span> launched the world's largest conditional cash transfer scheme, Janani Suraksha Yojana (JSY), to increase poor women's access to institutional delivery, anticipating that facility-based birthing would decrease deaths. Indian states have taken different approaches to implementing JSY. Tamil Nadu adopted JSY with a reorganization of its public health system, and <span class="hlt">Gujarat</span> augmented JSY with the state-funded Chiranjeevi Yojana (CY) scheme, contracting with private physicians for delivery services. Given scarce evidence of the outcomes of these approaches, especially in states with more optimal health indicators, this cross-sectional study examined the role of JSY/CY and other healthcare system and social factors in predicting poor, rural women's use of maternal health services in <span class="hlt">Gujarat</span> and Tamil Nadu. Using the District Level Household Survey (DLHS)-3, the sample included 1584 Gujarati and 601 Tamil rural women in the lowest two wealth quintiles. Multivariate logistic regression analyses examined associations between JSY/CY and other salient health system, socio-demographic, and obstetric factors with three outcomes: adequate antenatal care, institutional delivery, and Cesarean-section. Tamil women reported greater use of maternal healthcare services than Gujarati women. JSY/CY participation predicted institutional delivery in <span class="hlt">Gujarat</span> (AOR = 3.9), but JSY assistance failed to predict institutional delivery in Tamil Nadu, where mothers received some cash for home births under another scheme. JSY/CY assistance failed to predict adequate antenatal care, which was not incentivized. All-weather road access predicted institutional delivery in both Tamil Nadu (AOR = 3.4) and <span class="hlt">Gujarat</span> (AOR = 1.4). Women's education predicted institutional delivery and Cesarean-section in Tamil Nadu, while husbands</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28985232','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28985232"><span>Altered cropping pattern and cultural continuation with declined prosperity following abrupt and extreme arid event at ~4,200 yrs BP: Evidence from an Indus archaeological site Khirsara, <span class="hlt">Gujarat</span>, western <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Pokharia, Anil K; Agnihotri, Rajesh; Sharma, Shalini; Bajpai, Sunil; Nath, Jitendra; Kumaran, R N; Negi, Bipin Chandra</p> <p>2017-01-01</p> <p>Archaeological sites hold important clues to complex climate-human relationships of the past. Human settlements in the peripheral zone of Indus culture (<span class="hlt">Gujarat</span>, western <span class="hlt">India</span>) are of considerable importance in the assessment of past monsoon-human-subsistence-culture relationships and their survival thresholds against climatic stress exerted by abrupt changes. During the mature phase of Harappan culture between ~4,600-3,900yrsBP, the ~4,100±100yrsBP time slice is widely recognized as one of the major, abrupt arid-events imprinted innumerous well-dated palaeo records. However, the veracity of this dry event has not been established from any archaeological site representing the Indus (Harappan) culture, and issues concerning timing, changes in subsistence pattern, and the likely causes of eventual abandonment (collapse) continue to be debated. Here we show a significant change in crop-pattern (from barley-wheat based agriculture to 'drought-resistant' millet-based crops) at ~4,200 yrs BP, based on abundant macrobotanical remains and C isotopes of soil organic matter (δ13CSOM) in an archaeological site at Khirsara, in the <span class="hlt">Gujarat</span> state of western <span class="hlt">India</span>. The crop-change appears to be intentional and was likely used as an adaptation measure in response to deteriorated monsoonal conditions. The ceramic and architectural remains of the site indicate that habitation survived and continued after the ~4,200yrsBP dry climatic phase, but with declined economic prosperity. Switching to millet-based crops initially helped inhabitants to avoid immediate collapse due to climatic stresses, but continued aridity and altered cropping pattern led to a decline in prosperity levels of inhabitants and eventual abandonment of the site at the end of the mature Harappan phase.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.S51B1429M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.S51B1429M"><span><span class="hlt">Earthquake</span> Forecasting in Northeast <span class="hlt">India</span> using Energy Blocked Model</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mohapatra, A. K.; Mohanty, D. K.</p> <p>2009-12-01</p> <p>In the present study, the cumulative seismic energy released by <span class="hlt">earthquakes</span> (M ≥ 5) for a period 1897 to 2007 is analyzed for Northeast (NE) <span class="hlt">India</span>. It is one of the most seismically active regions of the world. The occurrence of three great <span class="hlt">earthquakes</span> like 1897 Shillong plateau <span class="hlt">earthquake</span> (Mw= 8.7), 1934 Bihar Nepal <span class="hlt">earthquake</span> with (Mw= 8.3) and 1950 Upper Assam <span class="hlt">earthquake</span> (Mw= 8.7) signify the possibility of great <span class="hlt">earthquakes</span> in future from this region. The regional seismicity map for the study region is prepared by plotting the <span class="hlt">earthquake</span> data for the period 1897 to 2007 from the source like USGS,ISC catalogs, GCMT database, Indian Meteorological department (IMD). Based on the geology, tectonic and seismicity the study region is classified into three source zones such as Zone 1: Arakan-Yoma zone (AYZ), Zone 2: Himalayan Zone (HZ) and Zone 3: Shillong Plateau zone (SPZ). The Arakan-Yoma Range is characterized by the subduction zone, developed by the junction of the Indian Plate and the Eurasian Plate. It shows a dense clustering of <span class="hlt">earthquake</span> events and the 1908 eastern boundary <span class="hlt">earthquake</span>. The Himalayan tectonic zone depicts the subduction zone, and the Assam syntaxis. This zone suffered by the great <span class="hlt">earthquakes</span> like the 1950 Assam, 1934 Bihar and the 1951 Upper Himalayan <span class="hlt">earthquakes</span> with Mw > 8. The Shillong Plateau zone was affected by major faults like the Dauki fault and exhibits its own style of the prominent tectonic features. The seismicity and hazard potential of Shillong Plateau is distinct from the Himalayan thrust. Using energy blocked model by Tsuboi, the forecasting of major <span class="hlt">earthquakes</span> for each source zone is estimated. As per the energy blocked model, the supply of energy for potential <span class="hlt">earthquakes</span> in an area is remarkably uniform with respect to time and the difference between the supply energy and cumulative energy released for a span of time, is a good indicator of energy blocked and can be utilized for the forecasting of major <span class="hlt">earthquakes</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007PApGe.164.2235M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007PApGe.164.2235M"><span>Source Parameters of the 8 October, 2005 Mw7.6 Kashmir <span class="hlt">Earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mandal, Prantik; Chadha, R. K.; Kumar, N.; Raju, I. P.; Satyamurty, C.</p> <p>2007-12-01</p> <p>During the last six years, the National Geophysical Research Institute, Hyderabad has established a semi-permanent seismological network of 5 broadband seismographs and 10 accelerographs in the Kachchh seismic zone, <span class="hlt">Gujarat</span>, with the prime objective to monitor the continued aftershock activity of the 2001 Mw7.7 Bhuj mainshock. The reliable and accurate broadband data for the Mw 7.6 (8 Oct., 2005) Kashmir <span class="hlt">earthquake</span> and its aftershocks from this network, as well as from the Hyderabad Geoscope station, enabled us to estimate the group velocity dispersion characteristics and the one-dimensional regional shear-velocity structure of peninsular <span class="hlt">India</span>. Firstly, we measure Rayleigh- and Love-wave group velocity dispersion curves in the range of 8 to 35 sec and invert these curves to estimate the crustal and upper mantle structure below the western part of peninsular <span class="hlt">India</span>. Our best model suggests a two-layered crust: The upper crust is 13.8-km thick with a shear velocity (Vs) of 3.2 km/s; the corresponding values for the lower crust are 24.9 km and 3.7 km/sec. The shear velocity for the upper mantle is found to be 4.65 km/sec. Based on this structure, we perform a moment tensor (MT) inversion of the bandpass (0.05 0.02 Hz) filtered seismograms of the Kashmir <span class="hlt">earthquake</span>. The best fit is obtained for a source located at a depth of 30 km, with a seismic moment, Mo, of 1.6 × 1027 dyne-cm, and a focal mechanism with strike 19.5°, dip 42°, and rake 167°. The long-period magnitude (MA ~ Mw) of this <span class="hlt">earthquake</span> is estimated to be 7.31. An analysis of well-developed sPn and sSn regional crustal phases from the bandpassed (0.02 0.25 Hz) seismograms of this <span class="hlt">earthquake</span> at four stations in Kachchh suggests a focal depth of 30.8 km.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMGC53G1286P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMGC53G1286P"><span>Impact assessment of climate change on wheat (Triticum aestivum L.) and mustard (Brassica spp.) production and its adaptation strategies in different districts of <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pandey, V.; Patel, H. R.; Yadav, S. B.; Patil, D. D.</p> <p>2015-12-01</p> <p><span class="hlt">Gujarat</span> is the western-most state of <span class="hlt">India</span> with a long (1600 km) sea coast on the Arabian Sea. Average annual rainfall ranges from as high as 1900 mm in the sub-humid southeast to as low as 250 mm in the arid north. There are three distinct crop seasons- rainy (June to September), winter (Oct.-Nov. through Feb.-March) and summer (Feb-March through May-June). Wheat and mustard are grown during winter seasons. The past climatic records suggested increasing trends in rainfall( 2 to 5 mm per year), maximum (0.03 to 0.05 0C per year) and minimum temperatures (0.02 to 0.05 0C per year) at most of places in <span class="hlt">Gujarat</span>. But the minimum temperature is fould to be increasing significantly at all the locations. This affects the winter season crops viz. wheat and mustard adversely. Simulation results with DSSAT CERES-wheat model revealed that with increase in temperature by 2 0C in different months (November to February) the decrease in wheat yield is observed between 7 to 29 per cent. The impact of increase in maximum temperature during early (November) and late (February) is less (<12.5 %) than that during active vegetative and reproductive period (December and January; >24.8 %). The climate change projections during 2071-2100 using PRECIS output suggested that there would be increase in maximum temperature by 3.2 to 5.2 0C in different districts of <span class="hlt">Gujarat</span> over baseline period of 1961-1990 while minimum temperature is project to increase by 2.8 to 5.8 0C. Rainfall is also projected to increase by 28 to 70 per cent in different districts. The impact of climate change on wheat would be reduction in its duration by 14-20 days and the grain yield would be reduced by 20-55 per cent in different districts. In case of mustard crops the duration of crop would be reduced by 11 to 16 days and seed yield would be reduced by 32-50 per cent. In order to mitigate the ill effect of climate change, various adaptation strategies vis change in dates of sowing, change in variety, additional</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016Tectp.688...36G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016Tectp.688...36G"><span>Seismological, geodetic, macroseismic and historical context of the 2016 Mw 6.7 Tamenglong (Manipur) <span class="hlt">India</span> <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gahalaut, V. K.; Martin, Stacey S.; Srinagesh, D.; Kapil, S. L.; Suresh, G.; Saikia, Saurav; Kumar, Vikas; Dadhich, Harendra; Patel, Aqeel; Prajapati, Sanjay K.; Shukla, H. P.; Gautam, J. L.; Baidya, P. R.; Mandal, Saroj; Jain, Ashish</p> <p>2016-10-01</p> <p>The 2016 Mw 6.7 Tamenglong <span class="hlt">earthquake</span> (in the state of Manipur in northeastern <span class="hlt">India</span>) on 4 January 2016 at 04:35 Indian Standard Time (3 January, 23:05 UTC) was the strongest <span class="hlt">earthquake</span> to strike Manipur since 1988. Using data from Indian stations, we constrain the hypocentral depth of the mainshock at 59 ± 3.8 km and determine a strike-slip mechanism with a moderate reverse component on a steeply dipping plane. Though coseismic offsets from GPS measurements from four nearby sites were inadequate to provide further constraints on the focal mechanism, they were consistent with the magnitude and hypocentral depth of the <span class="hlt">earthquake</span>. The epicentre of the mainshock was located 15-km west of the Churachandpur Mao Fault (CMF) but it was unrelated to this structure and was instead a typical intra-slab <span class="hlt">earthquake</span> within the Indian plate. A strong motion instrument at the Loktak Power Station (LOK), 56-km from the epicentre, recorded a peak ground acceleration (PGA) of 0.027g while a PGA of 0.103g was recorded at Shillong (SHL) at an epicentral distance of 111-km. We also present macroseismic observations from 461 locations in north-eastern <span class="hlt">India</span> and the adjacent areas for this <span class="hlt">earthquake</span>. The highest intensities ( 7 EMS) were observed in the Manipur Valley and in the hills to the west while shaking was perceptible as far as Delhi and Jaipur. Lastly, we present a catalogue of 333 felt <span class="hlt">earthquakes</span> in Manipur from 1588 ± 1 CE to 1955 derived from the royal chronicle of the kings of Manipur known as the Cheitharon Kumpapa, discuss important historical <span class="hlt">earthquakes</span> in the region, and also estimate intensity magnitudes for the 1852 (MI 6.5 ± 0.8), 1869 (MI 7.1 ± 0.7), 1880 (MI 6.3 ± 0.7) and 2016 (MI 6.8 ± 0.8) <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..11.1932J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..11.1932J"><span><span class="hlt">Earthquake</span> Hazard Assessment Based on Geological Data: An approach from Crystalline Terrain of Peninsular <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>John, B.</p> <p>2009-04-01</p> <p><span class="hlt">Earthquake</span> Hazard Assessment Based on Geological Data: An approach from Crystalline Terrain of Peninsular <span class="hlt">India</span> Biju John National Institute of Rock Mechanics b_johnp@yahoo.co.in Peninsular <span class="hlt">India</span> was for long considered as seismically stable. But the recent <span class="hlt">earthquake</span> sequence of Latur (1993), Jabalpur (1997), Bhuj (2001) suggests this region is among one of the active Stable Continental Regions (SCRs) of the world, where the recurrence intervals is of the order of tens of thousands of years. In such areas, <span class="hlt">earthquake</span> may happen at unexpected locations, devoid of any previous seismicity or dramatic geomorphic features. Even moderate <span class="hlt">earthquakes</span> will lead to heavy loss of life and property in the present scenario. So it is imperative to map suspected areas to identify active faults and evaluate its activities, which will be a vital input to seismic hazard assessment of SCR area. The region around Wadakkanchery, Kerala, South <span class="hlt">India</span> has been experiencing micro seismic activities since 1989. Subsequent studies, by the author, identified a 30 km long WNW-ESE trending reverse fault, dipping south (45°), that influenced the drainage system of the area. The macroscopic and microscopic studies of the fault rocks from the exposures near Desamangalam show an episodic nature of faulting. Dislocations of pegmatitic veins across the fault indicate a cumulative dip displacement of 2.1m in the reverse direction. A minimum of four episodes of faulting were identified in this fault based on the cross cutting relations of different structural elements and from the mineralogic changes of different generations of gouge zones. This suggests that an average displacement of 52cm per event might have occurred for each event. A cyclic nature of faulting is identified in this fault zone in which the inter-seismic period is characterized by gouge induration and fracture sealing aided by the prevailing fluids. Available empirical relations connecting magnitude with displacement and rupture</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1996Geomo..15...67A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1996Geomo..15...67A"><span>The palaeodelta of the ``Proto'' Vatrak and ``Proto'' Mahi rivers of northeastern <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: A remote sensing interpretation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Agarwal, R. P.; Dotiwala, Sucheta; Mitra, D. S.; Bhoj, R.</p> <p>1996-02-01</p> <p>Detailed remote sensing studies carried out in northeastern <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, suggest that there has been a major change in the drainage system as evidenced by the presence of a large palaeo-delta system. The area is drained by two major rivers, the Mahi and Vatrak originating from the Aravalli Hills to the east, which discharge into the Gulf of Cambay, in the Indian Ocean. Major lineaments, palaeodrainage patterns and palaeodeltas of the Vatrak and Mahi rivers were delineated. These were large rivers in the past with a high discharge and floodplains which were 5-10 km wide. Most of the palaeodrainage follows the NE-SW Precambrian lineaments/ faults indicating their structural control. Reactivation of these lineaments and differential uplift of the Aravalli Hills resulted in increased transportation of the eroded sediments and deposition of more than 5 km thick sediments into the Tarapur block of the Cambay Basin. The Gulf of Cambay extended up to the Limbasi-Sojitra-Petlad area during the Quaternary. There are implications for petroleum exploration in the sense that the results when integrated with subsurface geological and geophysical data help to delineate the reservoir facies suitable for petroleum exploration along the eastern margin of the Tarapur block.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26108747','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26108747"><span>Decadal changes in the land use/land cover and shoreline along the coastal districts of southern <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Misra, A; Balaji, R</p> <p>2015-07-01</p> <p>The coastal zone along the districts of Surat, Navsari, and Valsad in southern <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, is reported to be facing serious environmental challenges in the form of shoreline erosion, wetland loss, and man-made encroachments. This study assesses the decadal land use/ land cover (LULC) changes in these three districts for the years 1990, 2001, and 2014 using satellite datasets of Landsat TM, ETM, and OLI. The LULC changes are identified by using band ratios as a pre-classification step, followed by implementation of hybrid classification (a combination of supervised and unsupervised classification). An accuracy assessment is carried out for each dataset, and the overall accuracy ranges from 90 to 95%. It is observed that the spatial extents of aquaculture, urban built-up, and barren classes have appreciated over time, whereas the coverage of mudflats has depreciated due to rapid urbanization. The changes in the shoreline of these districts have also been analyzed for the same years, and significant changes are found in the form of shoreline erosion. The LULC maps prepared as well as the shoreline change analysis done for this study area will enable the local decision makers to adopt better land-use planning and shoreline protection measures, which will further aid in sustainable future developments in this region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5630146','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5630146"><span>Altered cropping pattern and cultural continuation with declined prosperity following abrupt and extreme arid event at ~4,200 yrs BP: Evidence from an Indus archaeological site Khirsara, <span class="hlt">Gujarat</span>, western <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Pokharia, Anil K.; Sharma, Shalini; Bajpai, Sunil; Nath, Jitendra; Kumaran, R. N.; Negi, Bipin Chandra</p> <p>2017-01-01</p> <p>Archaeological sites hold important clues to complex climate-human relationships of the past. Human settlements in the peripheral zone of Indus culture (<span class="hlt">Gujarat</span>, western <span class="hlt">India</span>) are of considerable importance in the assessment of past monsoon-human-subsistence-culture relationships and their survival thresholds against climatic stress exerted by abrupt changes. During the mature phase of Harappan culture between ~4,600–3,900yrsBP, the ~4,100±100yrsBP time slice is widely recognized as one of the major, abrupt arid-events imprinted innumerous well-dated palaeo records. However, the veracity of this dry event has not been established from any archaeological site representing the Indus (Harappan) culture, and issues concerning timing, changes in subsistence pattern, and the likely causes of eventual abandonment (collapse) continue to be debated. Here we show a significant change in crop-pattern (from barley-wheat based agriculture to ‘drought-resistant’ millet-based crops) at ~4,200 yrs BP, based on abundant macrobotanical remains and C isotopes of soil organic matter (δ13CSOM) in an archaeological site at Khirsara, in the <span class="hlt">Gujarat</span> state of western <span class="hlt">India</span>. The crop-change appears to be intentional and was likely used as an adaptation measure in response to deteriorated monsoonal conditions. The ceramic and architectural remains of the site indicate that habitation survived and continued after the ~4,200yrsBP dry climatic phase, but with declined economic prosperity. Switching to millet-based crops initially helped inhabitants to avoid immediate collapse due to climatic stresses, but continued aridity and altered cropping pattern led to a decline in prosperity levels of inhabitants and eventual abandonment of the site at the end of the mature Harappan phase. PMID:28985232</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4843669','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4843669"><span>Potential impact of spatially targeted adult tuberculosis vaccine in <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Chatterjee, Susmita; Rao, Krishna D.; Dowdy, David W.</p> <p>2016-01-01</p> <p>Some of the most promising vaccines in the pipeline for tuberculosis (TB) target adolescents and adults. Unlike for childhood vaccines, high-coverage population-wide vaccination is significantly more challenging for adult vaccines. Here, we aimed to estimate the impact of vaccine delivery strategies that were targeted to high-incidence geographical ‘hotspots’ compared with randomly allocated vaccination. We developed a spatially explicit mathematical model of TB transmission that distinguished these hotspots from the general population. We evaluated the impact of targeted and untargeted vaccine delivery strategies in India—a country that bears more than 25% of global TB burden, and may be a potential early adopter of the vaccine. We collected TB notification data and conducted a demonstration study in the state of <span class="hlt">Gujarat</span> to validate our estimates of heterogeneity in TB incidence. We then projected the impact of randomly vaccinating 8% of adults in a single mass campaign to a spatially targeted vaccination preferentially delivered to 80% of adults in the hotspots, with both strategies augmented by continuous adolescent vaccination. In consultation with vaccine developers, we considered a vaccine efficacy of 60%, and evaluated the population-level impact after 10 years of vaccination. Spatial heterogeneity in TB notification (per 100 000/year) was modest in <span class="hlt">Gujarat</span>: 190 in the hotspots versus 125 in the remaining population. At this level of heterogeneity, the spatially targeted vaccination was projected to reduce TB incidence by 28% after 10 years, compared with a 24% reduction projected to achieve via untargeted vaccination—a 1.17-fold augmentation in the impact of vaccination by spatially targeting. The degree of the augmentation was robust to reasonable variation in natural history assumptions, but depended strongly on the extent of spatial heterogeneity and mixing between the hotspot and general population. Identifying high-incidence hotspots and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5676993','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5676993"><span>Why are HIV-infected people not started on antiretroviral therapy? A mixed-methods study from <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Shringarpure, K.; Modi, B.; Sharma, R.; Rewari, B. B.; Shah, A. N.; Verma, P. B.; Dongre, A. R.; Kumar, A. M. V.</p> <p>2017-01-01</p> <p>Setting: Five purposively selected antiretroviral therapy (ART) centres in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. Objectives: To assess the proportion of ART-eligible people living with the human immunodeficiency virus (PLHIV) who were not initiated on ART within 2 months of being recorded as eligible, to identify factors associated with non-initiation and to explore reasons from the provider's perspective. Design: We used a mixed-methods design (triangulation) of 1) a quantitative phase involving record reviews and cohort analysis (Poisson regression) of PLHIV registered during April 2014–March 2015, and 2) a qualitative phase involving one-to-one interviews with 25 providers. Results: Of 2079 ART-eligible PLHIV, 339 (16%) were not started on ART within 2 months. PLHIV with CD4 counts of <350 cells/μl and patients who were labourers, hospitalised, bedridden or registered with certain ART centres were more likely not to be initiated on ART. Qualitative results were categorised into two broad themes: government health system- and patient-related challenges, which validated and complemented the quantitative findings. Conclusion: Several patient subgroups at greater risk of ART non-initiation were identified, along with reasons for risk; this has important programme implications for achieving the UNAIDS 90–90–90 goal, and particularly the second 90 component of having 90% of diagnosed PLHIV start ART. PMID:29201653</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_4");'>4</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li class="active"><span>6</span></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_6 --> <div id="page_7" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="121"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29637154','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29637154"><span>Epidemiological survey of mental health in adolescent school children of <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Nair, Sandhya; Ganjiwale, Jaishree; Kharod, Nikhil; Varma, Jagdish; Nimbalkar, Somashekhar Marutirao</p> <p>2017-01-01</p> <p>Mental health problems in adolescents are inadequately researched in low-resource settings. We aimed in this study to assess the prevalence of mental health problems and correlates in school children aged 13-17 years and compare differences between urban and rural schools in Anand District, <span class="hlt">Gujarat</span>. A cross-sectional study was conducted in five Gujarati medium higher secondary schools in Anand, <span class="hlt">Gujarat</span>. Six hundred and ninety-three students with equal distribution of boys and girls belonging to 9th to 12th grades were included in the study. Strengths and Difficulties Questionnaire (SDQ) was used to assess the mental health status of the students, and total difficulties scoring was used to categorise participants into normal (0-15) and high (borderline (16-19) and abnormal (20-40)). Socio-demographic data and Teenage Screening Questionnaire-Trivandrum (TSQ) were used to assess associated medical and psychosocial factors. Clearance was obtained from the institutional ethics committee before conducting the study. 15% participants had a high SDQ score. Girls had more emotional problems, while the rest of the mental health problems were more prevalent in boys. Rural children were found to have more mental health issues. Having an eye problem, scoring <50% in last annual examinations, failure in examinations, difficulties in studying at home and difficulties in relationships were associated with high SDQ score. Keeping physically fit and having friends were associated with normal SDQ score. Logistic regression model revealed that age, receiving punishment in form of more homework and difficulty discussing friends with parents increased odds of high SDQ score, while having friends and after-school entertainment like watching movies decreased odds of high SDQ score. At least one in eight adolescents in this study was at risk of mental health problems. SDQ self-report questionnaire and TSQ survey may be used as a screening modality to identify at-risk students.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29353200','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29353200"><span>Monitoring of soil radon by SSNTD in Eastern <span class="hlt">India</span> in search of possible <span class="hlt">earthquake</span> precursor.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Deb, Argha; Gazi, Mahasin; Ghosh, Jayita; Chowdhury, Saheli; Barman, Chiranjib</p> <p>2018-04-01</p> <p>The present paper deals with monitoring soil radon-222 concentration at two different locations, designated Site A and Site B, 200 m apart at Jadavpur University campus, Kolkata, <span class="hlt">India</span>, with a view to find possible precursors for the <span class="hlt">earthquakes</span> that occurred within a few hundred kilometers from the monitoring site. The solid state nuclear track detector CR-39 has been used for detection of radon gas coming out from soil. Radon-222 time series at both locations during the period August 2012-December 2013 have been analysed. Distinct anomalies in the soil radon time series have been observed for seven <span class="hlt">earthquakes</span> of magnitude greater than 4.0 M that occurred during this time. Of these, radon anomalies for two <span class="hlt">earthquakes</span> have been observed at both locations A and B. Absence of anomalies for some other <span class="hlt">earthquakes</span> has been discussed, and the observations have been compared with some <span class="hlt">earthquake</span> precursor models. Copyright © 2018. Published by Elsevier Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFM.S51C..04M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFM.S51C..04M"><span>Coda Q Attenuation and Source Parameters Analysis in North East <span class="hlt">India</span> Using Local <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mohapatra, A. K.; Mohanty, W. K.; Earthquake Seismology</p> <p>2010-12-01</p> <p>Alok Kumar Mohapatra1* and William Kumar Mohanty1 *Corresponding author: alokgpiitkgp@gmail.com 1Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur, West Bengal, <span class="hlt">India</span>. Pin-721302 ABSTRACT In the present study, the quality factor of coda waves (Qc) and the source parameters has been estimated for the Northeastern <span class="hlt">India</span>, using the digital data of ten local <span class="hlt">earthquakes</span> from April 2001 to November 2002. <span class="hlt">Earthquakes</span> with magnitude range from 3.8 to 4.9 have been taken into account. The time domain coda decay method of a single back scattering model is used to calculate frequency dependent values of Coda Q (Qc) where as, the source parameters like seismic moment(Mo), stress drop, source radius(r), radiant energy(Wo),and strain drop are estimated using displacement amplitude spectrum of body wave using Brune's model. The <span class="hlt">earthquakes</span> with magnitude range 3.8 to 4.9 have been used for estimation Qc at six central frequencies 1.5 Hz, 3.0 Hz, 6.0 Hz, 9.0 Hz, 12.0 Hz, and 18.0 Hz. In the present work, the Qc value of local <span class="hlt">earthquakes</span> are estimated to understand the attenuation characteristic, source parameters and tectonic activity of the region. Based on a criteria of homogeneity in the geological characteristics and the constrains imposed by the distribution of available events the study region has been classified into three zones such as the Tibetan Plateau Zone (TPZ), Bengal Alluvium and Arakan-Yuma Zone (BAZ), Shillong Plateau Zone (SPZ). It follows the power law Qc= Qo (f/fo)n where, Qo is the quality factor at the reference frequency (1Hz) fo and n is the frequency parameter which varies from region to region. The mean values of Qc reveals a dependence on frequency, varying from 292.9 at 1.5 Hz to 4880.1 at 18 Hz. Average frequency dependent relationship Qc values obtained of the Northeastern <span class="hlt">India</span> is 198 f 1.035, while this relationship varies from the region to region such as, Tibetan Plateau Zone (TPZ): Qc= 226 f 1.11, Bengal Alluvium</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23961956','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23961956"><span>Promoting universal financial protection: evidence from the Rashtriya Swasthya Bima Yojana (RSBY) in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Devadasan, Narayanan; Seshadri, Tanya; Trivedi, Mayur; Criel, Bart</p> <p>2013-08-20</p> <p><span class="hlt">India</span>'s health expenditure is met mostly by households through out-of-pocket (OOP) payments at the time of illness. To protect poor families, the Indian government launched a national health insurance scheme (RSBY). Those below the national poverty line (BPL) are eligible to join the RSBY. The premium is heavily subsidised by the government. The enrolled members receive a card and can avail of free hospitalisation care up to a maximum of US$ 600 per family per year. The hospitals are reimbursed by the insurance companies. The objective of our study was to analyse the extent to which RSBY contributes to universal health coverage by protecting families from making OOP payments. A two-stage stratified sampling technique was used to identify eligible BPL families in Patan district of <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. Initially, all 517 villages were listed and 78 were selected randomly. From each of these villages, 40 BPL households were randomly selected and a structured questionnaire was administered. Interviews and discussions were also conducted among key stakeholders. Our sample contained 2,920 households who had enrolled in the RSBY; most were from the poorer sections of society. The average hospital admission rate for the period 2010-2011 was 40/1,000 enrolled. Women, elderly and those belonging to the lowest caste had a higher hospitalisation rate. Forty four per cent of patients who had enrolled in RSBY and had used the RSBY card still faced OOP payments at the time of hospitalisation. The median OOP payment for the above patients was US$ 80 (interquartile range, $16-$200) and was similar in both government and private hospitals. Patients incurred OOP payments mainly because they were asked to purchase medicines and diagnostics, though the same were included in the benefit package. While the RSBY has managed to include the poor under its umbrella, it has provided only partial financial coverage. Nearly 60% of insured and admitted patients made OOP payments. We plea for better</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22293101','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22293101"><span>Prevalence and characteristics of Molar Incisor Hypomineralisation (MIH) in the child population residing in Gandhinagar, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Parikh, D R; Ganesh, M; Bhaskar, V</p> <p>2012-02-01</p> <p>Most prevalence studies on Molar Incisor Hypomineralisation (MIH) have been carried out in European countries and data from Asia especially south Asian populations are lacking. To investigate the prevalence and clinical characteristics of MIH in children residing in a western region of <span class="hlt">India</span>. A cross-sectional survey including 1,366 children from 5 age cohorts, 8-12 years, studying in primary schools or attending the University Department, was carried out in the area of Gandhinagar, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. The dental examination was performed by a single well-trained and calibrated examiner in day light conditions. Full mouth inspection of wet teeth was conducted using the EAPD 2003 criteria for diagnosis of MIH. Results were recorded and statistically analysed using Chi-square test, independent sample t-test and Pearson correlations. Prevalence of MIH was 9.2% in the examined population. Males and females were equally affected. Among 12 index teeth involved in the examination, the most commonly affected were in descending order 46, 36, 16, 11 [FDI] and the least 42, 32, and 22. 17.4% of the cases revealed only molars involved, the remaining 72.6% having both molars and incisors affected; all four first permanent molars showed in 23% of the cases while no cases of only affected incisors were found. Of the MIH teeth 77.3% revealed mild defects and 22.7% severe defects. All incisors were mildly affected, as compared with only 67.1% of the molars, the remaining 32.9% being severely affected. As age increased, a statistically significant larger total number and severity level of affected teeth were recorded. Prevalence of MIH using EAPD 2003 criteria was found to be similar to other studies evaluating children in different geographic locations such as Europe, South America etc. Using the EAPD standardised criteria, more studies should be conducted in other Indian regions, in order to further evaluate prevalence, characteristics and treatment needs for this clinically demanding</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001AGUFM.S32A0627F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001AGUFM.S32A0627F"><span>Earth-Atmospheric Coupling Prior to Strong <span class="hlt">Earthquakes</span> Analyzed by IR Remote Sensing Data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Freund, F.; Ouzounov, D.</p> <p>2001-12-01</p> <p>Earth-atmosphere interactions during major <span class="hlt">earthquakes</span> (M>5) are the subject of this study. A mechanism has recently been proposed to account for the appearance of hole-type electronic charge carriers in rocks subjected to transient stress [Freund, 2000]. If such charge carriers are activated in the crust prior to large <span class="hlt">earthquakes</span>, the predictable consequences are: injection of currents into the rocks, low frequency electromagnetic emission, changes in ground potentials, corona discharges with attendant light emission from high points at the surface of the Earth, and possibly an enhanced emission in the 8-12 μ m region similar to the thermal emission observed during laboratory rock deformation experiments [Geng et al., 1999]. Using data from MODIS (Moderate Resolution Imaging Spectroradiometer) and ASTER (Advanced Spaceborne Thermal Emission & Reflection radiometer) onboard NASA's TERRA satellite launched in Dec. 1999 we have begun analyzing vertical atmospheric profiles, land surface and kinetic temperatures. We looked for correlations between atmospheric dynamics and solid Earth processes prior to the Jan. 13, 2001 <span class="hlt">earthquake</span> in El Salvador (M=7.6) and the Jan. 26, 2001 <span class="hlt">Gujarat</span> <span class="hlt">earth-quake</span> in <span class="hlt">India</span> (M=7.7). With MODIS covering the entire Earth every 1-2 days in 36 wavelength bands (20 visible and 16 infrared) at different spatial resolutions (250 m, 500 m, and 1 km) we find evidence for a thermal anomaly pattern related to the pre-seismic activity. We also find evidence for changes in the aerosol content and atmospheric instability parameters, possibly due to changes in the ground potential that cause ion emission and lead to the formation of a thin near-ground aerosol layer. We analyze the aerosol content, atmospheric pressure, moisture profile and lifted index.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AdSpR..56.1613B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AdSpR..56.1613B"><span>Spectral pathways for exploration of secondary uranium: An investigation in the desertic tracts of Rajasthan and <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bharti, Rishikesh; Kalimuthu, R.; Ramakrishnan, D.</p> <p>2015-10-01</p> <p>This study aims at identifying potential zones of secondary uranium enrichment using hyperspectral remote sensing, γ-ray spectrometry, fluorimetry and geochemical techniques in the western Rajasthan and northern <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. The investigated area has suitable source rocks, conducive past-, and present-climate that can facilitate such enrichment. This enrichment process involves extensive weathering of uranium bearing source rocks, leaching of uranyl compounds in groundwater, and their precipitation in chemical deltas along with duricrusts like calcretes and gypcretes. Spatial distribution of groundwater calcretes (that are rich in Mg-calcite) and gypcretes (that are rich in gypsum) along palaeochannels and chemical deltas were mapped using hyperspectral remote sensing data based on spectral absorptions in 1.70 μm, 2.16 μm, 2.21 μm, 2.33 μm, 2.44 μm wavelength regions. Subsequently based on field radiometric survey, zones of U anomalies were identified and samples of duricrusts and groundwater were collected for geochemical analyses. Anomalous concentration of U (2345.7 Bq/kg) and Th (142.3 Bq/kg) are observed in both duricrusts and groundwater (U-1791 μg/l, Th-34 μg/l) within the palaeo-delta and river confluence. The estimated carnotite Solubility Index also indicates the secondary enrichment of U and the likelihood of occurrence of an unconventional deposit.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26062528','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26062528"><span>Perceived Stress and Professional Quality of Life in Neonatal Intensive Care Unit Nurses in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Amin, Amee A; Vankar, Jagdish R; Nimbalkar, Somashekhar M; Phatak, Ajay G</p> <p>2015-11-01</p> <p>To study the levels of perceived stress in Neonatal Intensive Care Unit (NICU) nurses and its association with professional quality of life domains viz. compassion satisfaction, burnout and secondary trauma. In this multicenter, cross sectional study, data was collected by surveying 129 nurses from nine NICUs across six cities of <span class="hlt">Gujarat</span>, <span class="hlt">India</span> using demographic questionnaire, Perceived Stress Scale (PSS14) and Professional Quality of Life Scale (ProQOL5) during July to September 2013. Descriptive statistics, correlation coefficient and multiple regression were used for analysis. The mean (SD) age of participants was 28.37 (8.20) y. Most were single, satisfied with salary benefits and reported 'good' to 'excellent' relationships at work. The mean (SD) duration of duty hours was 8.12 (0.76) h and 43.6% were attending to more than 4 patients/shift. The mean (SD) perceived stress level was 22.19 (7.17) [Range: 3 to 39]. High compassion satisfaction, high burnout, and high secondary traumatic stress were reported by 25 (19.4%), 30 (23.3%) and 30 (23.3%) nurses respectively. PSS14 was negatively correlated with compassion satisfaction (r = -0.28) and positively correlated with burnout (r = 0.43) and secondary traumatic stress (r = 0.24). Most of the nurses (91, 70.5%) were identified as perceiving moderate to high stress. Professional quality of life domains correlated with perceived stress. There is further need to study domains influencing NICU nurses' professional QOL. Identifying stress and QOL issues in NICU nurses can help formulate relevant policies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JGRB..119.6650C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JGRB..119.6650C"><span>Active faulting in apparently stable peninsular <span class="hlt">India</span>: Rift inversion and a Holocene-age great <span class="hlt">earthquake</span> on the Tapti Fault</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Copley, Alex; Mitra, Supriyo; Sloan, R. Alastair; Gaonkar, Sharad; Reynolds, Kirsty</p> <p>2014-08-01</p> <p>We present observations of active faulting within peninsular <span class="hlt">India</span>, far from the surrounding plate boundaries. Offset alluvial fan surfaces indicate one or more magnitude 7.6-8.4 thrust-faulting <span class="hlt">earthquakes</span> on the Tapti Fault (Maharashtra, western <span class="hlt">India</span>) during the Holocene. The high ratio of fault displacement to length on the alluvial fan offsets implies high stress-drop faulting, as has been observed elsewhere in the peninsula. The along-strike extent of the fan offsets is similar to the thickness of the seismogenic layer, suggesting a roughly equidimensional fault rupture. The subsiding footwall of the fault is likely to have been responsible for altering the continental-scale drainage pattern in central <span class="hlt">India</span> and creating the large west flowing catchment of the Tapti river. A preexisting sedimentary basin in the uplifting hanging wall implies that the Tapti Fault was active as a normal fault during the Mesozoic and has been reactivated as a thrust, highlighting the role of preexisting structures in determining the rheology and deformation of the lithosphere. The slip sense of faults and <span class="hlt">earthquakes</span> in <span class="hlt">India</span> suggests that deformation south of the Ganges foreland basin is driven by the compressive force transmitted between <span class="hlt">India</span> and the Tibetan Plateau. The along-strike continuation of faulting to the east of the Holocene ruptures we have studied represents a significant seismic hazard in central <span class="hlt">India</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3943149','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3943149"><span>Phenotype frequencies of blood group systems (Rh, Kell, Kidd, Duffy, MNS, P, Lewis, and Lutheran) in blood donors of south <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Kahar, Manoj A.; Patel, Rajnikant. D.</p> <p>2014-01-01</p> <p>Background: This is the first study on phenotype frequencies of various blood group systems in blood donors of south <span class="hlt">Gujarat</span>, <span class="hlt">India</span> using conventional tube technique. Material and Methods: A total of 115 “O” blood group donors from three different blood banks of south <span class="hlt">Gujarat</span> were typed for D, C, c, E, e, K, Jka, Lea, Leb, P1, M, and N antigens using monoclonal antisera and k, Kpa, Kpb, Fya,Fyb, Jkb, S,s, Lua, and Lub antigens were typed using polyclonal antisera employing Indirect Antiglobulin Test. Antigens and phenotype frequencies were expressed as percentages. Results: From the 115 blood donor samples used for extended antigen typing in the Rh system, e antigen was found in 100% donors, followed by D [84.35%], C [81.74%], c [56.32%], and E [21.74%] with DCe/DCe (R1 R1, 40.87%) as the most common phenotype. k was found to be positive in 100% of donors and no K+k- phenotype was found in Kell system. For Kidd and Duffy blood group system, Jk(a+b+) and Fy(a-b-) were the most common phenotypes with frequency of 52.17% and 48.69%, respectively. In the MNS system, 39.13% donors were typed as M+N+, 37.39% as M+N-, and 23.48% as M-N+. S+s+ was found in 24.35% of donors, S+s- in 8.69%, and S-s+ as the commonest amongst donors with 66.96%. No Lu(a+b+) or Lu(a+b-) phenotypes were detected in 115 donors typed for Lutheran antigens. A rare Lu(a-b-) phenotype was found in 2.61% donors. Conclusion: Data base for antigen frequency of various blood group systems in local donors help provide antigen negative compatible blood units to patients with multiple antibodies in order to formulate in-house red cells for antibody detection and identification and for preparing donor registry for rare blood groups. PMID:24678176</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T43B0678R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T43B0678R"><span><span class="hlt">Earthquakes</span> of Garhwal Himalaya region of NW Himalaya, <span class="hlt">India</span>: A study of relocated <span class="hlt">earthquakes</span> and their seismogenic source and stress</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>R, A. P.; Paul, A.; Singh, S.</p> <p>2017-12-01</p> <p>Since the continent-continent collision 55 Ma, the Himalaya has accommodated 2000 km of convergence along its arc. The strain energy is being accumulated at a rate of 37-44 mm/yr and releases at time as <span class="hlt">earthquakes</span>. The Garhwal Himalaya is located at the western side of a Seismic Gap, where a great <span class="hlt">earthquake</span> is overdue atleast since 200 years. This seismic gap (Central Seismic Gap: CSG) with 52% probability for a future great <span class="hlt">earthquake</span> is located between the rupture zones of two significant/great <span class="hlt">earthquakes</span>, viz. the 1905 Kangra <span class="hlt">earthquake</span> of M 7.8 and the 1934 Bihar-Nepal <span class="hlt">earthquake</span> of M 8.0; and the most recent one, the 2015 Gorkha <span class="hlt">earthquake</span> of M 7.8 is in the eastern side of this seismic gap (CSG). The Garhwal Himalaya is one of the ideal locations of the Himalaya where all the major Himalayan structures and the Himalayan Seimsicity Belt (HSB) can ably be described and studied. In the present study, we are presenting the spatio-temporal analysis of the relocated local micro-moderate <span class="hlt">earthquakes</span>, recorded by a seismicity monitoring network, which is operational since, 2007. The <span class="hlt">earthquake</span> locations are relocated using the HypoDD (double difference hypocenter method for <span class="hlt">earthquake</span> relocations) program. The dataset from July, 2007- September, 2015 have been used in this study to estimate their spatio-temporal relationships, moment tensor (MT) solutions for the <span class="hlt">earthquakes</span> of M>3.0, stress tensors and their interactions. We have also used the composite focal mechanism solutions for small <span class="hlt">earthquakes</span>. The majority of the MT solutions show thrust type mechanism and located near the mid-crustal-ramp (MCR) structure of the detachment surface at 8-15 km depth beneath the outer lesser Himalaya and higher Himalaya regions. The prevailing stress has been identified to be compressional towards NNE-SSW, which is the direction of relative plate motion between the <span class="hlt">India</span> and Eurasia continental plates. The low friction coefficient estimated along with the stress inversions</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23555130','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23555130"><span>A comparative study on the <span class="hlt">Earthquake</span> Information Management Systems (EIMS) in <span class="hlt">India</span>, Afghanistan and Iran.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ajami, Sima</p> <p>2012-01-01</p> <p>Damages and loss of life sustained during an <span class="hlt">earthquake</span> results from falling structures and flying glass and objects. To address these and other problems, new information technology and systems as a means can improve crisis management and crisis response. The most important factor for managing the crisis depends on our readiness before disasters by useful data. This study aimed to determine the <span class="hlt">Earthquake</span> Information Management System (EIMS) in <span class="hlt">India</span>, Afghanistan and Iran, and describe how we can reduce destruction by EIMS in crisis management. This study was an analytical comparison in which data were collected by questionnaire, observation and checklist. The population was EIMS in selected countries. Sources of information were staff in related organizations, scientific documentations and Internet. For data analysis, Criteria Rating Technique, Delphi Technique and descriptive methods were used. Findings showed that EIMS in <span class="hlt">India</span> (Disaster Information Management System), Afghanistan (Management Information for Natural Disasters) and Iran are decentralized. The Indian state has organized an expert group to inspect issues about disaster decreasing strategy. In Iran, there was no useful and efficient EIMS to evaluate <span class="hlt">earthquake</span> information. According to outcomes, it is clear that an information system can only influence decisions if it is relevant, reliable and available for the decision-makers in a timely fashion. Therefore, it is necessary to reform and design a model. The model contains responsible organizations and their functions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3410214','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3410214"><span>Prevalence of dental fluorosis & dental caries in association with high levels of drinking water fluoride content in a district of <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Kotecha, P.V.; Patel, S.V.; Bhalani, K.D.; Shah, D.; Shah, V.S.; Mehta, K.G.</p> <p>2012-01-01</p> <p>Background & objectives: Endemic fluorosis resulting from high fluoride concentration in groundwater is a major public health problem in <span class="hlt">India</span>. This study was carried out to measure and compare the prevalence of dental fluorosis and dental caries in the population residing in high and normal level of fluoride in their drinking water in Vadodara district, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. Methods: A cross-sectional study was conducted in Vadodara district, six of the 261 villages with high fluoride level and five of 1490 with normal fluoride level in drinking water were selected. The data collection was made by house-to-house visits twice during the study period. Results: The dental fluorosis prevalence in high fluoride area was 59.31 per cent while in normal fluoride area it was 39.21 per cent. The prevalence of dental caries in high fluoride area was 39.53 per cent and in normal fluoride area was 48.21 per cent with CI 6.16 to 11.18. Dental fluorosis prevalence was more among males as compared to females. Highest prevalence of dental fluorosis was seen in 12-24 yr age group. Interpretation & conclusions: The risk of dental fluorosis was higher in the areas showing more fluoride content in drinking water and to a lesser degree of dental caries in the same area. High fluoride content is a risk factor for dental fluorosis and problem of dental fluorosis increased with passage of time suggesting that the fluoride content in the water has perhaps increased over time. Longitudinal studies should be conducted to confirm the findings. PMID:22825606</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22825606','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22825606"><span>Prevalence of dental fluorosis & dental caries in association with high levels of drinking water fluoride content in a district of <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kotecha, P V; Patel, S V; Bhalani, K D; Shah, D; Shah, V S; Mehta, K G</p> <p>2012-06-01</p> <p>Endemic fluorosis resulting from high fluoride concentration in groundwater is a major public health problem in <span class="hlt">India</span>. This study was carried out to measure and compare the prevalence of dental fluorosis and dental caries in the population residing in high and normal level of fluoride in their drinking water in Vadodara district, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. A cross-sectional study was conducted in Vadodara district, six of the 261 villages with high fluoride level and five of 1490 with normal fluoride level in drinking water were selected. The data collection was made by house-to-house visits twice during the study period. The dental fluorosis prevalence in high fluoride area was 59.31 per cent while in normal fluoride area it was 39.21 per cent. The prevalence of dental caries in high fluoride area was 39.53 per cent and in normal fluoride area was 48.21 per cent with CI 6.16 to 11.18. Dental fluorosis prevalence was more among males as compared to females. Highest prevalence of dental fluorosis was seen in 12-24 yr age group. The risk of dental fluorosis was higher in the areas showing more fluoride content in drinking water and to a lesser degree of dental caries in the same area. High fluoride content is a risk factor for dental fluorosis and problem of dental fluorosis increased with passage of time suggesting that the fluoride content in the water has perhaps increased over time. Longitudinal studies should be conducted to confirm the findings.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70030135','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70030135"><span>Quantifying the media bias in intensity surveys: Lessons from the 2001 Bhuj, <span class="hlt">India</span>, <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hough, S.E.; Pande, P.</p> <p>2007-01-01</p> <p>Many seismologists have looked at the 26 January 2001 Bhuj <span class="hlt">earthquake</span> as a key modern calibration event that could be used to improve estimates of magnitudes of large historic mainshocks in stable continental regions. Since no instrumental data are available for important historic events such as the 1819 Allah Bund, <span class="hlt">India</span>, and the 1811-1812 New Madrid, central U.S. mainshocks, calibration hinges on comparisons of the macroseismic effects of these <span class="hlt">earthquakes</span> with those of comparable modern <span class="hlt">earthquakes</span> for which a reliable, instrumentally determined moment magnitude is available. However, although such a comparison is conceptually straightforward, in practice it is complicated by potentially significant inconsistencies in methods used to quantify macroseismic effects in different regions and/or times. For the Bhuj <span class="hlt">earthquake</span>, extensive intensity data sets have been compiled and published from both media accounts and detailed direct surveys. Comparing the two provides a quantification of the previously suspected media bias, whereby <span class="hlt">earthquake</span> effects can be exaggerated in media accounts. This bias is a strong function of intensity level, with substantial bias at the highest shaking levels and significantly less bias at low intensities. Because only sparse documentary data are in general available for older historic <span class="hlt">earthquakes</span>, the results of this study suggest that their inferred intensity distributions might be similarly biased. We further use the survey-based intensity values to develop a new relationship between intensities and ground motions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/16869355','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/16869355"><span>Managing hospital supplies: process reengineering at <span class="hlt">Gujarat</span> Cancer Research Institute, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ramani, K V</p> <p>2006-01-01</p> <p>Aims to give an overview of the re-engineering of processes and structures at <span class="hlt">Gujarat</span> Cancer Research Institute (GCRI), Ahmedabad. A general review of the design, development and implementation of reengineered systems in order to address concerns about the existing systems. Findings GCRI is a comprehensive cancer care center with 550 beds and well equipped with modern diagnostic and treatment facilities. It serves about 200,000 outpatients and 16,000 inpatients annually. The approach to a better management of hospital supplies led to the design, development, and implementation of an IT-based reengineered and integrated purchase and inventory management system. The new system has given GCRI a saving of about 8 percent of its annual costs of purchases, and improved the availability of materials to the user departments. Shows that the savings obtained are used not only for buying more hospital supplies, but also to buy better quality of hospital supplies, and thereby satisfactorily address the GCRI responsibility towards meeting its social obligations for cancer care.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=The%2bworld%2bof%2biPods&pg=3&id=EJ365297','ERIC'); return false;" href="https://eric.ed.gov/?q=The%2bworld%2bof%2biPods&pg=3&id=EJ365297"><span>Anand Niketan Ashram, Rangpur, <span class="hlt">India</span>: An Education for Meaningful Participation.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Desai, Prakash O.; Haggerson, Nelson L.</p> <p>1987-01-01</p> <p>Describes a visit to the Anand Niketan Ashram in the interior of the State of <span class="hlt">Gujarat</span> <span class="hlt">India</span>, an internationally known school with a model education for meaningful citizen participation. Explores the program's philosophy activities and describes how the authors came together to have this experience and write this article. (BSR)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27340871','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27340871"><span>Bottleneck analysis and strategic planning using Tanahashi model for childhood diarrhea management in <span class="hlt">Gujarat</span>, Western <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rupani, Mihir Prafulbhai; Gaonkar, Narayan T; Bhatt, Gneyaa S</p> <p>2016-10-01</p> <p>In spite of continued efforts, <span class="hlt">India</span> is still lagging behind in achieving its MDG goals. The objectives of this study were to identify stake-holders who have a role to play in childhood diarrhea management, to identify gaps in childhood diarrhea management and to propose strategic options for relieving these gaps. Bottleneck analysis exercise was carried out based on the Tanahashi model in six High Priority Districts (HPDs) of <span class="hlt">Gujarat</span> in period between July-November 2013. The major bottlenecks identified for Childhood Diarrhea management were poor demand generation, unsafe drinking water, poor access to improved sanitation facility and lack of equitable distribution and replenishment mechanisms for Oral Rehydration Solution (ORS) packets and Zinc tablets till the front-line worker level. The main strategic options that were suggested for relieving these bottlenecks were Zinc-ORS roll out in scale-up districts, develop Information Education Communication/Behaviour Change Communication (IEC/BCC) plan for childhood diarrhea management at state/district level, use of Drug Logistics Information Management System (DLIMS) software for supply chain management of Zinc-ORS, strengthening of chlorination activity at household level, monitoring implementation of Nirmal Bharat Abhiyaan (NBA) for constructing improved sanitation facilities at household level and to develop an IEC/BCC plan for hygiene promotion and usage of sanitary latrines. Use of Zinc tablets need to be intensified through an effective scale-up. Adequate demand generation activity is needed. There is need to address safe drinking water and improved sanitation measures at household levels. Multi-sectoral engagements and ownership of Zinc-ORS program is the need of the hour. Copyright © 2016 Elsevier Ltd. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26825366','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26825366"><span>Statewide program to promote institutional delivery in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: who participates and the degree of financial subsidy provided by the Chiranjeevi Yojana program.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sidney, Kristi; Iyer, Veena; Vora, Kranti; Mavalankar, Dileep; De Costa, Ayesha</p> <p>2016-01-27</p> <p>The Chiranjeevi Yojana (CY) is a large public-private partnership program in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, under which the state pays private sector obstetricians to provide childbirth services to poor and tribal women. The CY was initiated statewide in 2007 because of the limited ability of the public health sector to provide emergency obstetric care and high out-of-pocket expenditures in the private sector (where most qualified obstetricians work), creating financial access barriers for poor women. Despite a million beneficiaries, there have been few reports studying CY, particularly the proportion of vulnerable women being covered, the expenditures they incur in connection with childbirth, and the level of subsidy provided to beneficiaries by the program. Cross-sectional facility based the survey of participants in three districts of <span class="hlt">Gujarat</span> in 2012-2013. Women were interviewed to elicit sociodemographic characteristics, out-of-pocket expenditures, and CY program details. Descriptive statistics, chi square, and a multivariable logistic regression were performed. Of the 901 women surveyed in 129 facilities, 150 (16 %) were CY beneficiaries; 336 and 415 delivered in government and private facilities, respectively. Only 36 (24 %) of the 150 CY beneficiaries received a completely cashless delivery. Median out-of-pocket for vaginal/cesarean delivery among CY beneficiaries was $7/$71. The median degree of subsidy for women in CY who delivered vaginally/cesarean was 85/71 % compared to out-of-pocket expenditure of $44/$208 for vaginal/cesarean delivery paid by non-program beneficiaries in the private health sector. CY beneficiaries experienced a substantially subsidized childbirth compared to women who delivered in non-accredited private facilities. However, despite the government's efforts at increasing access to delivery services for poor women in the private sector, uptake was low and very few women experienced a cashless delivery. While the long-term focus remains on</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018CG....113....1Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018CG....113....1Z"><span>Forecasting of future <span class="hlt">earthquakes</span> in the northeast region of <span class="hlt">India</span> considering energy released concept</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zarola, Amit; Sil, Arjun</p> <p>2018-04-01</p> <p>This study presents the forecasting of time and magnitude size of the next <span class="hlt">earthquake</span> in the northeast <span class="hlt">India</span>, using four probability distribution models (Gamma, Lognormal, Weibull and Log-logistic) considering updated <span class="hlt">earthquake</span> catalog of magnitude Mw ≥ 6.0 that occurred from year 1737-2015 in the study area. On the basis of past seismicity of the region, two types of conditional probabilities have been estimated using their best fit model and respective model parameters. The first conditional probability is the probability of seismic energy (e × 1020 ergs), which is expected to release in the future <span class="hlt">earthquake</span>, exceeding a certain level of seismic energy (E × 1020 ergs). And the second conditional probability is the probability of seismic energy (a × 1020 ergs/year), which is expected to release per year, exceeding a certain level of seismic energy per year (A × 1020 ergs/year). The logarithm likelihood functions (ln L) were also estimated for all four probability distribution models. A higher value of ln L suggests a better model and a lower value shows a worse model. The time of the future <span class="hlt">earthquake</span> is forecasted by dividing the total seismic energy expected to release in the future <span class="hlt">earthquake</span> with the total seismic energy expected to release per year. The epicentre of recently occurred 4 January 2016 Manipur <span class="hlt">earthquake</span> (M 6.7), 13 April 2016 Myanmar <span class="hlt">earthquake</span> (M 6.9) and the 24 August 2016 Myanmar <span class="hlt">earthquake</span> (M 6.8) are located in zone Z.12, zone Z.16 and zone Z.15, respectively and that are the identified seismic source zones in the study area which show that the proposed techniques and models yield good forecasting accuracy.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_5");'>5</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li class="active"><span>7</span></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_7 --> <div id="page_8" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="141"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3577382','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3577382"><span>A comparative study on the <span class="hlt">Earthquake</span> Information Management Systems (EIMS) in <span class="hlt">India</span>, Afghanistan and Iran</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ajami, Sima</p> <p>2012-01-01</p> <p>Context: Damages and loss of life sustained during an <span class="hlt">earthquake</span> results from falling structures and flying glass and objects. To address these and other problems, new information technology and systems as a means can improve crisis management and crisis response. The most important factor for managing the crisis depends on our readiness before disasters by useful data. Aims: This study aimed to determine the <span class="hlt">Earthquake</span> Information Management System (EIMS) in <span class="hlt">India</span>, Afghanistan and Iran, and describe how we can reduce destruction by EIMS in crisis management. Materials and Methods: This study was an analytical comparison in which data were collected by questionnaire, observation and checklist. The population was EIMS in selected countries. Sources of information were staff in related organizations, scientific documentations and Internet. For data analysis, Criteria Rating Technique, Delphi Technique and descriptive methods were used. Results: Findings showed that EIMS in <span class="hlt">India</span> (Disaster Information Management System), Afghanistan (Management Information for Natural Disasters) and Iran are decentralized. The Indian state has organized an expert group to inspect issues about disaster decreasing strategy. In Iran, there was no useful and efficient EIMS to evaluate <span class="hlt">earthquake</span> information. Conclusions: According to outcomes, it is clear that an information system can only influence decisions if it is relevant, reliable and available for the decision-makers in a timely fashion. Therefore, it is necessary to reform and design a model. The model contains responsible organizations and their functions. PMID:23555130</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018E%26ES..154a2001P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018E%26ES..154a2001P"><span>GIS-based approach for the evaluation of offshore wind power potential for <span class="hlt">Gujarat</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Patel, Dhrumin; Nagababu, Garlapati; Radadia, Nishil; Parsana, Sohil; Sheth, Mohak; Sheth, Nisarg</p> <p>2018-05-01</p> <p>In the current global scenario, <span class="hlt">India</span> is increasing its focus towards the methods to enrich the benefits of non-renewable energy sources as much as possible due to their key advantage of having low carbon footprint. <span class="hlt">India</span> has already emerged as a key global player in on-shore wind energy and to achieve its annual wind energy production demand of 50 GWh, avenues other than current options have been researched on. Offshore wind energy has experienced remarkable growth worldwide but has not yet been harnessed sufficiently in <span class="hlt">India</span>, despite addressing many of environmental and economic concerns. The present study focuses on offshore wind resource assessment on Indian exclusive economic zone (EEZ) around <span class="hlt">Gujarat</span> region. The geographical information system (GIS) methodology has been used to develop maps of wind speed, power density and capacity factor maps. Further, careful consideration has been accorded for expulsion of marine protected areas, shipping transportation lines, fishing zones, and migratory bird movements. The resultant available area has been considered for annual energy production considering data from Siemens Wind Turbine 3.6. The results obtained shows that offshore wind energy can offset twice the annual energy demand of entire country with a potential energy production of more than 2580 TWh.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28603456','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28603456"><span>Cost-effectiveness analysis of the diarrhea alleviation through zinc and oral rehydration therapy (DAZT) program in rural <span class="hlt">Gujarat</span> <span class="hlt">India</span>: an application of the net-benefit regression framework.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Shillcutt, Samuel D; LeFevre, Amnesty E; Fischer-Walker, Christa L; Taneja, Sunita; Black, Robert E; Mazumder, Sarmila</p> <p>2017-01-01</p> <p>This study evaluates the cost-effectiveness of the DAZT program for scaling up treatment of acute child diarrhea in <span class="hlt">Gujarat</span> <span class="hlt">India</span> using a net-benefit regression framework. Costs were calculated from societal and caregivers' perspectives and effectiveness was assessed in terms of coverage of zinc and both zinc and Oral Rehydration Salt. Regression models were tested in simple linear regression, with a specified set of covariates, and with a specified set of covariates and interaction terms using linear regression with endogenous treatment effects was used as the reference case. The DAZT program was cost-effective with over 95% certainty above $5.50 and $7.50 per appropriately treated child in the unadjusted and adjusted models respectively, with specifications including interaction terms being cost-effective with 85-97% certainty. Findings from this study should be combined with other evidence when considering decisions to scale up programs such as the DAZT program to promote the use of ORS and zinc to treat child diarrhea.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24749203','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24749203"><span>Physico-chemical quality of drinking water in villages of Primary Health Centre, Waghodia, <span class="hlt">Gujarat</span> (<span class="hlt">India</span>).</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Desai, Gaurav; Vasisth, Smriti; Patel, Maharshi; Mehta, Vaibhav; Bhavsar, Bharat</p> <p>2012-07-01</p> <p>16 water samples were collected to study the physical and chemical quality of water of main source of drinking water in the villages of Primary Health Centre, Waghodia of Vadodara district of <span class="hlt">Gujarat</span>. The values recommended by Indian Standard for Drinking Water (IS 10500:1991) were used for comparison of observed values. The study indicates that the contamination problem in these villages is not alarming at present, but Waghodia being industrial town, ground water quality may deteriorate with passage of time, which needs periodical monitoring. The study provides the local area baseline data which may be useful for the comparison of future study.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JSeis..20..733R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JSeis..20..733R"><span>Liquefaction record of the great 1934 <span class="hlt">earthquake</span> predecessors from the north Bihar alluvial plains of <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rajendran, C. P.; John, Biju; Rajendran, Kusala; Sanwal, Jaishri</p> <p>2016-07-01</p> <p>The great 1934 Himalayan <span class="hlt">earthquake</span> of moment magnitude (Mw) 8.1 generated a large zone of ground failure and liquefaction in north Bihar, <span class="hlt">India</span>, in addition to the <span class="hlt">earthquakes</span> of 1833 (Mw ~7.7) and 1988 (Mw 6.7) that have also impacted this region. Here, we present the results of paleoliquefaction investigations from four sites in the plains of north Bihar and one in eastern Uttar Pradesh. The liquefaction features generated by successive <span class="hlt">earthquakes</span> were dated at AD 829-971, 886-1090, 907-1181, 1130-1376, 1112-1572, 1492-1672, 1733-1839, and 1814-1854. One of the liquefaction events dated at AD 829-971, 886-1090, and 907-1181 may correlate with the great <span class="hlt">earthquake</span> of AD ~1100, recognized in an earlier study from the sections across the frontal thrust in central eastern Nepal. Two late medieval liquefaction episodes of AD 1130-1376 and 1492-1672 were also exposed in our sites. The sedimentary sections also revealed sandblows that can be attributed to the 1833 <span class="hlt">earthquake</span>, a lesser magnitude event compared to the 1934. Liquefactions triggered by the 1934 and 1988 <span class="hlt">earthquakes</span> were evident within the topmost level in some sections. The available data lead us to conjecture that a series of temporally close spaced <span class="hlt">earthquakes</span> of both strong and large types, not including the infrequent great <span class="hlt">earthquakes</span> like the 1934, have affected the Bihar Plains during the last 1500 years with a combined recurrence interval of 124 ± 63 years.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=state+AND+gender+AND+inequality+AND+india&id=EJ921173','ERIC'); return false;" href="https://eric.ed.gov/?q=state+AND+gender+AND+inequality+AND+india&id=EJ921173"><span>Girls' Education and Discursive Spaces for Empowerment: Perspectives from Rural <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Shah, Payal P.</p> <p>2011-01-01</p> <p>This article examines a national girls' education program and its role in addressing gender inequality in the Indian state of <span class="hlt">Gujarat</span>. In 2004, the Ministry of Education, Government of <span class="hlt">India</span>, enacted the Kasturba Gandhi Balika Vidyala (KGBV) program. As a national program designed to increase educational access for the most marginalized girls, the…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PApGe.tmp.1305M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PApGe.tmp.1305M"><span>Magnetotelluric Investigations in Tuwa-Godhra Region, <span class="hlt">Gujarat</span> (<span class="hlt">India</span>)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mohan, Kapil; Chaudhary, Peush; Kumar, G. Pavan; Kothyari, Girish Ch.; Choudhary, Virender; Nagar, Mehul; Patel, Pruthul; Gandhi, Drasti; Kushwaha, Dilip; Rastogi, B. K.</p> <p>2018-05-01</p> <p>Magnetotelluric (MT) data have been acquired at 40 locations in Tuwa and its surrounding region (200 km east of Ahmedabad and 15 km north-northwest of Godhra) in the Mainland <span class="hlt">Gujarat</span> with an average station spacing of 1.5 km. MT impedance tensors have been estimated in the period range of 0.001-100 s. The data have been modeled using non-linear conjugate gradient scheme taking both apparent resistivity and phase into account. From the 2D models of the MT data, the weathered granite with Quaternary sediments (with resistivity of < 700 Ω m) have been inferred up to a depth of 500 m followed by Godhra granite (having resistivity up to 105 Ω m) with a thickness 6.5 km. The Aravalli supergroup has been inferred below Godhra granite. The Lunavada group of rocks have been inferred in the eastern part of the study area (having resistivity value ranging from 103 to 104 Ω m) separated from the Godhra granite by a contact zone. The comparatively very low-resistivity rocks (< 400 Ω m) of Udaipur formation followed by Paleoproterozoic carbonate rocks with fluid have been inferred below 8-10 km depth. The percolation of water from the surface through the contact zone of Lunavada and Champaner groups has been suggested. The presence of hot water springs in 10 km SW from the center of the study area (at the contact zone of Godhra granite and basalt) might be due to the western trending lithostratigraphic slope, hydrostatic pressure generated due to heat produced from interaction of water with the carbonate rocks at deeper depth and high subsurface temperature due to high geothermal gradient. The segmented nature of Himmatnagar Fault (HnF) is identified in the central portion of the study area.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=PIA03403&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dearthquakes','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=PIA03403&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3Dearthquakes"><span>Liquefaction Effects from the Bhuj <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2001-01-01</p> <p><p/>These MISR images show the Kachchh region in the <span class="hlt">Gujarat</span> province of western <span class="hlt">India</span>. On January 26, 2001, a magnitude 7.7 <span class="hlt">earthquake</span> devastated this area, killing 20,000 people and destroying buildings, dams, and port facilities. The two upper MISR images are pre- and post-<span class="hlt">earthquake</span> scenes acquired on January 15 and January 31, 2001, respectively (Terra orbits 5736 and 5969). They are 'true-color' images made by combining the red, green and blue bands from the nadir (vertically down-looking) camera. The two lower views are 'false-color' images made by combining the red bands from three different cameras. Blue is assigned to the camera pointing 70 degrees forward (more sun-facing), green to the nadir camera, and red to the camera pointing 70 degrees aftward. Each of these images is about 275 kilometers wide by 218 kilometers high.<p/>The <span class="hlt">earthquake</span> epicenter was just below the southern tip of the large, white area on the right-hand side of the images, and about 70 kilometers northeast of the city of Bhuj. The <span class="hlt">earthquake</span> may have occurred on the Kachchh Mainland Fault, which extends from the region of the epicenter westward along the curved boundary between the darker brown region to the south and the lighter brown area north of it. The compressive stresses responsible for the <span class="hlt">earthquake</span> are related to the collision of <span class="hlt">India</span> with Asia and the resulting rise of the Himalayas to the northeast.<p/>That part of the Kachchh region which lies north of the Kachchh Mainland Fault includes the Banni Plains and the Rann of Kachchh. It is a low, flat basin characterized by salt pans and mud flats. The salt forms in the Rann of Kachchh as mineral-laden waters evaporate. The salt flats can be seen in the nadir images as highly reflective, white and gray areas. During the <span class="hlt">earthquake</span>, strong shaking produced liquefaction in the fine silts and sands below the water table in the Rann of Kachchh. This caused the mineral grains to settle and expel their interstitial water to the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5014265','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5014265"><span>Spatiotemporal Analysis of Malaria in Urban Ahmedabad (<span class="hlt">Gujarat</span>), <span class="hlt">India</span>: Identification of Hot Spots and Risk Factors for Targeted Intervention</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Parizo, Justin; Sturrock, Hugh J. W.; Dhiman, Ramesh C.; Greenhouse, Bryan</p> <p>2016-01-01</p> <p>The world population, especially in developing countries, has experienced a rapid progression of urbanization over the last half century. Urbanization has been accompanied by a rise in cases of urban infectious diseases, such as malaria. The complexity and heterogeneity of the urban environment has made study of specific urban centers vital for urban malaria control programs, whereas more generalizable risk factor identification also remains essential. Ahmedabad city, <span class="hlt">India</span>, is a large urban center located in the state of <span class="hlt">Gujarat</span>, which has experienced a significant Plasmodium vivax and Plasmodium falciparum disease burden. Therefore, a targeted analysis of malaria in Ahmedabad city was undertaken to identify spatiotemporal patterns of malaria, risk factors, and methods of predicting future malaria cases. Malaria incidence in Ahmedabad city was found to be spatially heterogeneous, but temporally stable, with high spatial correlation between species. Because of this stability, a prediction method utilizing historic cases from prior years and seasons was used successfully to predict which areas of Ahmedabad city would experience the highest malaria burden and could be used to prospectively target interventions. Finally, spatial analysis showed that normalized difference vegetation index, proximity to water sources, and location within Ahmedabad city relative to the dense urban core were the best predictors of malaria incidence. Because of the heterogeneity of urban environments and urban malaria itself, the study of specific large urban centers is vital to assist in allocating resources and informing future urban planning. PMID:27382081</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=caste+AND+system+AND+india&id=EJ1036563','ERIC'); return false;" href="https://eric.ed.gov/?q=caste+AND+system+AND+india&id=EJ1036563"><span>Beyond the Education Silo? Tackling Adolescent Secondary Education in Rural <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Kelly, Orla; Bhabha, Jacqueline</p> <p>2014-01-01</p> <p>In this paper we examine the factors contributing to gender inequality in secondary schooling in <span class="hlt">India</span> by critically reviewing the government's secondary education policy. Drawing on the findings of a study in rural <span class="hlt">Gujarat</span>, we couple this analysis with an examination of the gendered dynamics that restrict girls' ability to fully benefit from the…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017Tectp.714..133M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Tectp.714..133M"><span>Paleoseismic evidence of the CE 1505 (?) and CE 1803 <span class="hlt">earthquakes</span> from the foothill zone of the Kumaon Himalaya along the Himalayan Frontal Thrust (HFT), <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Malik, Javed N.; Naik, Sambit P.; Sahoo, Santiswarup; Okumura, Koji; Mohanty, Asmita</p> <p>2017-09-01</p> <p>The importance of understanding <span class="hlt">earthquake</span> sources in <span class="hlt">India</span> and Nepal was underscored by the disastrous 2015 <span class="hlt">earthquakes</span> of 25 April Gorkha (Mw 7.8) and 12 May Kodari (Mw 7.3, aftershock) in Nepal. The Kumaon-Garhwal segment experienced strong <span class="hlt">earthquakes</span> in CE 1505 and CE 1803, probably along the Himalayan Frontal Thrust (HFT). Of these, the CE 1505 was the greatest <span class="hlt">earthquake</span> reported from the region in historical chronicles. However, no surface ruptures related to either of 1505 or 1803 have been identified from the Kumaon-Garhwal segment, and an ambiguity remained about their ruptures dispite recent reports of CE 1505 surface rupture in Western Nepal. We used high-resolution satellite (CARTOSAT-1) data for mapping active fault traces and carried out paleoseismic studies to identify paleo-<span class="hlt">earthquakes</span> along the HFT. A trench excavated across the Kaladungi Fault (KF), a branching fault of HFT, revealed evidence of at least three <span class="hlt">earthquakes</span>. Event I (the oldest) occurred between BCE 467 and CE 570; Event II occurred between CE 1294-1587. We infer that the Event II was the most likely historically-reported, great Himalayan <span class="hlt">earthquake</span> of CE 1505. Event III occurred between CE 1750-1932, and may represent the large magnitude CE 1803 (7.5 > Mw < 8.0) <span class="hlt">earthquake</span>. Our findings not only help in understanding the frontal fault dynamics, but also may aid seismic hazard evaluation in <span class="hlt">India</span> and Nepal.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70042312','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70042312"><span>Intensity, magnitude, location and attenuation in <span class="hlt">India</span> for felt <span class="hlt">earthquakes</span> since 1762</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Szeliga, Walter; Hough, Susan; Martin, Stacey; Bilham, Roger</p> <p>2010-01-01</p> <p>A comprehensive, consistently interpreted new catalog of felt intensities for <span class="hlt">India</span> (Martin and Szeliga, 2010, this issue) includes intensities for 570 <span class="hlt">earthquakes</span>; instrumental magnitudes and locations are available for 100 of these events. We use the intensity values for 29 of the instrumentally recorded events to develop new intensity versus attenuation relations for the Indian subcontinent and the Himalayan region. We then use these relations to determine the locations and magnitudes of 234 historical events, using the method of Bakun and Wentworth (1997). For the remaining 336 events, intensity distributions are too sparse to determine magnitude or location. We evaluate magnitude and location accuracy of newly located events by comparing the instrumental- with the intensity-derived location for 29 calibration events, for which more than 15 intensity observations are available. With few exceptions, most intensity-derived locations lie within a fault length of the instrumentally determined location. For events in which the azimuthal distribution of intensities is limited, we conclude that the formal error bounds from the regression of Bakun and Wentworth (1997) do not reflect the true uncertainties. We also find that the regression underestimates the uncertainties of the location and magnitude of the 1819 Allah Bund <span class="hlt">earthquake</span>, for which a location has been inferred from mapped surface deformation. Comparing our inferred attenuation relations to those developed for other regions, we find that attenuation for Himalayan events is comparable to intensity attenuation in California (Bakun and Wentworth, 1997), while intensity attenuation for cratonic events is higher than intensity attenuation reported for central/eastern North America (Bakun et al., 2003). Further, we present evidence that intensities of intraplate <span class="hlt">earthquakes</span> have a nonlinear dependence on magnitude such that attenuation relations based largely on small-to-moderate <span class="hlt">earthquakes</span> may significantly</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70037226','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70037226"><span>Intensity, magnitude, location, and attenuation in <span class="hlt">India</span> for felt <span class="hlt">earthquakes</span> since 1762</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Szeliga, W.; Hough, S.; Martin, S.; Bilham, R.</p> <p>2010-01-01</p> <p>A comprehensive, consistently interpreted new catalog of felt intensities for <span class="hlt">India</span> (Martin and Szeliga, 2010, this issue) includes intensities for 570 <span class="hlt">earth-quakes</span>; instrumental magnitudes and locations are available for 100 of these events. We use the intensity values for 29 of the instrumentally recorded events to develop new intensity versus attenuation relations for the Indian subcontinent and the Himalayan region. We then use these relations to determine the locations and magnitudes of 234 historical events, using the method of Bakun and Wentworth (1997). For the remaining 336 events, intensity distributions are too sparse to determine magnitude or location. We evaluate magnitude and location accuracy of newly located events by comparing the instrumental-with the intensity-derived location for 29 calibration events, for which more than 15 intensity observations are available. With few exceptions, most intensity-derived locations lie within a fault length of the instrumentally determined location. For events in which the azimuthal distribution of intensities is limited, we conclude that the formal error bounds from the regression of Bakun and Wentworth (1997) do not reflect the true uncertainties. We also find that the regression underestimates the uncertainties of the location and magnitude of the 1819 Allah Bund <span class="hlt">earthquake</span>, for which a location has been inferred from mapped surface deformation. Comparing our inferred attenuation relations to those developed for other regions, we find that attenuation for Himalayan events is comparable to intensity attenuation in California (Bakun and Wentworth, 1997), while intensity attenuation for cratonic events is higher than intensity attenuation reported for central/eastern North America (Bakun et al., 2003). Further, we present evidence that intensities of intraplate <span class="hlt">earth-quakes</span> have a nonlinear dependence on magnitude such that attenuation relations based largely on small-to-moderate <span class="hlt">earthquakes</span> may significantly</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001AGUSM...S22A07B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001AGUSM...S22A07B"><span>Aftershocks of the <span class="hlt">India</span> Republic Day <span class="hlt">Earthquake</span>: the MAEC/ISTAR Temporary Seismograph Network</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bodin, P.; Horton, S.; Johnston, A.; Patterson, G.; Bollwerk, J.; Rydelek, P.; Steiner, G.; McGoldrick, C.; Budhbhatti, K. P.; Shah, R.; Macwan, N.</p> <p>2001-05-01</p> <p>The MW=7.7 Republic Day (26 January, 2001) <span class="hlt">earthquake</span> on the Kachchh in western <span class="hlt">India</span> initiated a strong sequence of small aftershocks. Seventeen days following the mainshock, we deployed a network of portable digital event recorders as a cooperative project of the Mid America <span class="hlt">Earthquake</span> Center in the US and the Institute for Scientific and Technological Advanced Research. Our network consisted of 8 event-triggered Kinemetrics K2 seismographs with 6 data channels (3 accelerometer, 3 Mark L-28/3d seismometer) sampled at 200 Hz, and one continuously-recording Guralp CMG40TD broad-band seismometer sampled at 220 Hz. This network was in place for 18 days. Underlying our network deployment was the notion that because of its tectonic and geologic setting the Republic Day <span class="hlt">earthquake</span> and its aftershocks might have source and/or propagation characteristics common to <span class="hlt">earthquakes</span> in stable continental plate-interiors rather than those on plate boundaries or within continental mobile belts. Thus, our goals were to provide data that could be used to compare the Republic Day <span class="hlt">earthquake</span> with other <span class="hlt">earthquakes</span>. In particular, the objectives of our network deployment were: (1) to characterize the spatial distribution and occurrence rates of aftershocks, (2) to examine source characteristics of the aftershocks (stress-drops, focal mechanisms), (3) to study the effect of deep unconsolidated sediment on wave propagation, and (4) to determine if other faults (notably the Allah Bundh) were simultaneously active. Most of our sites were on Jurassic bedrock, and all were either free-field, or on the floor of light structures built on rock or with a thin soil cover. However, one of our stations was on a section of unconsolidated sediments hundreds of meters thick adjacent to a site that was subjected to shaking-induced sediment liquefaction during the mainshock. The largest aftershock reported by global networks was an MW=5.9 event on January 28, prior to our deployment. The largest</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PIAHS.379..351M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PIAHS.379..351M"><span>Fluoride in groundwater: a case study in Precambrian terranes of Ambaji region, North <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mohan Pradhan, Rudra; Biswal, Tapas Kumar</p> <p>2018-06-01</p> <p>Fluoride is one of the critical ions that influence the groundwater quality. World Health Organization (WHO, 1970) and Bureau of Indian Standards (BIS, 1991) set an upper limit of 1.5 mg L-1 in F- concentration for drinking water purpose and above affects teeth and bones of humans. The presence of fluoride in groundwater is due to an interaction of groundwater and fluoride bearing rocks. Fluoride rich groundwater is well known in granitic aquifers in <span class="hlt">India</span> and elsewhere. Generally, the concentration of F- in groundwater is controlled by local geological setting; leaching and weathering of bedrock and climatic condition of an area. The main objective of the present study is to assess the hydrogeochemistry of groundwater and to understand the abundance of F- in groundwater in hard rock terranes of Ambaji region, North <span class="hlt">Gujarat</span>. A total of forty-three representative groundwater samples were collected and analyzed for major cations and anions using ICP-AES, Ion Chromatograph (Metrohm 883 Basic IC Plus) and titration methods. The F- concentration in groundwater of this study area ranges from 0.17 to 2.7 mg L-1. Among, twenty groundwater samples have fluoride exceeding the maximum permissible limit as per the BIS (1.5 mg L-1). It is also noticed that residents of this region are affected by dental fluorosis. The general order of the dominance of major cations and anions are Ca2+ > Mg2+ > Na+ > K+ and HCO3- > Cl- > F- respectively. Geochemical classification of groundwater shows most of the samples are the alkaline earth-bicarbonate type. The semi-arid climatic conditions of the region, the dominance of granitoid-granulite suite rocks and the fracture network in the disturbed and brittle zone has facilitated the development of potential aquifers and enrichment in F- concentration in this area. The concentration of fluoride is due to high evaporation rate, longer residence time in the aquifer zone, intensive and long term pumping for irrigation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=middle+AND+class+AND+india&pg=2&id=EJ881821','ERIC'); return false;" href="https://eric.ed.gov/?q=middle+AND+class+AND+india&pg=2&id=EJ881821"><span>Marital Ideoscapes in 21st-Century <span class="hlt">India</span>: Creative Combinations of Love and Responsibility</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Netting, Nancy S.</p> <p>2010-01-01</p> <p>Although arranged marriage has survived in <span class="hlt">India</span>, the custom is increasingly challenged by the current influx of new commodities, media, and ideas. Interviews with 15 male and 15 female unmarried professionals, age 22 to 29, in Vadodara, <span class="hlt">Gujarat</span>, showed that educated youth have moved beyond the conventional love-versus-arranged marriage dichotomy.…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=education+AND+child&pg=6&id=EJ960526','ERIC'); return false;" href="https://eric.ed.gov/?q=education+AND+child&pg=6&id=EJ960526"><span>Relationship between Household Literacy and Educational Engagement: Analysis of Data from Rajkot District, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Chudgar, Amita; Miller, Karyn; Kothari, Brij</p> <p>2012-01-01</p> <p>Household engagement in a child's education is a complex process; depending on the culture and the context, it may be revealed through a variety of behaviours. Using data from one district in rural <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, four indicators of a household's educational engagement were employed to investigate the relationship between household literacy levels…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25374099','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25374099"><span>Considerations of private sector obstetricians on participation in the state led "Chiranjeevi Yojana" scheme to promote institutional delivery in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: a qualitative study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ganguly, Parthasarathi; Jehan, Kate; de Costa, Ayesha; Mavalankar, Dileep; Smith, Helen</p> <p>2014-11-05</p> <p>In <span class="hlt">India</span> a lack of access to emergency obstetric care contributes to maternal deaths. In 2005 <span class="hlt">Gujarat</span> state launched a public-private partnership (PPP) programme, Chiranjeevi Yojana (CY), under which the state pays accredited private obstetricians a fixed fee for providing free intrapartum care to poor and tribal women. A million women have delivered under CY so far. The participation of private obstetricians in the partnership is central to the programme's effectiveness. We explored with private obstetricians the reasons and experiences that influenced their decisions to participate in the CY programme. In this qualitative study we interviewed 24 purposefully selected private obstetricians in <span class="hlt">Gujarat</span>. We explored their views on the scheme, the reasons and experiences leading up to decisions to participate, not participate or withdraw from the CY, as well as their opinions about the scheme's impact. We analysed data using the Framework approach. Participants expressed a tension between doing public good and making a profit. Bureaucratic procedures and perceptions of programme misuse seemed to influence providers to withdraw from the programme or not participate at all. Providers feared that participating in CY would lower the status of their practices and some were deterred by the likelihood of more clinically difficult cases among eligible CY beneficiaries. Some providers resented taking on what they saw as a state responsibility to provide safe maternity services to poor women. Younger obstetricians in the process of establishing private practices, and those in more remote, 'less competitive' areas, were more willing to participate in CY. Some doctors had reservations over the quality of care that doctors could provide given the financial constraints of the scheme. While some private obstetricians willingly participate in CY and are satisfied with its functioning, a larger number shared concerns about participation. Operational difficulties and a trust deficit</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24088383','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24088383"><span>The transition of childbirth practices among tribal women in <span class="hlt">Gujarat</span>, <span class="hlt">India</span> - a grounded theory approach.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sharma, Bharati; Giri, Gayatri; Christensson, Kyllike; K V, Ramani; Johansson, Eva</p> <p>2013-10-03</p> <p>Under the National Rural Health Mission, the current emphasis is on achieving universal institutional births through incentive schemes as part of reforms related to childbirth in <span class="hlt">India</span>. There has been rapid progress in achieving this goal. To understand the choices made as well as practices and perceptions related to childbirth amongst tribal women in <span class="hlt">Gujarat</span> and how these have been influenced by modernity in general and modernity brought in through maternal health policies. A model depicting the transition in childbirth practices amongst tribal women was constructed using the grounded theory approach with; 8 focus groups of women, 5 in depth interviews with traditional birth attendants, women, and service providers and field notes on informal discussions and observations. A transition in childbirth practices across generations was noted, i.e. a shift from home births attended by Traditional Birth Attendants (TBAs) to hospital births. The women and their families both adapted to and shaped this transition through a constant 'trade-off between desirable and essential'- the desirable being a traditional homebirth in secure surroundings and the essential being the survival of mother and baby by going to hospital. This transition was shaped by complex multiple factors: 1) Overall economic growth and access to modern medical care influencing women's choices, 2) External context in terms of the international maternal health discourses and national policies, especially incentive schemes for promoting institutional deliveries, 3) Socialisation into medical childbirth practices, through exposure to many years of free outreach services for maternal and child health, 4) Loss of self reliance in the community as a consequence of role redefinition and deskilling of the TBAs and 5) Cultural belief that intervention is necessary during childbirth aiding easy acceptance of medical interventions. In resource poor settings where choices are limited and mortality is high, hospital</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3826869','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3826869"><span>The transition of childbirth practices among tribal women in <span class="hlt">Gujarat</span>, <span class="hlt">India</span> - a grounded theory approach</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2013-01-01</p> <p>Background Under the National Rural Health Mission, the current emphasis is on achieving universal institutional births through incentive schemes as part of reforms related to childbirth in <span class="hlt">India</span>. There has been rapid progress in achieving this goal. To understand the choices made as well as practices and perceptions related to childbirth amongst tribal women in <span class="hlt">Gujarat</span> and how these have been influenced by modernity in general and modernity brought in through maternal health policies. Method A model depicting the transition in childbirth practices amongst tribal women was constructed using the grounded theory approach with; 8 focus groups of women, 5 in depth interviews with traditional birth attendants, women, and service providers and field notes on informal discussions and observations. Results A transition in childbirth practices across generations was noted, i.e. a shift from home births attended by Traditional Birth Attendants (TBAs) to hospital births. The women and their families both adapted to and shaped this transition through a constant ’trade-off between desirable and essential’- the desirable being a traditional homebirth in secure surroundings and the essential being the survival of mother and baby by going to hospital. This transition was shaped by complex multiple factors: 1) Overall economic growth and access to modern medical care influencing women’s choices, 2) External context in terms of the international maternal health discourses and national policies, especially incentive schemes for promoting institutional deliveries, 3) Socialisation into medical childbirth practices, through exposure to many years of free outreach services for maternal and child health, 4) Loss of self reliance in the community as a consequence of role redefinition and deskilling of the TBAs and 5) Cultural belief that intervention is necessary during childbirth aiding easy acceptance of medical interventions. Conclusion In resource poor settings where choices are</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_6");'>6</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li class="active"><span>8</span></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_8 --> <div id="page_9" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="161"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1911760L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1911760L"><span>Rock magnetic and anisotropy of magnetic susceptibility(AMS) of <span class="hlt">earthquake</span> affected soft sediments: Examples from Shillong and Latur (Deccan Trap), <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lakshmi, B. V., ,, Dr.; Gawali, Mr. Praveen B.; Deenadayalan, K., ,, Dr.; Ramesh, D. S., ,, Prof.</p> <p>2017-04-01</p> <p>Rock magnetic and anisotropy of magnetic susceptibility (AMS) of <span class="hlt">earthquake</span> affected soft sediments: Examples from Shillong and Latur (Deccan Trap), <span class="hlt">India</span>. B.V.Lakshmi, Praveen B.Gawali, K.Deenadayalan and D.S.Ramesh Indian Institute of Geomagnetism, plot 5, sector 18, Near Kalamboli Highway, New Panvel(W), Navi Mumbai 410218 Combined rock magnetism and anisotropy of magnetic susceptibility (AMS) studies on <span class="hlt">earthquake</span> induced soft and non-soft sediments from Shillong and Latur, <span class="hlt">India</span> have thrown up interesting results. The morphology of hysteresis loops, the pattern of isothermal remanent magnetization (IRM) acquisition, and temperature dependence of susceptibility indicate that titano-magnetite/magnetite is the main magnetic carrier in these sediments. We also analyzed the anisotropy of magnetic susceptibility (AMS) of liquefaction features within the seismically active Dauki fault, Shillong Plateau. We discovered that host sediments (non-liquefied), are characterized by an oblate AMS ellipsoid and liquefied sediment are characterized by a triaxial AMS ellipsoid, well grouped maximum susceptibility axis K1 (NNW-SSE trend). Field evidence and AMS analysis indicate that most of these features were emplaced by injection inferred to be due to seismically triggered fluidization. Anisotropy of magnetic susceptibility (AMS) of deformed and undeformed unconsolidated clay samples of Deccan Trap terrain from the 2000-year-old paleoearthquake site of Ther village, Maharashtra, <span class="hlt">India</span>, was also studied. Such deposits are rare in the compact basaltic terrain because of which the results acquired are very important. The undeformed clay samples exhibit typical sedimentary fabric with an oblate AMS ellipsoid, whereas the deformed samples are tightly grouped in the inferred compression direction, probably effected by an <span class="hlt">earthquake</span>, exhibiting prolate as well as oblate AMS ellipsoids. Rock magnetic and AMS methodology can help understand the behavior of different sediments to the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70180071','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70180071"><span>Structure of the Koyna-Warna Seismic Zone, Maharashtra, <span class="hlt">India</span>: A possible model for large induced <span class="hlt">earthquakes</span> elsewhere</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Catchings, Rufus D.; Dixit, M.M.; Goldman, Mark R.; Kumar, S.</p> <p>2015-01-01</p> <p>The Koyna-Warna area of <span class="hlt">India</span> is one of the best worldwide examples of reservoir-induced seismicity, with the distinction of having generated the largest known induced <span class="hlt">earthquake</span> (M6.3 on 10 December 1967) and persistent moderate-magnitude (>M5) events for nearly 50 years. Yet, the fault structure and tectonic setting that has accommodated the induced seismicity is poorly known, in part because the seismic events occur beneath a thick sequence of basalt layers. On the basis of the alignment of <span class="hlt">earthquake</span> epicenters over an ~50 year period, lateral variations in focal mechanisms, upper-crustal tomographic velocity images, geophysical data (aeromagnetic, gravity, and magnetotelluric), geomorphic data, and correlation with similar structures elsewhere, we suggest that the Koyna-Warna area lies within a right step between northwest trending, right-lateral faults. The sub-basalt basement may form a local structural depression (pull-apart basin) caused by extension within the step-over zone between the right-lateral faults. Our postulated model accounts for the observed pattern of normal faulting in a region that is dominated by north-south directed compression. The right-lateral faults extend well beyond the immediate Koyna-Warna area, possibly suggesting a more extensive zone of seismic hazards for the central <span class="hlt">India</span> area. Induced seismic events have been observed many places worldwide, but relatively large-magnitude induced events are less common because critically stressed, preexisting structures are a necessary component. We suggest that releasing bends and fault step-overs like those we postulate for the Koyna-Warna area may serve as an ideal tectonic environment for generating moderate- to large- magnitude induced (reservoir, injection, etc.) <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28460595','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28460595"><span>'You're disabled, why did you have sex in the first place?' An intersectional analysis of experiences of disabled women with regard to their sexual and reproductive health and rights in <span class="hlt">Gujarat</span> State, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dean, Laura; Tolhurst, Rachel; Khanna, Renu; Jehan, Kate</p> <p></p> <p>Globally, disabled people have significant unmet needs in relation to sexual and reproductive health (SRH). Disabled women in <span class="hlt">India</span> face multiple discrimination: social exclusion, lack of autonomy with regard to their SRH, vulnerability to violence, and lack of access to SRH care. While they may face shared challenges, an intersectional perspective suggests that considering disabled women as a uniform and 'vulnerable' group is likely to mask multiple differences in their lived experiences. To explore commonality and heterogeneity in the experiences of disabled women in relation to their SRH needs and rights in <span class="hlt">Gujarat</span> State, <span class="hlt">India</span>. We conducted 22 in-depth qualitative interviews with women between the ages of 18 and 49 with any form of self-identified disability. Intersectionality was used as a lens for analysis and in sampling. Findings explore the experiences of disabled women in a number of different spheres related to decision making and SRH service use. Recognising heterogeneity is critical to inform rights-based approaches to promote SRH and rights for all disabled women. This suggests a need to encourage strategic alliances between social movements for gender equity and SRH and disability rights, in which common interests and agendas can be pursued whilst recognising and respecting differences.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28038338','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28038338"><span>Analysis of copper tolerant rhizobacteria from the industrial belt of <span class="hlt">Gujarat</span>, western <span class="hlt">India</span> for plant growth promotion in metal polluted agriculture soils.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sharaff, Murali; Kamat, Shalmali; Archana, G</p> <p>2017-04-01</p> <p>Agricultural sites irrigated for long term with water polluted by industrial effluents containing heavy metals might adversely affect the soil microbial communities and crop yield. Hence it is important to study rhizobacterial communities and their metal tolerance in such affected agricultural fields to restore soil fertility and ecosystem. Present work deals with the study of rhizobacterial communities from plants grown in copper (Cu) contaminated agricultural fields along the industrial zone of <span class="hlt">Gujarat</span>, <span class="hlt">India</span> and are compared with communities from a Cu mine site. Microbial communities from rhizosphere soil samples varied in the magnitude of their Cu tolerance index indicating differences in long term pollution effects. Culture dependent denaturing gradient gel electrophoresis (CD-DGGE) of bacterial communities revealed the diverse composition at the sampling sites and a reduced total diversity due to Cu toxicity. Analysis of 16S rRNA gene diversity of Cu tolerant rhizobacteria revealed the predominance of Enterobacter spp. and Pseudomonas spp. under Cu stress conditions. Cu tolerant bacterial isolates that were able to promote growth of mung bean plants in vitro under Cu stress were obtained from these samples. Cu tolerant rhizobacterium P36 identified as Enterobacter sp. exhibited multiple plant growth promoting traits and significantly alleviated Cu toxicity to mung bean plants by reducing the accumulation of Cu in plant roots and promoted the plant growth in CuSO 4 amended soils. Copyright © 2016 Elsevier Inc. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JAESc.154...42B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JAESc.154...42B"><span>Seismic b-value anomalies prior to the 3rd January 2016, Mw = 6.7 Manipur <span class="hlt">earthquake</span> of northeast <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Borgohain, Jayanta Madhab; Borah, Kajaljyoti; Biswas, Rajib; Bora, Dipok K.</p> <p>2018-04-01</p> <p>Spatial variation of seismic b-value is estimated in the Indo-Myanmar subduction zone of northeast (NE) <span class="hlt">India</span> using the homogeneous part of <span class="hlt">earthquake</span> catalogue (1996-2015), recorded by International Seismological Center (ISC), consisting of 895 events of magnitude MW ≥ 3.9. The study region is divided into 1° × 1° square grids and b-values are estimated at each grid by maximum likelihood method. In this study, the b-value varies from 0.75 to 1.54 in the region. Significant variation of low b-value in the respective location may indicate high stress accumulation in that region. Spatial variation reveals intermediate b-value anomalies around the epicenter of the Mw = 6.7 Manipur <span class="hlt">earthquake</span> which occurred on 3rd January at 23:05 UTC (4 January 2016 at 04:35 IST). The variations of b-values are also estimated with respect to depth. The low b-value associated with the depth range ∼15-55 km, which may imply crustal homogeneity and high stress accumulation in the crust. Since, NE <span class="hlt">India</span> lies in the seismic zone V of the country; this study can be helpful to understand seismotectonics in the region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2567585','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2567585"><span>Reduction of catastrophic health care expenditures by a community-based health insurance scheme in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: current experiences and challenges.</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Ranson, Michael Kent</p> <p>2002-01-01</p> <p>OBJECTIVE: To assess the Self Employed Women's Association's Medical Insurance Fund in <span class="hlt">Gujarat</span> in terms of insurance coverage according to income groups, protection of claimants from costs of hospitalization, time between discharge and reimbursement, and frequency of use. METHODS: One thousand nine hundred and thirty claims submitted over six years were analysed. FINDINGS: Two hundred and fifteen (11%) of 1927 claims were rejected. The mean household income of claimants was significantly lower than that of the general population. The percentage of households below the poverty line was similar for claimants and the general population. One thousand seven hundred and twelve (1712) claims were reimbursed: 805 (47%) fully and 907 (53%) at a mean reimbursement rate of 55.6%. Reimbursement more than halved the percentage of catastrophic hospitalizations (>10% of annual household income) and hospitalizations resulting in impoverishment. The average time between discharge and reimbursement was four months. The frequency of submission of claims was low (18.0/1000 members per year: 22-37% of the estimated frequency of hospitalization). CONCLUSIONS: The findings have implications for community-based health insurance schemes in <span class="hlt">India</span> and elsewhere. Such schemes can protect poor households against the uncertain risk of medical expenses. They can be implemented in areas where institutional capacity is too weak to organize nationwide risk-pooling. Such schemes can cover poor people, including people and households below the poverty line. A trade off exists between maintaining the scheme's financial viability and protecting members against catastrophic expenditures. To facilitate reimbursement, administration, particularly processing of claims, should happen near claimants. Fine-tuning the design of a scheme is an ongoing process - a system of monitoring and evaluation is vital. PMID:12219151</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/12219151','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/12219151"><span>Reduction of catastrophic health care expenditures by a community-based health insurance scheme in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: current experiences and challenges.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ranson, Michael Kent</p> <p>2002-01-01</p> <p>To assess the Self Employed Women's Association's Medical Insurance Fund in <span class="hlt">Gujarat</span> in terms of insurance coverage according to income groups, protection of claimants from costs of hospitalization, time between discharge and reimbursement, and frequency of use. One thousand nine hundred and thirty claims submitted over six years were analysed. Two hundred and fifteen (11%) of 1927 claims were rejected. The mean household income of claimants was significantly lower than that of the general population. The percentage of households below the poverty line was similar for claimants and the general population. One thousand seven hundred and twelve (1712) claims were reimbursed: 805 (47%) fully and 907 (53%) at a mean reimbursement rate of 55.6%. Reimbursement more than halved the percentage of catastrophic hospitalizations (>10% of annual household income) and hospitalizations resulting in impoverishment. The average time between discharge and reimbursement was four months. The frequency of submission of claims was low (18.0/1000 members per year: 22-37% of the estimated frequency of hospitalization). The findings have implications for community-based health insurance schemes in <span class="hlt">India</span> and elsewhere. Such schemes can protect poor households against the uncertain risk of medical expenses. They can be implemented in areas where institutional capacity is too weak to organize nationwide risk-pooling. Such schemes can cover poor people, including people and households below the poverty line. A trade off exists between maintaining the scheme's financial viability and protecting members against catastrophic expenditures. To facilitate reimbursement, administration, particularly processing of claims, should happen near claimants. Fine-tuning the design of a scheme is an ongoing process - a system of monitoring and evaluation is vital.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EP%26S...68...40S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EP%26S...68...40S"><span>Fatality rates of the M w ~8.2, 1934, Bihar-Nepal <span class="hlt">earthquake</span> and comparison with the April 2015 Gorkha <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sapkota, Soma Nath; Bollinger, Laurent; Perrier, Frédéric</p> <p>2016-03-01</p> <p>Large Himalayan <span class="hlt">earthquakes</span> expose rapidly growing populations of millions of people to high levels of seismic hazards, in particular in northeast <span class="hlt">India</span> and Nepal. Calibrating vulnerability models specific to this region of the world is therefore crucial to the development of reliable mitigation measures. Here, we reevaluate the >15,700 casualties (8500 in Nepal and 7200 in <span class="hlt">India</span>) from the M w ~8.2, 1934, Bihar-Nepal <span class="hlt">earthquake</span> and calculate the fatality rates for this <span class="hlt">earthquake</span> using an estimation of the population derived from two census held in 1921 and 1942. Values reach 0.7-1 % in the epicentral region, located in eastern Nepal, and 2-5 % in the urban areas of the Kathmandu valley. Assuming a constant vulnerability, we obtain, if the same <span class="hlt">earthquake</span> would have repeated in 2011, fatalities of 33,000 in Nepal and 50,000 in <span class="hlt">India</span>. Fast-growing population in <span class="hlt">India</span> indeed must unavoidably lead to increased levels of casualty compared with Nepal, where the population growth is smaller. Aside from that probably robust fact, extrapolations have to be taken with great caution. Among other effects, building and life vulnerability could depend on population concentration and evolution of construction methods. Indeed, fatalities of the April 25, 2015, M w 7.8 Gorkha <span class="hlt">earthquake</span> indicated on average a reduction in building vulnerability in urban areas, while rural areas remained highly vulnerable. While effective scaling laws, function of the building stock, seem to describe these differences adequately, vulnerability in the case of an M w >8.2 <span class="hlt">earthquake</span> remains largely unknown. Further research should be carried out urgently so that better prevention strategies can be implemented and building codes reevaluated on, adequately combining detailed ancient and modern data.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27421254','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27421254"><span>Utilization of the state led public private partnership program "Chiranjeevi Yojana" to promote facility births in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: a cross sectional community based study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yasobant, Sandul; Vora, Kranti Suresh; Shewade, Hemant Deepak; Annerstedt, Kristi Sidney; Isaakidis, Petros; Mavalankar, Dileep V; Dholakia, Nishith B; De Costa, Ayesha</p> <p>2016-07-15</p> <p>"Chiranjeevi Yojana (CY)", a state-led large-scale demand-side financing scheme (DSF) under public-private partnership to increase institutional delivery, has been implemented across <span class="hlt">Gujarat</span> state, <span class="hlt">India</span> since 2005. The scheme aims to provide free institutional childbirth services in accredited private health facilities to women from socially disadvantaged groups (eligible women). These services are paid for by the state to the private facility with the intention of service being free to the user. This community-based study estimates CY uptake among eligible women and explores factors associated with non-utilization of the CY program. This was a community-based cross sectional survey of eligible women who gave birth between January and July 2013 in 142 selected villages of three districts in <span class="hlt">Gujarat</span>. A structured questionnaire was administered by trained research assistant to collect information on socio-demographic details, pregnancy details, details of childbirth and out-of-pocket (OOP) expenses incurred. A multivariable inferential analysis was done to explore the factors associated with non-utilization of the CY program. Out of 2,143 eligible women, 559 (26 %) gave birth under the CY program. A further 436(20 %) delivered at free public facilities, 713(33 %) at private facilities (OOP payment) and 435(20 %) at home. Eligible women who belonged to either scheduled tribe or poor [aOR = 3.1, 95 % CI:2.4 - 3.8] or having no formal education [aOR = 1.6, 95 % CI:1.1, 2.2] and who delivered by C-section [aOR = 2.1,95 % CI: 1.2, 3.8] had higher odds of not utilizing CY program. Of births at CY accredited facilities (n = 924), non-utilization was 40 % (n = 365) mostly because of lack of required official documentation that proved eligibility (72 % of eligible non-users). Women who utilized the CY program overall paid more than women who delivered in the free public facilities. Uptake of the CY among eligible women was low after almost a decade</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1994EOSTr..75..474.','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1994EOSTr..75..474."><span><span class="hlt">Earthquakes</span> and emergence</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p></p> <p></p> <p><span class="hlt">Earthquakes</span> and emerging infections may not have a direct cause and effect relationship like tax evasion and jail, but new evidence suggests that there may be a link between the two human health hazards. Various media accounts have cited a massive 1993 <span class="hlt">earthquake</span> in Maharashtra as a potential catalyst of the recent outbreak of plague in <span class="hlt">India</span> that has claimed more than 50 lives and alarmed the world. The hypothesis is that the <span class="hlt">earthquake</span> may have uprooted underground rat populations that carry the fleas infected with the bacterium that causes bubonic plague and can lead to the pneumonic form of the disease that is spread through the air.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/1393758-improving-building-energy-efficiency-india-state-level-analysis-building-energy-efficiency-policies','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/1393758-improving-building-energy-efficiency-india-state-level-analysis-building-energy-efficiency-policies"><span>Improving building energy efficiency in <span class="hlt">India</span>: State-level analysis of building energy efficiency policies</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Yu, Sha; Tan, Qing; Evans, Meredydd</p> <p></p> <p><span class="hlt">India</span> is expected to add 40 billion m2 of new buildings till 2050. Buildings are responsible for one third of India’s total energy consumption today and building energy use is expected to continue growing driven by rapid income and population growth. The implementation of the Energy Conservation Building Code (ECBC) is one of the measures to improve building energy efficiency. Using the Global Change Assessment Model, this study assesses growth in the buildings sector and impacts of building energy policies in <span class="hlt">Gujarat</span>, which would help the state adopt ECBC and expand building energy efficiency programs. Without building energy policies, buildingmore » energy use in <span class="hlt">Gujarat</span> would grow by 15 times in commercial buildings and 4 times in urban residential buildings between 2010 and 2050. ECBC improves energy efficiency in commercial buildings and could reduce building electricity use in <span class="hlt">Gujarat</span> by 20% in 2050, compared to the no policy scenario. Having energy codes for both commercial and residential buildings could result in additional 10% savings in electricity use. To achieve these intended savings, it is critical to build capacity and institution for robust code implementation.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27809807','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27809807"><span>Nosocomial infection of CCHF among health care workers in Rajasthan, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Yadav, Pragya D; Patil, Deepak Y; Shete, Anita M; Kokate, Prasad; Goyal, Pulkit; Jadhav, Santosh; Sinha, Sanjeev; Zawar, Divya; Sharma, Surendra K; Kapil, Arti; Sharma, D K; Upadhyay, Kamlesh J; Mourya, Devendra T</p> <p>2016-11-03</p> <p>Ever since Crimean-Congo hemorrhagic fever [CCHF] discovered in <span class="hlt">India</span>, several outbreaks of this disease have been recorded in <span class="hlt">Gujarat</span> State, <span class="hlt">India</span>. During the year 2011 to 2015 several districts of <span class="hlt">Gujarat</span> and Rajasthan state (Sirohi) found to be affected with CCHF including the positivity among ticks and livestock. During these years many infected individuals succumbed to this disease; which subsequently led to nosocomial infections. Herein, we report CCHF cases recorded from Rajasthan state during January 2015. This has affected four individuals apparently associated with one suspected CCHF case admitted in a private hospital in Jodhpur, Rajasthan. A 30-year-old male was hospitalized in a private hospital in Jodhpur, Rajasthan State, who subsequently had developed thrombocytopenia and showed hemorrhagic manifestations and died in the hospital. Later on, four nursing staff from the same hospital also developed the similar symptoms (Index case and Case A, B, C). Index case succumbed to the disease in the hospital at Jodhpur followed by the death of the case A that was shifted to AIIMS hospital, Delhi due to clinical deterioration. Blood samples of the index case and Case A, B, C were referred to the National institute of Virology, Pune, <span class="hlt">India</span> for CCHF diagnosis from the different hospitals in Rajasthan, Delhi and <span class="hlt">Gujarat</span>. However, a sample of deceased suspected CCHF case was not referred. Subsequently, blood samples of 5 nursing staff and 37 contacts (Case D was one of them) from Pokhran area, Jaisalmer district were referred to NIV, Pune. It clearly indicated that nursing staff acquired a nosocomial infection while attending the suspected CCHF case in an Intensive Care Unit of a private hospital in Jodhpur. However, one case was confirmed from the Pokhran area where the suspected CCHF case was residing. This case might have got the infection from suspected CCHF case or through other routes. CCHF strain associated with these nosocomial infections shares the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5645650','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5645650"><span>‘You’re disabled, why did you have sex in the first place?’ An intersectional analysis of experiences of disabled women with regard to their sexual and reproductive health and rights in <span class="hlt">Gujarat</span> State, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Dean, Laura; Tolhurst, Rachel; Khanna, Renu; Jehan, Kate</p> <p>2017-01-01</p> <p>ABSTRACT ​Background: Globally, disabled people have significant unmet needs in relation to sexual and reproductive health (SRH). Disabled women in <span class="hlt">India</span> face multiple discrimination: social exclusion, lack of autonomy with regard to their SRH, vulnerability to violence, and lack of access to SRH care. While they may face shared challenges, an intersectional perspective suggests that considering disabled women as a uniform and ‘vulnerable’ group is likely to mask multiple differences in their lived experiences. Objective: To explore commonality and heterogeneity in the experiences of disabled women in relation to their SRH needs and rights in <span class="hlt">Gujarat</span> State, <span class="hlt">India</span>. Methods: We conducted 22 in-depth qualitative interviews with women between the ages of 18 and 49 with any form of self-identified disability. Intersectionality was used as a lens for analysis and in sampling. Results: Findings explore the experiences of disabled women in a number of different spheres related to decision making and SRH service use. Conclusions: Recognising heterogeneity is critical to inform rights-based approaches to promote SRH and rights for all disabled women. This suggests a need to encourage strategic alliances between social movements for gender equity and SRH and disability rights, in which common interests and agendas can be pursued whilst recognising and respecting differences. PMID:28460595</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24479073','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24479073"><span>Third Angle of RSBY: Service Providers' Perspective to RSBY-operational Issues in <span class="hlt">Gujarat</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Trivedi, Mayur; Saxena, Deepak B</p> <p>2013-04-01</p> <p>Government of <span class="hlt">India</span> in 2008, launched its flagship health insurance scheme for the poor. The Rashtriya Swasthya Bima Yojana (RSBY) combines cutting edge technology with an unusual reliance on incentives to provide inpatient insurance coverage. The scheme allows for cashless hospitalization services at any of the empaneled hospitals. Stakeholders in RSBY include members of the community, Insurance Company and the service provider. The study manuscript is an attempt to get an insight to understand the bottle necks in faced by the service providers with an overall goal to understand issues in complete roll out of RSBY and its successful implementation across country. It was conducted to undertake the stakeholder analysis and understand the service providers' perspective to RSBY. The present study was conducted in the Patan district of <span class="hlt">Gujarat</span> state. Qualitative tool mainly in-depth interview of service providers of RSBY in Patan district of <span class="hlt">Gujarat</span> state was utilized for the data collection. Service providers opined an ineffective IEC around the utility of the RSBY service in the community. In spite of the claim that scheme relies heavily on technology to ensure paperless cashless services, on field, it was observed in the present study that the claim settlements are done through physical documents. The service providers had a perceived threat of being suspended from the list/de-empanelment of the provider by the insurance company. There is an urgent need for improved and effective IEC for the service and possibilities of an arrangement for to settle the case of grievances around suspensions ao that genuine hospitals can have fair deal as well. There definitely remains a greater and more serious role of government, which ranges from ownership to larger issue of governance.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=water+OR+aquatic+OR+freshwater+OR+groundwater&id=EJ1111938','ERIC'); return false;" href="https://eric.ed.gov/?q=water+OR+aquatic+OR+freshwater+OR+groundwater&id=EJ1111938"><span>Groundwater Scarcity Impact on Inclusiveness and Women Empowerment: Insights from School Absenteeism of Female Students in Two Watersheds in <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Kookana, Rai S.; Maheshwari, Basant; Dillon, Peter; Dave, Seema H.; Soni, Prahlad; Bohra, Hakimuddin; Dashora, Yogita; Purohit, Ramesh C.; Ward, John; Oza, Sachin; Katara, Pratibha; Yadav, Kamal K.; Varua, Maria E.; Grewal, Harsharn Singh; Packham, Roger; Jodha, Anand Singh; Patel, Ashishkumar</p> <p>2016-01-01</p> <p>A survey was conducted in eight secondary schools located in two watersheds in <span class="hlt">Gujarat</span> and Rajasthan (semi-arid region of <span class="hlt">India</span>) to assess students' perceptions about groundwater scarcity issues and the impact of the scarcity on their educational opportunities. Survey responses to a detailed questionnaire by a cohort of students in both…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017E%26ES...76a2002S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017E%26ES...76a2002S"><span>Geological and Rock Mechanics Perspectives for Underground Coal Gasification in <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Singh, Ajay K.; Singh, Rajendra</p> <p>2017-07-01</p> <p>The geological resources of coal in <span class="hlt">India</span> are more than 308 billion tonnes upto a depth of 1200 m, out of which proved reserve has been reported at around 130 billion tonnes. There is an increasing requirement to increase the energy extraction efficiency from coal as the developmental prospects of <span class="hlt">India</span> increase. Underground coal gasification (UCG) is a potential mechanism which may be utilized for extraction of deep-seated coal reserves. Some previous studies suggest that lignites from <span class="hlt">Gujarat</span> and Rajasthan, along with tertiary coals from northeastern <span class="hlt">India</span> can be useful from the point of view of UCG. We discuss some geological literature available for these areas. Coming to the rock mechanics perspectives, during UCG the rock temperature is considerable high. At this temperature, most empirical models of rock mechanics may not be applied. In this situation, the challenges for numerical modelling of UCG sites increases manifold. We discuss some of the important modelling geomechanical issues related to UCG in <span class="hlt">India</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4500497','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4500497"><span>Loss-To-Follow-Up on Multidrug Resistant Tuberculosis Treatment in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: The WHEN and WHO of It</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Shringarpure, Kalpita S.; Isaakidis, Petros; Sagili, Karuna D.; Baxi, R. K.</p> <p>2015-01-01</p> <p>Background Multidrug-resistant Tuberculosis (MDR-TB) is a rising global threat to public health and concerted efforts for its treatment are diluted if the outcomes are not successful, loss to follow up (LFU) being one of them. It is therefore necessary to know the proportion and the associated reasons for LFU and devise effective patient-centered strategies to improve retention in care. Methods A retrospective cohort study was conducted at the MDR-TB treatment site (DR-TB Site)in Central <span class="hlt">Gujarat</span> among all patients registered from February 2010 to June 2013.LFU patients were defined as those whose treatment was interrupted for two or more consecutive months for any reason. Descriptive statistics, survival analysis and multivariate modeling were used to determine the proportion of patients LFU and to assess associations between LFU and selected demographic and clinical factors. Results A total of 796 patients were enrolled during the study period; 71.9% were male and the median age was 35 years [Interquartile range (IQR) 27-45].The overall proportion of LFU patients was 153/796 (19.2%).The majority of LFU patients (133/153 i.e.87%) were lost within the first 6 months of treatment. Ambulatory treatment initiation (adjusted Hazards ratio aHR=2.63, CI:1.01-6.86), different providers in IP and CP ( aHR=1.27, CI:1.18-1.38)and culture conversion after more than 4 months of treatment(aHR=1.34, CI: 1.21-1.49)were found to be significantly associated with LFU in multivariate models. Conclusions A high proportion of LFU among patients on MDR-TB treatment was found in a programmatic setting in <span class="hlt">India</span>. Clinical but equally important programmatic factors were associated with LFU, accounting for one-fifth of all the outcomes of MDR-TB treatment. Proper training for DOT providers and aggressive counseling and health system strengthening with patient friendly follow up services may help reduce LFU. PMID:26167891</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JESS..127...55S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JESS..127...55S"><span>Comparison of <span class="hlt">earthquake</span> source characteristics in the Kachchh Rift Basin and Saurashtra horst, Deccan Volcanic Province, western <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sairam, B.; Singh, A. P.; Ravi Kumar, M.</p> <p>2018-06-01</p> <p>Seismic source parameters of small to moderate sized intraplate <span class="hlt">earthquakes</span> that occurred during 2002-2009 in the tectonic blocks of Kachchh Rift Basin (KRB) and the Saurashtra Horst (SH), in the stable continental region of western peninsular <span class="hlt">India</span>, are studied through spectral analysis of shear waves. The data of aftershock sequence of the 2001 Bhuj <span class="hlt">earthquake</span> (Mw 7.7) in the KRB and the 2007 Talala <span class="hlt">earthquake</span> (Mw 5.0) in the SH are used for this study. In the SH, the seismic moment (Mo), corner frequency (fc), stress drop (Δ σ ) and source radius ( r) vary from 7.8× 10^{11} to 4.0× 10^{16} N-m, 1.0-8.9 Hz, 4.8-10.2 MPa and 195-1480 m, respectively. While in the KRB, these parameters vary from Mo ˜ 1.24 × 10^{11} to 4.1 × 10^{16} N-m, f_{c }˜ 1.6 to 13.1 Hz, Δ σ ˜ 0.06 to 16.62 MPa and r ˜ 100 to 840 m. The kappa ( K) value in the KRB (0.025-0.03) is slightly larger than that in the SH region (0.02), probably due to thick sedimentary layers. The estimated stress drops of <span class="hlt">earthquakes</span> in the KRB are relatively higher than those in SH, due to large crustal stress concentration associated with mafic/ultramafic rocks at the hypocentral depths. The results also suggest that the stress drop value of intraplate <span class="hlt">earthquakes</span> is larger than the interplate <span class="hlt">earthquakes</span>. In addition, it is observed that the strike-slip events in the SH have lower stress drops, compared to the thrust and strike-slip events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JGRB..119.6372D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JGRB..119.6372D"><span>Seismicity, faulting, and structure of the Koyna-Warna seismic region, Western <span class="hlt">India</span> from local <span class="hlt">earthquake</span> tomography and hypocenter locations</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dixit, Madan M.; Kumar, Sanjay; Catchings, R. D.; Suman, K.; Sarkar, Dipankar; Sen, M. K.</p> <p>2014-08-01</p> <p>Although seismicity near Koyna Reservoir (<span class="hlt">India</span>) has persisted for ~50 years and includes the largest induced <span class="hlt">earthquake</span> (M 6.3) reported worldwide, the seismotectonic framework of the area is not well understood. We recorded ~1800 <span class="hlt">earthquakes</span> from 6 January 2010 to 28 May 2010 and located a subset of 343 of the highest-quality <span class="hlt">earthquakes</span> using the tomoDD code of Zhang and Thurber (2003) to better understand the framework. We also inverted first arrivals for 3-D Vp, Vs, and Vp/Vs and Poisson's ratio tomography models of the upper 12 km of the crust. Epicenters for the recorded <span class="hlt">earthquakes</span> are located south of the Koyna River, including a high-density cluster that coincides with a shallow depth (<1.5 km) zone of relatively high Vp and low Vs (also high Vp/Vs and Poisson's ratios) near Warna Reservoir. This anomalous zone, which extends near vertically to at least 8 km depth and laterally northward at least 15 km, is likely a water-saturated zone of faults under high pore pressures. Because many of the <span class="hlt">earthquakes</span> occur on the periphery of the fault zone, rather than near its center, the observed seismicity-velocity correlations are consistent with the concept that many of the <span class="hlt">earthquakes</span> nucleate in fractures adjacent to the main fault zone due to high pore pressure. We interpret our velocity images as showing a series of northwest trending faults locally near the central part of Warna Reservoir and a major northward trending fault zone north of Warna Reservoir.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009aogs...13..265A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009aogs...13..265A"><span><span class="hlt">Earthquake</span> Potential in Myanmar</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Aung, Hla Hla</p> <p></p> <p>Myanmar region is generally believed to be an area of high <span class="hlt">earthquake</span> potential from the point of view of seismic activity which has been low compared to the surrounding regions like Indonesia, China, and Pakistan. Geoscientists and seismologists predicted <span class="hlt">earthquakes</span> to occur in the area north of the Sumatra-Andaman Islands, i.e. the southwest and west part of Myanmar. Myanmar tectonic setting relative to East and SE Asia is rather peculiar and unique with different plate tectonic models but similar to the setting of western part of North America. Myanmar crustal blocks are caught within two lithospheric plates of <span class="hlt">India</span> and Indochina experiencing oblique subduction with major dextral strike-slip faulting of the Sagaing fault. Seismic tomography and thermal structure of <span class="hlt">India</span> plate along the Sunda subduction zone vary from south to north. Strong partitioning in central Andaman basin where crustal fragmentation and northward dispersion of Burma plate by back-arc spreading mechanism has been operating since Neogene. Northward motion of Burma plate relative to SE Asia would dock against the major continent further north and might have caused the accumulation of strain which in turn will be released as <span class="hlt">earthquakes</span> in the future.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_7");'>7</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li class="active"><span>9</span></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_9 --> <div id="page_10" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="181"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AdSpR..61.1952S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AdSpR..61.1952S"><span>Ionospheric perturbations due to <span class="hlt">earthquakes</span> as determined from VLF and GPS-TEC data analysis at Agra, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Singh, Dhananjali; Singh, Birbal; Pundhir, Devbrat</p> <p>2018-04-01</p> <p>Employing SoftPAL receiver, amplitude variations of VLF transmitter signals NWC (19.8 kHz) and NPM (21.4 kHz) are analyzed at Agra station in <span class="hlt">India</span> (Geograph. lat. 27.2°N, long. 78°E) ±15 days from five major <span class="hlt">earthquakes</span> of magnitude M = 6.9-8.5 occurred in Indian subcontinent during the years 2011-2013. We apply nighttime fluctuation (NF) method and show that in almost all cases the trend decreases and dispersion and NF increase on the same days corresponding to each <span class="hlt">earthquake</span> about 11-15 days prior to the main shock. Assuming that the ionospheric perturbations are caused by atmospheric gravity waves (AGW), we also calculate AGW modulation index for each case and find its values increased on the days amplitude fluctuations take place. Its value is decreased in one case only where the perturbations may be attributed to penetration of seismogenic electric field. In order to support the above results we also present GPS-TEC data analyzed by us corresponding to three of the above <span class="hlt">earthquakes</span>. We study the TEC anomalies (unusual enhancements) and find that in one case the precursory period is almost the same as that found in NF method.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70175906','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70175906"><span>Seismicity, faulting, and structure of the Koyna-Warna seismic region, Western <span class="hlt">India</span> from local <span class="hlt">earthquake</span> tomography and hypocenter locations</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Dixit, Madan M.; Kumar, Sanjay; Catchings, Rufus D.; Suman, K.; Sarkar, Dipankar; Sen, M.K.</p> <p>2014-01-01</p> <p>Although seismicity near Koyna Reservoir (<span class="hlt">India</span>) has persisted for ~50 years and includes the largest induced <span class="hlt">earthquake</span> (M 6.3) reported worldwide, the seismotectonic framework of the area is not well understood. We recorded ~1800 <span class="hlt">earthquakes</span> from 6 January 2010 to 28 May 2010 and located a subset of 343 of the highest-quality <span class="hlt">earthquakes</span> using the tomoDD code of Zhang and Thurber (2003) to better understand the framework. We also inverted first arrivals for 3-D Vp, Vs, and Vp/Vs and Poisson's ratio tomography models of the upper 12 km of the crust. Epicenters for the recorded <span class="hlt">earthquakes</span> are located south of the Koyna River, including a high-density cluster that coincides with a shallow depth (<1.5 km) zone of relatively high Vp and low Vs (also high Vp/Vs and Poisson's ratios) near Warna Reservoir. This anomalous zone, which extends near vertically to at least 8 km depth and laterally northward at least 15 km, is likely a water-saturated zone of faults under high pore pressures. Because many of the <span class="hlt">earthquakes</span> occur on the periphery of the fault zone, rather than near its center, the observed seismicity-velocity correlations are consistent with the concept that many of the <span class="hlt">earthquakes</span> nucleate in fractures adjacent to the main fault zone due to high pore pressure. We interpret our velocity images as showing a series of northwest trending faults locally near the central part of Warna Reservoir and a major northward trending fault zone north of Warna Reservoir.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-PIA03308.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-PIA03308.html"><span>SRTM Stereo Pair: Northwest of Bhuj, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2001-05-31</p> <p>On January 26, 2001, the Kachchh region in western <span class="hlt">India</span> suffered the most deadly <span class="hlt">earthquake</span> in <span class="hlt">India</span> history. Geologists traversed the region looking for ground surface disruptions, that could provide clues to the tectonic processes here.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.G11B0490K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.G11B0490K"><span>Active Fault Mapping of Naga-Disang Thrust (Belt of Schuppen) for Assessing Future <span class="hlt">Earthquake</span> Hazards in NE <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kumar, A.</p> <p>2014-12-01</p> <p>We observe the geodynamic appraisal of Naga-Disang Thrust North East <span class="hlt">India</span>. The Disang thrust extends NE-SW over a length of 480 km and it defines the eastern margin of Neogene basin. It branches out from Haflong-Naga thrust and in the NE at Bulbulia in the right bank of Noa Dihing River, it is terminated by Mishmi thrust, which extends into Myanmar as 'Sagaing fault,which dip generally towards SE. It extends between Dauki fault in the SW and Mishmi thrust in the NE. When the SW end of 'Belt of Schuppen' moved upwards and towards east along the Dauki fault, the NE end moved downwards and towards west along the Mishmi thrust, causing its 'S' shaped bending. The SRTM generated DEM is used to map the topographic expression of the schuppen belt, where these thrusts are significantly marked by topographic break. Satellite imagery map also shows presence lineaments supporting the post tectonic activities along Naga-Disang Thrusts. The southern part of 'Belt of Schuppen' extends along the sheared western limb of southerly plunging Kohima synform, a part of Indo Burma Ranges (IBR) and it is seismically active.The crustal velocity at SE of Schuppen is 39.90 mm/yr with a azimuth of 70.780 at Lumami, 38.84 mm/yr (Azimuth 54.09) at Senapati and 36.85 mm/yr (Azimuth 54.09) at Imphal. The crustal velocity at NW of Schuppen belt is 52.67 mm/yr (Azimuth 57.66) near Dhauki Fault in Meghalaya. It becomes 43.60 mm/yr (Azimuth76.50) - 44.25 (Azimuth 73.27) at Tiding and Kamlang Nagar around Mishmi thrust. The presence of Schuppen is marked by a change in high crustal velocity from Indian plate to low crustal velocity in Mishmi Suture as well as Indo Burma Ranges. The difference in crustal velocities results in building up of strain along the Schuppen which may trigger a large <span class="hlt">earthquake</span> in the NE <span class="hlt">India</span> in future. The belt of schuppean seems to be seismically active, however, the enough number of large <span class="hlt">earthquakes</span> are not recorded. These observations are significant on Naga</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.T41B2887A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.T41B2887A"><span>The Northern Rupture of the 1762 Arakan Meghathrust <span class="hlt">Earthquake</span> and other Potential <span class="hlt">Earthquake</span> Sources in Bangladesh.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Akhter, S. H.; Seeber, L.; Steckler, M. S.</p> <p>2015-12-01</p> <p>Bangladesh is one of the most densely populated countries in the world. It occupies a major part of the Bengal Basin, which contains the Ganges-Brahmaputra Delta (GBD), the largest and one of the most active of world deltas, and is located along the Alpine-Himalayan seismic belt. As such it is vulnerable to many natural hazards, especially <span class="hlt">earthquakes</span>. The country sits at the junction of three tectonic plates - Indian, Eurasian, and the Burma 'sliver' of the Sunda plate. These form two boundaries where plates converge- the <span class="hlt">India</span>-Eurasia plate boundary to the north forming the Himalaya Arc and the <span class="hlt">India</span>-Burma plate boundary to the east forming the Indo-Burma Arc. The <span class="hlt">India</span>-Burma plate boundary is exceptionally wide because collision with the GBD feeds an exception amount of sediment into the subduction zone. Thus the Himalayan continent collision orogeny along with its syntaxes to the N and NE of Bangladesh and the Burma Arc subduction boundary surround Bangladesh on two sides with active faults of regional scale, raising the potential for high-magnitude <span class="hlt">earthquakes</span>. In recent years Bangladesh has experienced minor to moderate <span class="hlt">earthquakes</span>. Historical records show that major and great <span class="hlt">earthquakes</span> have ravaged the country and the neighboring region several times over the last 450 years. Field observations of Tertiary structures along the Chittagong-Teknaf coast reveal that the rupture of 1762 Arakan megathrust <span class="hlt">earthquake</span> extended as far north as the Sitakund anticline to the north of the city of Chittagong. This <span class="hlt">earthquake</span> brought changes to the landscape, uplifting the Teknaf peninsula and St. Martin's Island by about 2-2.5 m, and activated two mud volcanos along the axis of the Sitakund anticline, where large tabular blocks of exotic crystalline limestone, were tectonically transported from a deep-seated formation along with the eruptive mud. Vast area of the coast including inland areas east of the lower Meghna River were inundated. More than 500 peoples died near</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T43B0680P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T43B0680P"><span>Seismotectonics of the trans-Himalaya, Eastern Ladakh, <span class="hlt">India</span>: constraints from Moment Tensor Solutions of local <span class="hlt">earthquake</span> data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Paul, A.</p> <p>2017-12-01</p> <p>The eastern Ladakh-Karakoram zone, the northwest part of the Trans-Himalayan belt, bears signature of this collisional process in the form of suture zones, exhumed blocks that underwent deeper subduction and also intra-continental fault zones. The seismotectonic scenario of northwest part of <span class="hlt">India</span>-Asia collision zone is studied by analyzing the local <span class="hlt">earthquake</span> data (M 1.4-4.3) recorded by a broadband seismological network consisting of 14 stations. Focal Mechanism Solution (FMS) of 13 selected <span class="hlt">earthquakes</span> were computed through waveform inversion of three-component broadband records. Depth distribution of the <span class="hlt">earthquakes</span> and FMS of local <span class="hlt">earthquakes</span> obtained through waveform inversion reveal the kinematics of the major fault zones present in Eastern Ladakh. The most pronounced cluster of seismicity is observed in the Karakoram Fault (KF) zone up to a depth of 65 km (Fig.1). The FMS reveals transpressive environment with the strike of inferred fault plane roughly parallel to the KF. It is inferred that the KF at least penetrates up to the lower crust and is a manifestation of active under thrusting of Indian lower crust beneath Tibet. Two clusters of micro seismicity is observed at a depth range of 5-20 km at north western and southeastern fringe of the Tso Morari gneiss dome which can be correlated to the activities along the Zildat fault and Karzok fault respectively. The FMSs estimated for representative <span class="hlt">earthquakes</span> show thrust fault solutions for the Karzok fault and normal fault solution for the Zildat fault. It is inferred that the Zildat fault is acting as detachment, facilitating the exhumation of the Tso Morari dome. On the other hand, the Tso Morari dome is underthrusting the Karzok ophiolite on its southern margin along the Karzok fault, due to gravity collapse.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26682047','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26682047"><span>Scaling-up public sector childhood diarrhea management program: Lessons from Indian states of <span class="hlt">Gujarat</span>, Uttar Pradesh and Bihar.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kumar, Sanjeev; Roy, Rajashree; Dutta, Sucharita</p> <p>2015-12-01</p> <p>Diarrhea remains a leading cause of death among children under five in <span class="hlt">India</span>. Public health sector is an important source for diarrhea treatment with oral rehydration salts (ORS) and zinc. In 2010, Micronutrient Initiative started a project to improve service delivery for childhood diarrhea management through public health sector in <span class="hlt">Gujarat</span>, Uttar Pradesh (UP) and Bihar. This paper aims to highlight feasible strategies, experiences and lessons learned from scaling-up zinc and ORS for childhood diarrhea management in the public sector in three Indian states. The project was implemented in six districts of <span class="hlt">Gujarat</span>, 12 districts of UP and 15 districts of Bihar, which includes 10.5 million children. Program strategies included capacity building of health care providers, expanding service delivery through community health workers (CHWs), providing supportive supervision to CHWs, ensuring supplies and conducting monitoring and evaluation. The lessons described in this paper are based on program data, government documents and studies that were used to generate evidence and inform program scale-up. 140 000 health personnel, including CHWs, were trained in childhood diarrhea management. During three years, CHWs had sustained knowledge and have treated and reported more than three million children aged 2-59 months having diarrhea, of which 84% were treated with both zinc and ORS. The successful strategies were scaled-up. It is feasible and viable to introduce and scale-up zinc and ORS for childhood diarrhea treatment through public sector. Community-based service delivery, timely and adequate supplies, trained staff and pro-active engagement with government were essential for program success.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26085020','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26085020"><span>Appropriate Management of Acute Diarrhea in Children Among Public and Private Providers in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: A Cross-Sectional Survey.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Walker, Christa L Fischer; Taneja, Sunita; LeFevre, Amnesty; Black, Robert E; Mazumder, Sarmila</p> <p>2015-05-07</p> <p>Diarrhea remains a leading cause of morbidity and mortality among children under 5 years of age in low- and middle-income countries. In 2006, the Indian government formally endorsed the World Health Organization guidelines that introduced zinc supplementation and low-osmolarity oral rehydration salts (ORS) for the treatment of diarrhea. Despite this, zinc is rarely prescribed and has not been available in the public sector in <span class="hlt">India</span> until very recently. The Diarrhea Alleviation Through Zinc and ORS Treatment (DAZT) project was implemented in <span class="hlt">Gujarat</span> between 2011 and 2013 to accelerate the uptake of zinc and ORS among public and private providers in 6 rural districts. As part of an external evaluation of DAZT, we interviewed 619 randomly selected facility- and community-based public and private providers 2-3 months after a 1-day training event had been completed (or, in the case of private providers, after at least 1 drug-detailing visit by a pharmaceutical representative had occurred) and supplies were in place. The purpose of the interviews was to assess providers' knowledge of appropriate treatment for diarrhea in children, reported treatment practices, and availability of drugs in stock. More than 80% of all providers interviewed reported they had received training or a drug-detailing visit on diarrheal treatment in the past 6 months. Most providers in all cadres (range, 68% to 100%) correctly described how to prepare ORS and nearly all (range, 90% to 100%) reported routinely prescribing it to treat diarrhea in children. Reported routine prescription of zinc was lower, ranging from 62% among private providers to 96% among auxiliary nurse-midwives. Among providers who reported ever not recommending zinc (n = 242), the 2 most frequently reported reasons for not doing so were not completely understanding zinc for diarrhea treatment and not having zinc in stock at the time of contact with the patient. In a multiple logistic regression analysis, recent training or</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=tectonic+AND+plates&pg=6&id=EJ409416','ERIC'); return false;" href="https://eric.ed.gov/?q=tectonic+AND+plates&pg=6&id=EJ409416"><span><span class="hlt">Earthquakes</span> in Stable Continental Crust.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Johnston, Arch C.; Kanter, Lisa R.</p> <p>1990-01-01</p> <p>Discussed are some of the reasons for <span class="hlt">earthquakes</span> which occur in stable crust away from familiar zones at the ends of tectonic plates. Crust stability and the reactivation of old faults are described using examples from <span class="hlt">India</span> and Australia. (CW)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26161686','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26161686"><span>Life-Stage and Mobility: An Exploratory GPS Study of Mobility in Multigenerational Families, Ahmedabad, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Isaacson, Michal; D'Ambrosio, Lisa; Samanta, Tannistha; Coughlin, Joseph</p> <p>2015-01-01</p> <p>As the population of older adults in <span class="hlt">India</span> grows, research is needed to plan a sustainable future for <span class="hlt">India</span>'s older adults. This article reports results from a Global Positioning System (GPS)-based pilot study that examined the mobility of middle-class, older adults living in Ahmedabad, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. Using mobility as a lens through which to examine the lives of older adults, we map potential research and identify policy areas of interest considering older adults in urban <span class="hlt">India</span>. The study explores the role of life stage in mobility as well as the effects of gender and urban environment on mobility. Using this distinctive perspective on day-to-day life, we propose themes through which, using policy and planning tools, the living environments of older adults in Indian cities can be improved. These policy measures include focusing on walkability and pedestrian safety in residential areas and building on existing mixed land use to create high accessibility to goods and services in urban environments.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27255714','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27255714"><span>Is the Annual Confidential Report system effective? A study of the government appraisal system in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Purohit, Bhaskar; Martineau, Tim</p> <p>2016-06-02</p> <p>Effective performance appraisal systems can not only motivate employees to improve performance but also be important for the performance of organizations. However, the appraisal systems in civil services called the Annual Confidential Report (ACR) systems can be ineffective and do not contribute to employees' learning and development. With this background, the current study aimed at understanding the ACR system and assessing its effectiveness. The research aims to contribute in filling the knowledge gap in the existing literature on the need as to why the ACR system in civil services is an important human resource management (HRM) function. The analysis is based on policy review to understand the extant appraisal-related rules and policies. Nineteen in-depth interviews with medical officers (MOs) working with the government health department of <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, were conducted. The main objective of the research was to assess the effectiveness of the actual appraisal system called or referred to as the ACR as perceived by MOs. Thematic framework approach was used to analyze qualitative data using NVIVO 9. Themes were built around five features of an effective appraisal system, i.e., purpose, source, feedback quality, link of the ACR system with other human resource functions, and administrative effectiveness. The five features of the effective appraisal system studied in the current research (purpose, source, feedback quality, link of ACR system with other HRM functions, and administrative effectiveness) indicate that the overall appraisal system is ineffective. The overall appraisal system was perceived to be subjective and one directional in character by the study respondents. Furthermore, respondents perceived the appraisal system to be a ritual and where MOs hardly got to know about their performance, especially good performance. Hence, the feedback loop, an important feature for an effective appraisal system, was absent. The overall ACR system functions in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26831933','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26831933"><span>Identification and molecular characterization of a new recombinant begomovirus and associated betasatellite DNA infecting Capsicum annuum in <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bhatt, Bhavin S; Chahwala, Fenisha D; Rathod, Sangeeta; Singh, Achuit K</p> <p>2016-05-01</p> <p>Capsicum annuum (Chilli) is a perennial herbaceous plant that is cultivated as an annual crop throughout the world, including <span class="hlt">India</span>. Chilli leaf curl disease (ChiLCD) is a major biotic constraint, causing major losses in chilli production. During 2014, leaf samples of chilli plants displaying leaf curl disease were collected from the Ahmedabad district of <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. These samples were used to isolate, clone and sequence viral genomic DNA and an associated betasatellite DNA molecule. Sequence analysis showed 90.4 % nucleotide sequence identity to the previously reported chilli leaf curl virus-[<span class="hlt">India</span>:Guntur:2009] (ChiLCV-[IN:Gun:09]. As per ICTV nomenclature rules, ChiLCV-Ahm represents a new species of begomovirus, and we therefore propose the name chilli leaf curl Ahmedabad virus-[<span class="hlt">India</span>:Ahmedabad:2014] (ChiLCAV-[IN:Ahm:14]). The associated betasatellite DNA showed a maximum of 93.5 % nucleotide sequence identity to a previously reported tomato leaf curl Bangladesh betasatellite and may be named tomato leaf curl Bangladesh betasatellite-[<span class="hlt">India</span>:Ahmedabad:Chilli:2014].</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29247089','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29247089"><span>Study protocol for Smartphone Monitoring for Atrial fibrillation in Real-Time in <span class="hlt">India</span> (SMART-<span class="hlt">India</span>): a community-based screening and referral programme.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Soni, Apurv; Karna, Sunil; Patel, Harshil; Fahey, Nisha; Raithatha, Shyamsundar; Handorf, Anna; Bostrom, John; Bashar, Syed; Talati, Kandarp; Shah, Ravi; Goldberg, Robert J; Thanvi, Sunil; Phatak, Ajay Gajanan; Allison, Jeroan J; Chon, Ki; Nimbalkar, Somashekhar Marutirao; McManus, David D</p> <p>2017-12-14</p> <p>Atrial fibrillation (AF), the world's most common arrhythmia, often goes undetected and untreated in low-resource communities, including <span class="hlt">India</span>, where AF epidemiology is undefined. AF is an important risk factor for stroke, which plagues an estimated 1.6 million Indians annually. As such, early detection of AF and management of high-risk patients is critically important to decrease stroke burden in individuals with AF. This study aims to describe the epidemiology of AF in Anand District, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, characterise the clinical profile of individuals who are diagnosed with AF and determine the performance of two mobile technologies for community-based AF screening. This observational study builds on findings from a previous feasibility study and leverages two novel technologies as well as an existing community health programme to perform door-to-door AF screening for 2000 people from 60 villages of Anand District, <span class="hlt">Gujarat</span>, <span class="hlt">India</span> using local health workers. A single-lead ECG and a pulse-based application is used to screen each individual for AF three times over a period of 5 days. Participants with suspected arrhythmias are followed up by study cardiologist who makes final diagnoses. Participants diagnosed with AF are initiated on treatment based on current anticoagulation guidelines and clinical reasoning. Age-stratified and sex-stratified prevalence of AF in the Anand District will be calculated for sample and estimated for Anand distribution using survey design weights. Sociodemographic and clinical factors associated with AF will be evaluated using multivariable regression methods. Performance of each mobile technology in detecting AF will be evaluated using a 12-lead ECG interpretation as the gold standard. This protocol was approved separately by the Institutional Review Board of University of Massachusetts Medical School and the Human Research Ethics Committee at Charutar Arogya Mandal. The findings of this study will be disseminated through peer</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5736031','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5736031"><span>Study protocol for Smartphone Monitoring for Atrial fibrillation in Real-Time in <span class="hlt">India</span> (SMART-<span class="hlt">India</span>): a community-based screening and referral programme</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Karna, Sunil; Patel, Harshil; Fahey, Nisha; Raithatha, Shyamsundar; Handorf, Anna; Bostrom, John; Bashar, Syed; Talati, Kandarp; Shah, Ravi; Goldberg, Robert J; Thanvi, Sunil; Allison, Jeroan J; Chon, Ki; Nimbalkar, Somashekhar Marutirao; McManus, David D</p> <p>2017-01-01</p> <p>Introduction Atrial fibrillation (AF), the world’s most common arrhythmia, often goes undetected and untreated in low-resource communities, including <span class="hlt">India</span>, where AF epidemiology is undefined. AF is an important risk factor for stroke, which plagues an estimated 1.6 million Indians annually. As such, early detection of AF and management of high-risk patients is critically important to decrease stroke burden in individuals with AF. This study aims to describe the epidemiology of AF in Anand District, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, characterise the clinical profile of individuals who are diagnosed with AF and determine the performance of two mobile technologies for community-based AF screening. Methods This observational study builds on findings from a previous feasibility study and leverages two novel technologies as well as an existing community health programme to perform door-to-door AF screening for 2000 people from 60 villages of Anand District, <span class="hlt">Gujarat</span>, <span class="hlt">India</span> using local health workers. A single-lead ECG and a pulse-based application is used to screen each individual for AF three times over a period of 5 days. Participants with suspected arrhythmias are followed up by study cardiologist who makes final diagnoses. Participants diagnosed with AF are initiated on treatment based on current anticoagulation guidelines and clinical reasoning. Analytical plan Age-stratified and sex-stratified prevalence of AF in the Anand District will be calculated for sample and estimated for Anand distribution using survey design weights. Sociodemographic and clinical factors associated with AF will be evaluated using multivariable regression methods. Performance of each mobile technology in detecting AF will be evaluated using a 12-lead ECG interpretation as the gold standard. Ethics and dissemination This protocol was approved separately by the Institutional Review Board of University of Massachusetts Medical School and the Human Research Ethics Committee at Charutar Arogya Mandal. The</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26849442','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26849442"><span>Direct Observation of Treatment Provided by a Family Member as Compared to Non-Family Member among Children with New Tuberculosis: A Pragmatic, Non-Inferiority, Cluster-Randomized Trial in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dave, Paresh Vamanrao; Shah, Amar Niranjan; Nimavat, Pankaj B; Modi, Bhavesh B; Pujara, Kirit R; Patel, Pradip; Mehariya, Keshabhai; Rade, Kiran Vaman; Shekar, Soma; Sachdeva, Kuldeep S; Oeltmann, John E; Kumar, Ajay M V</p> <p>2016-01-01</p> <p>The World Health Organization recommends direct observation of treatment (DOT) to support patients with tuberculosis (TB) and to ensure treatment completion. As per national programme guidelines in <span class="hlt">India</span>, a DOT provider can be anyone who is acceptable and accessible to the patient and accountable to the health system, except a family member. This poses challenges among children with TB who may be more comfortable receiving medicines from their parents or family members than from unfamiliar DOT providers. We conducted a non-inferiority trial to assess the effect of family DOT on treatment success rates among children with newly diagnosed TB registered for treatment during June-September 2012. We randomly assigned all districts (n = 30) in <span class="hlt">Gujarat</span> to the intervention (n = 15) or usual-practice group (n = 15). Adult family members in the intervention districts were given the choice to become their child's DOT provider. DOT was provided by a non-family member in the usual-practice districts. Using routinely collected clinic-based TB treatment cards, we compared treatment success rates (cured and treatment completed) between the two groups and the non-inferiority limit was kept at 5%. Of 624 children with newly diagnosed TB, 359 (58%) were from intervention districts and 265 (42%) were from usual-practice districts. The two groups were similar with respect to baseline characteristics including age, sex, type of TB, and initial body weight. The treatment success rates were 344 (95.8%) and 247 (93.2%) (p = 0.11) among the intervention and usual-practice groups respectively. DOT provided by a family member is not inferior to DOT provided by a non-family member among new TB cases in children and can attain international targets for treatment success. Clinical Trials Registry-<span class="hlt">India</span>, National Institute of Medical Statistics (Indian Council of Medical Research) CTRI/2015/09/006229.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4743945','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4743945"><span>Direct Observation of Treatment Provided by a Family Member as Compared to Non-Family Member among Children with New Tuberculosis: A Pragmatic, Non-Inferiority, Cluster-Randomized Trial in <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Modi, Bhavesh B.; Pujara, Kirit R.; Patel, Pradip; Mehariya, Keshabhai; Rade, Kiran Vaman; Shekar, Soma; Sachdeva, Kuldeep S.; Oeltmann, John E.; Kumar, Ajay M. V.</p> <p>2016-01-01</p> <p>Background The World Health Organization recommends direct observation of treatment (DOT) to support patients with tuberculosis (TB) and to ensure treatment completion. As per national programme guidelines in <span class="hlt">India</span>, a DOT provider can be anyone who is acceptable and accessible to the patient and accountable to the health system, except a family member. This poses challenges among children with TB who may be more comfortable receiving medicines from their parents or family members than from unfamiliar DOT providers. We conducted a non-inferiority trial to assess the effect of family DOT on treatment success rates among children with newly diagnosed TB registered for treatment during June–September 2012. Methods We randomly assigned all districts (n = 30) in <span class="hlt">Gujarat</span> to the intervention (n = 15) or usual-practice group (n = 15). Adult family members in the intervention districts were given the choice to become their child’s DOT provider. DOT was provided by a non-family member in the usual-practice districts. Using routinely collected clinic-based TB treatment cards, we compared treatment success rates (cured and treatment completed) between the two groups and the non-inferiority limit was kept at 5%. Results Of 624 children with newly diagnosed TB, 359 (58%) were from intervention districts and 265 (42%) were from usual-practice districts. The two groups were similar with respect to baseline characteristics including age, sex, type of TB, and initial body weight. The treatment success rates were 344 (95.8%) and 247 (93.2%) (p = 0.11) among the intervention and usual-practice groups respectively. Conclusion DOT provided by a family member is not inferior to DOT provided by a non-family member among new TB cases in children and can attain international targets for treatment success. Trial Registration Clinical Trials Registry–<span class="hlt">India</span>, National Institute of Medical Statistics (Indian Council of Medical Research) CTRI/2015/09/006229 PMID:26849442</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-PIA02798.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-PIA02798.html"><span>SRTM Perspective View with Landsat Overlay: Bhuj, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2001-04-05</p> <p>This perspective view shows the city of Bhuj, <span class="hlt">India</span>, in the foreground gray area after an <span class="hlt">earthquake</span> in western <span class="hlt">India</span> on January 26, 2001. This image was generated from NASA Landsat satellite and data from Shuttle Radar Topography Mission SRTM.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3237257','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3237257"><span>Genetic counselling in tribals in <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Mohanty, Dipika; Das, Kishalaya</p> <p>2011-01-01</p> <p>Genetic counselling in tribals unlike general population residing in cities and near villages is a difficult task due of their lower literacy and poor socio-economic status. However, sustained effort is essential with a close interaction in the local language, certain misbeliefs need to be removed gradually taking into account their socio-cultural background. The present communication deals with our experience in counselling for haemoglobinopathies during Neonatal Screening Programme undertaken for sickle cell disease in Kalahandi district of Orissa and Community Screening Programmes in primitive tribes of <span class="hlt">India</span> in four States viz. Orissa, <span class="hlt">Gujarat</span>, Tamil Nadu and Maharashtra. Counselling during neonatal screening programme was very well accepted demonstrating the benefit to the small babies as regards the morbidity. Premarital marriage counselling was also accepted by them. The success rate as followed up for 5 years is almost 50 per cent, the limitation being long follow up. Genetic counselling in these areas has to be continuous to achieve success and therefore the need for setting up of permanent centres in the tribal areas in <span class="hlt">India</span>. PMID:22089621</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007GeoJI.168..818D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007GeoJI.168..818D"><span>Instantaneous deformation and kinematics of the <span class="hlt">India</span>-Australia Plate</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Delescluse, Matthias; Chamot-Rooke, Nicolas</p> <p>2007-02-01</p> <p>Active intraplate deformation of the <span class="hlt">India</span>-Australia Plate is now being captured by far-field global positioning system (GPS) measurements as well as measurements on a few islands located within the deforming zone itself. In this paper, we combine global and regional geodetic solutions with focal mechanisms of <span class="hlt">earthquakes</span> to derive the present-day strain field of the <span class="hlt">India</span>-Australia Plate. We first compile an updated catalogue of 131 Indian intraplate <span class="hlt">earthquakes</span> (M > 5) spanning the period between the two Asian mega <span class="hlt">earthquakes</span> of Assam 1897 and Sumatra 2004. Using Haines and Holt's numerical approach applied to a fully deformable <span class="hlt">India</span>-Australia Plate, we show that the use of GPS data only or <span class="hlt">earthquakes</span> data only has severe drawbacks, related, respectively, to the small number of stations and the incompleteness of the <span class="hlt">earthquakes</span> catalogue. The combined solution avoids underestimation of the strain inherent to the Kostrov summation of seismic moments and provides details that cannot be reached by pure GPS modelling. We further explore the role of heterogeneity of the <span class="hlt">India</span>-Australia Plate and find that the best model, in terms of geodetic vectors fit, relative distribution of strain, style and direction of principal strain from <span class="hlt">earthquakes</span>, is obtained using the surface heat-flow as a proxy for rheological weakness of the oceanic lithosphere. The present-day deformation is distributed around the Afanasy Nikitin Chain in the Central Indian Basin (CIB)-where it is almost pure shortening-and within the Wharton Basin (WB) off Sumatra-where it is almost pure lateral strike-slip. The northern portion of NinetyEast ridge (NyR) appears as a major discontinuity for both strain and velocity. The new velocity field gives an <span class="hlt">India</span>/Australia rotation pole located at 11.3°S, 72.8°E (-0.301°Myr-1) overlapping with previous solutions, with continental <span class="hlt">India</span> moving eastward at rates ranging from 13 mm yr-1 (southern <span class="hlt">India</span>) to 26 mm yr-1 (northern <span class="hlt">India</span>) with respect to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-PIA03304.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-PIA03304.html"><span>SRTM Perspective View with Landsat Overlay: Rann of Kachchh, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2001-04-26</p> <p>The <span class="hlt">earthquake</span> that struck western <span class="hlt">India</span> on January 26, 2001, was the country strongest in the past 50 years. This perspective view shows the area of the <span class="hlt">earthquake</span> epicenter in the lower left corner.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_10 --> <div id="page_11" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="201"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70025419','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70025419"><span>2001 Bhuj, <span class="hlt">India</span>, <span class="hlt">earthquake</span> engineering seismoscope recordings and Eastern North America ground-motion attenuation relations</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Cramer, C.H.; Kumar, A.</p> <p>2003-01-01</p> <p>Engineering seismoscope data collected at distances less than 300 km for the M 7.7 Bhuj, <span class="hlt">India</span>, mainshock are compatible with ground-motion attenuation in eastern North America (ENA). The mainshock ground-motion data have been corrected to a common geological site condition using the factors of Joyner and Boore (2000) and a classification scheme of Quaternary or Tertiary sediments or rock. We then compare these data to ENA ground-motion attenuation relations. Despite uncertainties in recording method, geological site corrections, common tectonic setting, and the amount of regional seismic attenuation, the corrected Bhuj dataset agrees with the collective predictions by ENA ground-motion attenuation relations within a factor of 2. This level of agreement is within the dataset uncertainties and the normal variance for recorded <span class="hlt">earthquake</span> ground motions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1994PApGe.142..319C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1994PApGe.142..319C"><span>Excitation of T waves in the Indian Ocean between Srilanka and southern <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chadha, R. K.</p> <p>1994-06-01</p> <p>T phases of three <span class="hlt">earthquakes</span> from the Indian Ocean region, recorded by a short-period vertical-component seismic station network located in the vicinity of Kanyakumari on the southernmost tip of <span class="hlt">India</span>, are studied. Two of these <span class="hlt">earthquakes</span> are located west of 90°E ridge and one in the Nicobar Island region. However, seven other <span class="hlt">earthquakes</span> which occurred 150 200 km south of Kanyakumari in the ocean did not produce T phases. An analysis of T-waves (tertiary waves) travel time reveals the zone of P-wave to T-wave conversion (i.e., PT phase) region to coincide with the western continental slope of Srilanka. Further, it is observed that the disposition of the bathymetry between Srilanka and southern <span class="hlt">India</span> strongly favours the downslope propagation mechanism of T-wave travel to the southern coast of <span class="hlt">India</span> through SOFAR channel. These observations are reported for the first time from <span class="hlt">India</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JESS..123.1481P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JESS..123.1481P"><span>Satellite image based quantification of invasion and patch dynamics of mesquite ( Prosopis juliflora) in Great Rann of Kachchh, Kachchh Biosphere Reserve, <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pasha, S. Vazeed; Satish, K. V.; Reddy, C. Sudhakar; Prasada Rao, P. V. V.; Jha, C. S.</p> <p>2014-10-01</p> <p>The invasion of alien species is a significant threat to global biodiversity and the top driver of climate change. The present study was conducted in the Great Rann of Kachchh, part of Kachchh Biosphere Reserve, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, which has been severely affected by invasion of Prosopis juliflora. The invasive weed infestation has been identified using multi-temporal remote sensing datasets of 1977, 1990, 1999, 2005 and 2011. Spatial analyses of the transition matrix, extent of invasive colonies, patchiness, coalescence and rate of spread were carried out. During the study period of three and half decades, almost 295 km2 of the natural land cover was converted into Prosopis cover. This study has shown an increment of 42.9% of area under Prosopis cover in the Great Rann of Kachchh, part of the Kachchh Biosphere Reserve during 1977 to 2011. Spatial analysis indicates high occupancy of Prosopis cover with most of the invasion (95.9%) occurring in the grasslands and only 4.1% in other land cover types. The process of Prosopis invasion shows high patch initiation, followed by coalescence, indicating aggressive colonization of species. The number of patches within an area of < 1 km2 increased from 1977 to 2011, indicating the formation of new Prosopis habitats by replacing the grasslands. The largest patch of Prosopis cover increased from 144 km2 in 1977 to 430 km2 in 2011. The estimated mean patch size was 7.8 km2 in 1977. The mean patch size was largest during 2011, i.e., 9 km2. The annual spread rate for Prosopis has been estimated as 2.1% during 2005-2011. The present work has investigated the long term changes in Prosopis cover in the Great Rann of Kachchh, part of Kachchh Biosphere Reserve. The spatial database generated will be useful in preparing strategies for the management of Prosopis juliflora.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70155213','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70155213"><span>Why the New Madrid <span class="hlt">earthquakes</span> are M 7–8 and the Charleston <span class="hlt">earthquake</span> is ∼M 7</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Cramer, Chris H.; Boyd, Oliver</p> <p>2014-01-01</p> <p>Estimates of magnitudes of large historical <span class="hlt">earthquakes</span> are an essential input to and can seriously affect seismic‐hazard estimates. The earthquake‐intensity observations, modified Mercalli intensities (MMI), and assigned magnitudes Mof the 1811–1812 New Madrid events have been reinterpreted several times in the last decade and have been a source of controversy in making seismic‐hazard estimates in the central United States. Observations support the concept that the larger the <span class="hlt">earthquake</span>, the greater the maximum‐felt distance. For the same crustal attenuation and local soil conditions, magnitude should be the main influence on intensity values at large distances. We apply this concept by comparing the mean MMI at distances of 600–1200 km for each of the four largest New Madrid 1811–1812 <span class="hlt">earthquakes</span>, the 1886 Charleston, South Carolina, <span class="hlt">earthquake</span>, the 1929 M 7.2 Grand Banks <span class="hlt">earthquake</span>, and the 2001M 7.6 Bhuj, <span class="hlt">India</span>, <span class="hlt">earthquake</span>. We fit the intensity observations using the form MMI=A+C×dist−0.8×log(dist) to better define intensity attenuation in eastern North America (ENA). The intensity attenuation in cratonic <span class="hlt">India</span> differs from ENA and is corrected to ENA using both the above estimate and published intensity relations. We evaluate source, marine geophysical, Q, and stress‐drop information, as well as a 1929 Milne–Shaw record at Chicago to confirm that the 1929 Grand Banks <span class="hlt">earthquake</span> occurred in ENA crust. Our direct comparison of mean intensities beyond 600 km suggests M 7.5, 7.3, 7.7, and 6.9 for the three New Madrid 1811–1812 mainshocks and the largest aftershock and M 7.0 for the 1886 Charleston, South Carolina, <span class="hlt">earthquake</span>, with an estimated uncertainty of 0.3 units at the 95% confidence level (based on a Monte Carlo analysis). Our mean New Madrid and Charleston mainshock magnitudes are similar to those of Bakun and Hopper (2004) and are much higher than those of Hough and Page (2011) for New Madrid.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5656312','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5656312"><span>Discovery of the first ichthyosaur from the Jurassic of <span class="hlt">India</span>: Implications for Gondwanan palaeobiogeography</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Pandey, Dhirendra K.; Alberti, Matthias; Fürsich, Franz T.; Thakkar, Mahesh G.; Chauhan, Gaurav D.</p> <p>2017-01-01</p> <p>An articulated and partially preserved skeleton of an ichthyosaur was found in the Upper Jurassic (Upper Kimmeridgian) Katrol Formation exposed at a site south of the village Lodai in Kachchh district, <span class="hlt">Gujarat</span> (western <span class="hlt">India</span>). Here we present a detailed description and inferred taxonomic relationship of the specimen. The present study revealed that the articulated skeleton belongs to the family Ophthalmosauridae. The new discovery from <span class="hlt">India</span> further improves the depauperate fossil record of ichthyosaurs from the former Gondwanan continents. Based on the preserved length of the axial skeleton and anterior part of the snout and taking into account the missing parts of the skull and postflexural region, it is suggested that the specimen may represent an adult possibly reaching a length of 5.0–5.5 m. The widespread occurrence of ophthalmosaurids in the Upper Jurassic deposits of western Tethys, Madagascar, South America and <span class="hlt">India</span> points to possible faunal exchanges between the western Tethys and Gondwanan continents through a southern seaway. PMID:29069082</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S14A..02G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S14A..02G"><span>Artificial Water Reservoir Triggered <span class="hlt">Earthquakes</span> at Koyna, <span class="hlt">India</span>: Completion of the 3 km deep Pilot Borehole</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gupta, H. K.; Tiwari, V. M.; Satyanarayana, H.; Roy, S.; Arora, K.; Patro, P. K.; Shashidhar, D.; Mallika, K.; Akkiraju, V.; Misra, S.; Goswami, D.; Podugu, N.; Mishra, S.</p> <p>2017-12-01</p> <p>Koyna, near the west coast of <span class="hlt">India</span> is the most prominent site of artificial water reservoir triggered seismicity (RTS). Soon after the impoundment of the Koyna Dam in 1962, RTS was observed. It has continued till now. It includes the largest RTS <span class="hlt">earthquake</span> M 6.3 on December 10, 1967; 22 M≥5.0, and thousands of smaller <span class="hlt">earthquakes</span>. The entire <span class="hlt">earthquake</span> activity is limited to an area of about 30 km x 20 km, with most focal depths being within 6 km. There is no other <span class="hlt">earthquake</span> source within 50 km of the Koyna Dam. An ICDP Workshop held in March 2011 found Koyna to be the most suitable site to investigate reservoir- triggered seismicity (RTS) through deep drilling. Studies carried out in the preparatory phase since 2011 include airborne magnetic and gravity-gradient surveys, MT surveys, drilling of 9 boreholes going to depths of 1500 m and logging, heat flow measurements, seismological investigations including the deployment of six borehole seismometers, and LiDAR. The Second ICDP Workshop held during 16- 18 May 2014, reviewed the progress made and detailed planning of putting the borehole observatory was discussed. The site of a 3 km deep pilot borehole was debated and among the 5 possible location. Based on the seismic activity and logistics the location of the first Pilot Borehole has been finalized and the drilling started on the 21st December 2016. The 3000 m deep borehole was completed on 11th June 2017. The basement was touched at 1247 m depth and there were no sediments below basalt. Several zones with immense fluid losses were encountered. Geophysical Logging has been completed. Cores were recovered from 1269, 1892 and 2091 depths. The cores are 9 m long and with 4 inches diameter. The core recovery is almost 100%. In-situ stress measurements have been conducted at depths of 1600 m onwards.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4510747','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4510747"><span>Sickle cell disease in tribal populations in <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Colah, Roshan B.; Mukherjee, Malay B.; Martin, Snehal; Ghosh, Kanjaksha</p> <p>2015-01-01</p> <p>The sickle gene is widespread among many tribal population groups in <span class="hlt">India</span> with prevalence of heterozygotes varying from 1-40 per cent. Co-inheritance of the sickle gene with β-thalassaemia, HbD Punjab and glucose-6-phosphate dehydrogenase (G6PD) deficiency has also been reported. Most of the screening programmes in <span class="hlt">India</span> now use high performance liquid chromatography (HPLC) analysis although the solubility test is also sensitive and cheap. Sickle cell disease (SCD) among tribal populations is generally milder than among non-tribal groups with fewer episodes of painful crises, infections, acute chest syndrome and need for hospitalization. This has partly been attributed to the very high prevalence of α-thalassaemia among these tribes as well as higher foetal haemoglobin levels. However, the clinical presentation is variable with many cases having a severe presentation. There is not much information available on maternal and perinatal outcome in tribal women with sickle cell disease. Newborn screening programmes for SCD have recently been initiated in Maharashtra, <span class="hlt">Gujarat</span>, Odisha and Chattisgarh and monitoring these birth cohorts will help to understand the natural history of SCD in <span class="hlt">India</span>. Prenatal diagnosis is acceptable by tribal families in <span class="hlt">India</span>. The Indian Council of Medical Research and the National Rural Health Mission in different States are undertaking outreach programmes for better management and control of the disease. PMID:26139766</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-PIA03301.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-PIA03301.html"><span>SRTM Perspective View with Landsat Overlay: Bhuj and Anjar, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2001-04-12</p> <p>This perspective view shows the city of Bhuj, <span class="hlt">India</span>, in the foreground near the right side dark gray area. Bhuj and many other towns and cities nearby were almost completely destroyed by the January 26, 2001, <span class="hlt">earthquake</span> in western <span class="hlt">India</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AIPC.1857e0002B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AIPC.1857e0002B"><span><span class="hlt">Earthquake</span> vulnerability assessment of buildings of ward no. 8 of Haldwani-Kathgodam Municipal Corporation, Uttarakhand, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bora, Kritika; Pande, Ravindra K.</p> <p>2017-07-01</p> <p>"<span class="hlt">Earthquake</span> does not kill people; it is the building which kills people". <span class="hlt">Earthquake</span> is a sudden event below the surface of the earth which results in vertical and horizontal waves that causes destruction. The main aim of this research is to bring into light the unplanned and non-engineered construction practices growing in the Urban areas. Lack of space and continuous migration from hills has resulted in Multistorey construction. The present study is based on primary data collection through Rapid Visual Screening for the assessment of vulnerability of buildings. "Haldwani-Kathgodam being a new Municipal Corporation located in the foot hills of Himalayas is facing same problem. The seismic zonation brings this area into zone 4 of damage risk. Therefore an assessment to estimate the risk of the built up environment is important. This paper presents a systematic and useful way of assessing physical vulnerability of buildings. The present paper will show how the growing pressure on urban area tends to make the built up environment vulnerable towards seismic activities. The challenge today is to make our living environment safe for living. The day by day growing population pressure on urban area as a migration trend in developing countries is leading to high rise building, no planning and reckless construction. For the sake of saving some money people usually do not take the approval from structural engineer. This unplanned and haphazard construction proves non-resistant towards <span class="hlt">earthquake</span> and brings lives and properties to death and a stand still. The total no. of household in the current study area is 543 whereas the total population is 2497 (2011). The recent formation of Himalayas makes the area more sensitive towards seismic event. The closeness to the Main Boundary thrust brings it to zone 4 in the Seismic Zonation of <span class="hlt">India</span> i.e., High Damage Risk Zone</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25410701','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25410701"><span>Early Eocene fossils suggest that the mammalian order Perissodactyla originated in <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rose, Kenneth D; Holbrook, Luke T; Rana, Rajendra S; Kumar, Kishor; Jones, Katrina E; Ahrens, Heather E; Missiaen, Pieter; Sahni, Ashok; Smith, Thierry</p> <p>2014-11-20</p> <p>Cambaytheres (Cambaytherium, Nakusia and Kalitherium) are recently discovered early Eocene placental mammals from the Indo-Pakistan region. They have been assigned to either Perissodactyla (the clade including horses, tapirs and rhinos, which is a member of the superorder Laurasiatheria) or Anthracobunidae, an obscure family that has been variously considered artiodactyls or perissodactyls, but most recently placed at the base of Proboscidea or of Tethytheria (Proboscidea+Sirenia, superorder Afrotheria). Here we report new dental, cranial and postcranial fossils of Cambaytherium, from the Cambay Shale Formation, <span class="hlt">Gujarat</span>, <span class="hlt">India</span> (~54.5 Myr). These fossils demonstrate that cambaytheres occupy a pivotal position as the sister taxon of Perissodactyla, thereby providing insight on the phylogenetic and biogeographic origin of Perissodactyla. The presence of the sister group of perissodactyls in western <span class="hlt">India</span> near or before the time of collision suggests that Perissodactyla may have originated on the Indian Plate during its final drift toward Asia.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.U23C..06G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.U23C..06G"><span>Deep Scientific Drilling at Koyna, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gupta, H. K.</p> <p>2011-12-01</p> <p>The Stable Continental Region (SCR) <span class="hlt">earthquakes</span> tend to claim more human lives and inflict heavier financial losses as they occur where not expected and the local and regional preparedness to mitigate such catastrophes is minimal. Artificial water Reservoir Triggered Seismicity (RTS), most prominent in SCR, provides an exceptional window to comprehend genesis of such <span class="hlt">earthquakes</span>. Since the first scientific reporting of the RTS at the Boulder Dam, USA during 1930s, over 100 cases of RTS have been reported globally. Damaging <span class="hlt">earthquakes</span> exceeding M 6 have occurred at Hsingfengkiang (China), Kariba (Zambia -Zimbabwe border), Kremasta (Greece) and Koyna (<span class="hlt">India</span>). It is debated that the 2008 M 7.8 Sichuan <span class="hlt">earthquake</span> in China, which claimed over 80,000 human lives was triggered by filling of a nearby reservoir. Located close to the west coast of <span class="hlt">India</span>, Koyna is a classical site of RTS, where triggered <span class="hlt">earthquakes</span> have been occurring since the impoundment in 1962, including the largest RTS <span class="hlt">earthquake</span> of M 6.3 on December 10, 1967 which claimed over 200 human lives and destroyed Koyna town. Over the past 49 years 22 <span class="hlt">earthquakes</span> of M ≥ 5 and several thousand smaller <span class="hlt">earthquakes</span> have occurred in a restricted area of 20 X 30 sq. km. with no other seismic activity within 50 km of the Koyna Dam. The latest M 5.1 <span class="hlt">earthquake</span> occurred on December 12, 2009. Although several studies have clearly established the association of continued RTS at Koyna with precipitation driven loading and unloading of the Koyna and Warna reservoirs, the trigger mechanism is little understood. Our knowledge about the physical properties of rocks and fluids in the fault zones and how they affect the build-up of stress for an extended period is limited by the lack of data from the near field region. A deep bore hole of up to 7 km depth at a scientifically and logistically suitable location is under an advance stage of planning. A detailed workshop and field visits involving some 50 scientists from 10</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28790459','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28790459"><span>Dengue burden in <span class="hlt">India</span>: recent trends and importance of climatic parameters.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mutheneni, Srinivasa Rao; Morse, Andrew P; Caminade, Cyril; Upadhyayula, Suryanaryana Murty</p> <p>2017-08-09</p> <p>For the past ten years, the number of dengue cases has gradually increased in <span class="hlt">India</span>. Dengue is driven by complex interactions among host, vector and virus that are influenced by climatic factors. In the present study, we focused on the extrinsic incubation period (EIP) and its variability in different climatic zones of <span class="hlt">India</span>. The EIP was calculated by using daily and monthly mean temperatures for the states of Punjab, Haryana, <span class="hlt">Gujarat</span>, Rajasthan and Kerala. Among the studied states, a faster/low EIP in Kerala (8-15 days at 30.8 and 23.4 °C) and a generally slower/high EIP in Punjab (5.6-96.5 days at 35 and 0 °C) were simulated with daily temperatures. EIPs were calculated for different seasons, and Kerala showed the lowest EIP during the monsoon period. In addition, a significant association between dengue cases and precipitation was also observed. The results suggest that temperature is important in virus development in different climatic regions and may be useful in understanding spatio-temporal variations in dengue risk. Climate-based disease forecasting models in <span class="hlt">India</span> should be refined and tailored for different climatic zones, instead of use of a standard model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29040336','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29040336"><span>Characteristics of private partners in Chiranjeevi Yojana, a public-private-partnership to promote institutional births in <span class="hlt">Gujarat</span>, <span class="hlt">India</span> - Lessons for universal health coverage.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Iyer, Veena; Sidney, Kristi; Mehta, Rajesh; Mavalankar, Dileep; De Costa, Ayesha</p> <p>2017-01-01</p> <p>The Chiranjeevi Yojana (CY) is a Public-Private-Partnership between the state and private obstetricians in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, since 2007. The state pays for institutional births of the most vulnerable households (below-poverty-line and tribal) in private hospitals. An innovative remuneration package has been designed to disincentivise unnecessary cesareans. This study examines characteristics of private facilities which participated in the program. We conducted a cross-sectional survey of all facilities which had conducted any births between June 2012 and April 2013 in three districts. We identified 111 private and 47 public facilities. Ninety of the 111 private facilities did caesarean sections in the last three months and were eligible to participate in the CY program. Of these, 40 (44%) participated in the CY program. We conducted descriptive and bivariate analyses followed by a Poisson regression model to estimate prevalence ratios of facility characteristics that predicted participation. We found that facilities participating in the CY program had a significantly higher likelihood of being general facilities (PR 1.9, 95% CI 1.3-2.9), or conducting lower proportion of cesarean births (PR 2.1, 95% CI 1.2-3.5) or having obstetricians new in private practice (PR 1.9, 95% CI 1.2-3.1) or being less expensive (PR 1.8, 95% CI 1.1-3.0). But none of these factors retained significance in a multi variable model. Private obstetricians who participate in the CY program tend to be new to private practice, provide general services, conduct fewer caesareans and are also less expensive. This is advantageous to the PPP and widens the target beneficiary groups that can be serviced by the PPP. The state should design remuneration packages with the aim of attracting relatively new obstetricians to set up practices in more remote areas. It is possible that the CY remuneration package design is effective in keeping caesarean rates in check, and needs to be studied further.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=PIA02797&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dearthquakes','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=PIA02797&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dearthquakes"><span>SRTM Anaglyph: Bhuj, <span class="hlt">India</span>, Two Weeks After <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2001-01-01</p> <p><p/> On January 26, 2001, the city of Bhuj suffered the most deadly <span class="hlt">earthquake</span> in <span class="hlt">India</span>'s history. About 20,000 were killed and more than one million homes were damaged or destroyed. Shortly after the quake, geologists conducted field investigations to inventory and analyze the natural effects of the event. Stereoscopic views, similar to this anaglyph, aided the geologists in locating landforms indicative of long-term (and possibly ongoing) deformation. Soon, elevation data from the Shuttle Radar Topography Mission (SRTM) will be used in the study of a wide variety of natural hazards worldwide.<p/>In this image, the city of Bhuj appears as a medium gray area at the scene center, and the city airport is toward the north (top). Vegetation appears very dark. Rugged but low relief hills of previously folded and faulted bedrock appear south (bottom) and northwest (upper-left) of the city.<p/>The stereoscopic effect of this anaglyph was created by first draping a Landsat satellite image (taken just two weeks after the <span class="hlt">earthquake</span>) over preliminary digital elevation data from the SRTM and then generating two differing perspectives, one for each eye. When viewed through special glasses, the result is a vertically exaggerated view of the Earth's surface in its full three dimensions. Anaglyph glasses cover the left eye with a red filter and cover the right eye with a blue filter.<p/>Landsat has been providing visible and infrared views of the Earth since 1972. SRTM elevation data matches the 30-meter resolution of most Landsat images and will substantially help in analyses of the large and growing Landsat image archive. The Landsat7 Thematic Mapper image used here was provided to the SRTM project by the United States Geological Survey, Earth Resources Observation Systems (EROS) Data Center,Sioux Falls, South Dakota.<p/>Elevation data used in this image was acquired by the Shuttle Radar Topography Mission (SRTM) aboard the Space Shuttle Endeavour, launched on February 11, 2000</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.S31A2220A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.S31A2220A"><span><span class="hlt">Earthquake</span> Occurrence in Bangladesh and Surrounding Region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Al-Hussaini, T. M.; Al-Noman, M.</p> <p>2011-12-01</p> <p>The collision of the northward moving Indian plate with the Eurasian plate is the cause of frequent <span class="hlt">earthquakes</span> in the region comprising Bangladesh and neighbouring <span class="hlt">India</span>, Nepal and Myanmar. Historical records indicate that Bangladesh has been affected by five major <span class="hlt">earthquakes</span> of magnitude greater than 7.0 (Richter scale) during 1869 to 1930. This paper presents some statistical observations of <span class="hlt">earthquake</span> occurrence in fulfilment of a basic groundwork for seismic hazard assessment of this region. An up to date catalogue covering <span class="hlt">earthquake</span> information in the region bounded within 17°-30°N and 84°-97°E for the period of historical period to 2010 is derived from various reputed international sources including ISC, IRIS, Indian sources and available publications. Careful scrutiny is done to remove duplicate or uncertain <span class="hlt">earthquake</span> events. <span class="hlt">Earthquake</span> magnitudes in the range of 1.8 to 8.1 have been obtained and relationships between different magnitude scales have been studied. Aftershocks are removed from the catalogue using magnitude dependent space window and time window. The main shock data are then analyzed to obtain completeness period for different magnitudes evaluating their temporal homogeneity. Spatial and temporal distribution of <span class="hlt">earthquakes</span>, magnitude-depth histograms and other statistical analysis are performed to understand the distribution of seismic activity in this region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20060010263&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dearthquakes','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20060010263&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D40%26Ntt%3Dearthquakes"><span>Weather Satellite Thermal IR Responses Prior to <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>OConnor, Daniel P.</p> <p>2005-01-01</p> <p>A number of observers claim to have seen thermal anomalies prior to <span class="hlt">earthquakes</span>, but subsequent analysis by others has failed to produce similar findings. What exactly are these anomalies? Might they be useful for <span class="hlt">earthquake</span> prediction? It is the purpose of this study to determine if thermal anomalies can be found in association with known <span class="hlt">earthquakes</span> by systematically co-registering weather satellite images at the sub-pixel level and then determining if statistically significant responses occurred prior to the <span class="hlt">earthquake</span> event. A new set of automatic co-registration procedures was developed for this task to accommodate all properties particular to weather satellite observations taken at night, and it relies on the general condition that the ground cools after sunset. Using these procedures, we can produce a set of temperature-sensitive satellite images for each of five selected <span class="hlt">earthquakes</span> (Algeria 2003; Bhuj, <span class="hlt">India</span> 2001; Izmit, Turkey 2001; Kunlun Shan, Tibet 2001; Turkmenistan 2000) and thus more effectively investigate heating trends close to the epicenters a few hours prior to the <span class="hlt">earthquake</span> events. This study will lay tracks for further work in <span class="hlt">earthquake</span> prediction and provoke the question of the exact nature of the thermal anomalies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013JESS..122..289R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013JESS..122..289R"><span>Palynostratigraphy and depositional environment of Vastan Lignite Mine (Early Eocene), <span class="hlt">Gujarat</span>, western <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rao, M. R.; Sahni, Ashok; Rana, R. S.; Verma, Poonam</p> <p>2013-04-01</p> <p>Early Eocene sedimentary successions of south Asia, are marked by the development of extensive fossil-bearing, lignite-rich sediments prior to the collision of <span class="hlt">India</span> with Asia and provide data on contemporary equatorial faunal and vegetational assemblages. One such productive locality in western <span class="hlt">India</span> is the Vastan Lignite Mine representing approximately a 54-52 Ma sequence dated by the presence of benthic zone marker species, Nummulites burdigalensis burdigalensis. The present study on Vastan Lignite Mine succession is based on the spore-pollen and dinoflagellate cyst assemblages and documents contemporary vegetational changes. 86 genera and 105 species belonging to algal remains (including dinoflagellate cysts), fungal remains, pteridophytic spores and angiospermous pollen grains have been recorded. On the basis of first appearance, acme and decline of palynotaxa, three cenozones have been recognized and broadly reflect changing palaeodepositional environments. These are in ascending stratigraphic order (i) Proxapertites Spp. Cenozone, (ii) Operculodinium centrocarpum Cenozone and (iii) Spinizonocolpites Spp. Cenozone. The basal sequence is lagoonal, palm-dominated and overlain by more open marine conditions with dinoflagellate cysts and at the top, mangrove elements are dominant. The succession has also provided a unique record of fish, lizards, snakes, and mammals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.T11G..04G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.T11G..04G"><span>Lake deposits record evidence of large post-1505 AD <span class="hlt">earthquakes</span> in western Nepal</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ghazoui, Z.; Bertrand, S.; Vanneste, K.; Yokoyama, Y.; Van Der Beek, P.; Nomade, J.; Gajurel, A.</p> <p>2016-12-01</p> <p>According to historical records, the last large <span class="hlt">earthquake</span> that ruptured the Main Frontal Thrust (MFT) in western Nepal occurred in 1505 AD. Since then, no evidence of other large <span class="hlt">earthquakes</span> has been found in historical records or geological archives. In view of the catastrophic consequences to millions of inhabitants of Nepal and northern <span class="hlt">India</span>, intense efforts currently focus on improving our understanding of past <span class="hlt">earthquake</span> activity and complement the historical data on Himalayan <span class="hlt">earthquakes</span>. Here we report a new record, based on <span class="hlt">earthquake</span>-triggered turbidites in lakes. We use lake sediment records from Lake Rara, western Nepal, to reconstruct the occurrence of seismic events. The sediment cores were studied using a multi-proxy approach combining radiocarbon and 210Pb chronologies, physical properties (X-ray computerized axial tomography scan, Geotek multi-sensor core logger), high-resolution grain size, inorganic geochemistry (major elements by ITRAX XRF core scanning) and bulk organic geochemistry (C, N concentrations and stable isotopes). We identified several sequences of dense and layered fine sand mainly composed of mica, which we interpret as <span class="hlt">earthquake</span>-triggered turbidites. Our results suggest the presence of a synchronous event between the two lake sites correlated with the well-known 1505 AD <span class="hlt">earthquake</span>. In addition, our sediment records reveal five <span class="hlt">earthquake</span>-triggered turbidites younger than the 1505 AD event. By comparison with historical archives, we relate one of those to the 1833 AD MFT rupture. The others may reflect successive ruptures of the Western Nepal Fault System. Our study sheds light on events that have not been recorded in historical chronicles. Those five MMI>7 <span class="hlt">earthquakes</span> permit addressing the problem of missing slip on the MFT in western Nepal and reevaluating the risk of a large <span class="hlt">earthquake</span> affecting western Nepal and North <span class="hlt">India</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26332207','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26332207"><span>Options for Optimal Coverage of Free C-Section Services for Poor Mothers in Indian State of <span class="hlt">Gujarat</span>: Location Allocation Analysis Using GIS.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Vora, Kranti Suresh; Yasobant, Sandul; Sengupta, Raja; De Costa, Ayesha; Upadhyay, Ashish; Mavalankar, Dileep V</p> <p>2015-01-01</p> <p><span class="hlt">Gujarat</span>, a western state of <span class="hlt">India</span>, has seen a steep rise in the proportion of institutional deliveries over the last decade. However, there has been a limited access to cesarean section (C-Section) deliveries for complicated obstetric cases especially for poor rural women. C-section is a lifesaving intervention that can prevent both maternal and perinatal mortality. Poor women bear a disproportionate burden of maternal mortality, and lack of access to C-section, especially for these women, is an important contributor for high maternal and perinatal mortality in resource limited settings. To improve access for this underserved population in the context of inadequate public provision of emergency obstetric services, the state government of <span class="hlt">Gujarat</span> initiated a public private partnership program called "Chiranjeevi Yojana" (CY) in 2005 to increase the number of facilities providing free C-section services. This study aimed to analyze the current availability of these services in three districts of <span class="hlt">Gujarat</span> and to identify the best locations for additional service centres to optimize access to free C-section services using Geographic Information System technology. Supply and demand for obstetric care were calculated using secondary data from sources such as Census and primary data from cross-sectional facility survey. The study is unique in using primary data from facilities, which was collected in 2012-13. Information on obstetric beds and functionality of facilities to calculate supply was collected using pretested questionnaire by trained researchers after obtaining written consent from the participating facilities. Census data of population and birth rates for the study districts was used for demand calculations. Location-allocation model of ArcGIS 10 was used for analyses. Currently, about 50 to 84% of populations in all three study districts have access to free C-section facilities within a 20km radius. The model suggests that about 80-96% of the population can be</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015IJEaS.104.1511G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015IJEaS.104.1511G"><span>Investigations related to scientific deep drilling to study reservoir-triggered <span class="hlt">earthquakes</span> at Koyna, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gupta, Harsh; Purnachandra Rao, N.; Roy, Sukanta; Arora, Kusumita; Tiwari, V. M.; Patro, Prasanta K.; Satyanarayana, H. V. S.; Shashidhar, D.; Mallika, K.; Akkiraju, Vyasulu V.; Goswami, Deepjyoti; Vyas, Digant; Ravi, G.; Srinivas, K. N. S. S. S.; Srihari, M.; Mishra, S.; Dubey, C. P.; Raju, D. Ch. V.; Borah, Ujjal; Chinna Reddy, K.; Babu, Narendra; Rohilla, Sunil; Dhar, Upasana; Sen, Mrinal; Bhaskar Rao, Y. J.; Bansal, B. K.; Nayak, Shailesh</p> <p>2015-09-01</p> <p>Artificial water reservoir-triggered <span class="hlt">earthquakes</span> have continued at Koyna in the Deccan Traps province, <span class="hlt">India</span>, since the impoundment of the Shivaji Sagar reservoir in 1962. Existing models, to comprehend the genesis of triggered <span class="hlt">earthquakes</span>, suffer from lack of observations in the near field. To investigate further, scientific deep drilling and setting up a fault zone observatory at depth of 5-7 km is planned in the Koyna area. Prior to undertaking deep drilling, an exploratory phase of investigations has been launched to constrain subsurface geology, structure and heat flow regime in the area that provide critical inputs for the design of the deep borehole observatory. Two core boreholes drilled to depths of 1,522 and 1,196 m have penetrated the Deccan Traps and sampled the granitic basement in the region for the first time. Studies on cores provide new and direct information regarding the thickness of the Deccan Traps, the absence of infra-Trappean sediments and the nature of the underlying basement rocks. Temperatures estimated at a depth of 6 km in the area, made on the basis of heat flow and thermal properties data sets, do not exceed 150 °C. Low-elevation airborne gravity gradient and magnetic data sets covering 5,012 line km, together with high-quality magnetotelluric data at 100 stations, provide both regional information about the thickness of the Deccan Traps and the occurrence of localized density heterogeneities and anomalous conductive zones in the vicinity of the hypocentral zone. Acquisition of airborne LiDAR data to obtain a high-resolution topographic model of the region has been completed over an area of 1,064 km2 centred on the Koyna seismic zone. Seismometers have been deployed in the granitic basement inside two boreholes and are planned in another set of six boreholes to obtain accurate hypocentral locations and constrain the disposition of fault zones.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_11 --> <div id="page_12" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="221"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27287822','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27287822"><span>Counterfeit Avastin in <span class="hlt">India</span>: Punish the Criminals, Not the Patients.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Stewart, Michael W; Narayanan, Raja; Gupta, Vishali; Rosenfeld, Philip J; Martin, Daniel F; Chakravarthy, Usha</p> <p>2016-10-01</p> <p>To report the recent controversy surrounding the intraocular use of bevacizumab in <span class="hlt">India</span> and its relationship to the broader problems of off-label drug use, medication compounding, and drug counterfeiting. Perspective. Data for this perspective were obtained from several sources. Literature reviews for compounding-related endophthalmitis and drug counterfeiting were performed. Supplemental information was obtained through targeted Google searches for related published manuscripts. First-hand accounts of negotiations between representatives of the Vitreoretinal Society of <span class="hlt">India</span> (VRSI) and <span class="hlt">India</span>'s Central Drugs Standards Control Organization (CDSCO) were provided by 2 of the authors (R.N., V.G.). In December, 2015, 15 cases of intraocular inflammation following injections of counterfeit bevacizumab occurred in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. CDSCO reacted by prohibiting the use of intraocular bevacizumab throughout the country. Intense negotiations between the VRSI and CDSCO resulted in the permission to use bevacizumab in accordance with new safety guidelines. These include an enhanced informed consent process, the stamping of the Kezzler code on all bevacizumab vials, a real-time digital verification process between the end user and Roche Pharmaceuticals, and mandatory destruction of empty drug vials. Counterfeit bevacizumab has caused outbreaks of sterile and infectious postinjection endophthalmitis in at least 3 countries during the past 5 years and has entered the supply chain in other countries. Physicians and compounding pharmacists need to be aware that international counterfeiters have targeted bevacizumab. Copyright © 2016 Elsevier Inc. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFM.S11B2206S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFM.S11B2206S"><span>Focal mechanisms of <span class="hlt">earthquakes</span> in Mongolia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sodnomsambuu, D.; Natalia, R.; Gangaadorj, B.; Munkhuu, U.; Davaasuren, G.; Danzansan, E.; Yan, R.; Valentina, M.; Battsetseg, B.</p> <p>2011-12-01</p> <p>Focal mechanism data provide information on the relative magnitudes of the principal stresses, so that a tectonic regime can be assigned. Especially such information is useful for the study of intraplate seismic active regions. A study of <span class="hlt">earthquake</span> focal mechanisms in the territory of Mongolia as landlocked and intraplate region was conducted. We present map of focal mechanisms of <span class="hlt">earthquakes</span> with M4.5 which occurred in Mongolia and neighboring regions. Focal mechanisms solutions were constrained by the first motion solutions, as well as by waveform modeling, particularly CMT solutions. Four <span class="hlt">earthquakes</span> have been recorded in Mongolia in XX century with magnitude more than 8, the 1905 M7.9 Tsetserleg and M8.4 Bolnai <span class="hlt">earthquakes</span>, the 1931 M8.0 Fu Yun <span class="hlt">earthquake</span>, the 1957 M8.1 Gobi-Altai <span class="hlt">earthquake</span>. However the map of focal mechanisms of <span class="hlt">earthquakes</span> in Mongolia allows seeing all seismic active structures: Gobi Altay, Mongolian Altay, active fringe of Hangay dome, Hentii range etc. <span class="hlt">Earthquakes</span> in the most of Mongolian territory and neighboring China regions are characterized by strike-slip and reverse movements. Strike-slip movements also are typical for <span class="hlt">earthquakes</span> in Altay Range in Russia. The north of Mongolia and south part of the Baikal area is a region where have been occurred <span class="hlt">earthquakes</span> with different focal mechanisms. This region is a zone of the transition between compressive regime associated to <span class="hlt">India</span>-Eurasian collision and extensive structures localized in north of the country as Huvsgul area and Baykal rift. <span class="hlt">Earthquakes</span> in the Baikal basin itself are characterized by normal movements. <span class="hlt">Earthquakes</span> in Trans-Baikal zone and NW of Mongolia are characterized dominantly by strike-slip movements. Analysis of stress-axis orientations, the tectonic stress tensor is presented. The map of focal mechanisms of <span class="hlt">earthquakes</span> in Mongolia could be useful tool for researchers in their study on Geodynamics of Central Asia, particularly of Mongolian and Baikal regions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70026934','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70026934"><span>Postseismic deformation and stress changes following the 1819 Rann of Kachchh, <span class="hlt">India</span> <span class="hlt">earthquake</span>: Was the 2001 Bhuj <span class="hlt">earthquake</span> a triggered event?</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>To, A.; Burgmann, R.; Pollitz, F.</p> <p>2004-01-01</p> <p>The 2001 Mw 7.6 Bhuj <span class="hlt">earthquake</span> occurred in an intraplate region with rather unusual active seismicity, including an earlier major <span class="hlt">earthquake</span>, the 1819 Rann of Kachchh <span class="hlt">earthquake</span> (M7.7). We examine if static coseismic and transient postseismic deformation following the 1819 <span class="hlt">earthquake</span> contributed to the enhanced seismicity in the region and the occurrence of the 2001 Bhuj <span class="hlt">earthquake</span>, ???100 km away and almost two centuries later. Based on the Indian shield setting, great rupture depth of the 2001 event and lack of significant early postseismic deformation measured following the 2001 event, we infer that little viscous relaxation occurs in the lower crust and choose an upper mantle effective viscosity of 1019 Pas. The predicted Coulomb failure stress (DCFS) on the rupture plane of the 2001 event increased by more than 0.1 bar at 20 km depth, which is a small but possibly significant amount. Stress change from the 1819 event may have also affected the occurrence of other historic <span class="hlt">earthquakes</span> in this region. We also evaluate the postseismic deformation and ??CFS in this region due to the 2001 event. Positive ??CFS from the 2001 event occur to the NW and SE of the Bhuj <span class="hlt">earthquake</span> rupture. Copyright 2004 by the American Geophysical Union.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5583666','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5583666"><span>Dengue burden in <span class="hlt">India</span>: recent trends and importance of climatic parameters</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Mutheneni, Srinivasa Rao; Morse, Andrew P; Caminade, Cyril; Upadhyayula, Suryanaryana Murty</p> <p>2017-01-01</p> <p>For the past ten years, the number of dengue cases has gradually increased in <span class="hlt">India</span>. Dengue is driven by complex interactions among host, vector and virus that are influenced by climatic factors. In the present study, we focused on the extrinsic incubation period (EIP) and its variability in different climatic zones of <span class="hlt">India</span>. The EIP was calculated by using daily and monthly mean temperatures for the states of Punjab, Haryana, <span class="hlt">Gujarat</span>, Rajasthan and Kerala. Among the studied states, a faster/low EIP in Kerala (8–15 days at 30.8 and 23.4 °C) and a generally slower/high EIP in Punjab (5.6–96.5 days at 35 and 0 °C) were simulated with daily temperatures. EIPs were calculated for different seasons, and Kerala showed the lowest EIP during the monsoon period. In addition, a significant association between dengue cases and precipitation was also observed. The results suggest that temperature is important in virus development in different climatic regions and may be useful in understanding spatio-temporal variations in dengue risk. Climate-based disease forecasting models in <span class="hlt">India</span> should be refined and tailored for different climatic zones, instead of use of a standard model. PMID:28790459</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/423162-seismic-hazard-evaluation-oman-india-pipeline','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/423162-seismic-hazard-evaluation-oman-india-pipeline"><span>Seismic hazard evaluation of the Oman <span class="hlt">India</span> pipeline</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Campbell, K.W.; Thenhaus, P.C.; Mullee, J.E.</p> <p>1996-12-31</p> <p>The proposed Oman <span class="hlt">India</span> pipeline will traverse approximately 1,135 km of the northern Arabian Sea floor and adjacent continental shelves at depths of over 3 km on its route from Ra`s al Jifan, Oman, to Rapar Gadhwali, <span class="hlt">India</span>. The western part of the route crosses active faults that form the transform boundary between the Arabian and Indian tectonic plates. The eastern terminus of the route lies in the vicinity of the great (M {approximately} 8) 1829 Kutch, <span class="hlt">India</span> <span class="hlt">earthquake</span>. A probabilistic seismic hazard analysis was used to estimate the values of peak ground acceleration (PGA) with return periods of 200,more » 500 and 1,000 years at selected locations along the pipeline route and the submarine Indus Canyon -- a possible source of large turbidity flows. The results defined the ground-shaking hazard along the pipeline route and Indus Canyon for evaluation of risks to the pipeline from potential <span class="hlt">earthquake</span>-induced geologic hazards such as liquefaction, slope instability, and turbidity flows. 44 refs.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.S13E..02W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.S13E..02W"><span>Regional Seismic Amplitude Modeling and Tomography for <span class="hlt">Earthquake</span>-Explosion Discrimination</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Walter, W. R.; Pasyanos, M. E.; Matzel, E.; Gok, R.; Sweeney, J.; Ford, S. R.; Rodgers, A. J.</p> <p>2008-12-01</p> <p>Empirically explosions have been discriminated from natural <span class="hlt">earthquakes</span> using regional amplitude ratio techniques such as P/S in a variety of frequency bands. We demonstrate that such ratios discriminate nuclear tests from <span class="hlt">earthquakes</span> using closely located pairs of <span class="hlt">earthquakes</span> and explosions recorded on common, publicly available stations at test sites around the world (e.g. Nevada, Novaya Zemlya, Semipalatinsk, Lop Nor, <span class="hlt">India</span>, Pakistan, and North Korea). We are examining if there is any relationship between the observed P/S and the point source variability revealed by longer period full waveform modeling. For example, regional waveform modeling shows strong tectonic release from the May 1998 <span class="hlt">India</span> test, in contrast with very little tectonic release in the October 2006 North Korea test, but the P/S discrimination behavior appears similar in both events using the limited regional data available. While regional amplitude ratios such as P/S can separate events in close proximity, it is also empirically well known that path effects can greatly distort observed amplitudes and make <span class="hlt">earthquakes</span> appear very explosion-like. Previously we have shown that the MDAC (Magnitude Distance Amplitude Correction, Walter and Taylor, 2001) technique can account for simple 1-D attenuation and geometrical spreading corrections, as well as magnitude and site effects. However in some regions 1-D path corrections are a poor approximation and we need to develop 2-D path corrections. Here we demonstrate a new 2-D attenuation tomography technique using the MDAC <span class="hlt">earthquake</span> source model applied to a set of events and stations in both the Middle East and the Yellow Sea Korean Peninsula regions. We believe this new 2-D MDAC tomography has the potential to greatly improve <span class="hlt">earthquake</span>-explosion discrimination, particularly in tectonically complex regions such as the Middle East.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28959438','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28959438"><span>The effect of community health worker-led education on women's health and treatment-seeking: A cluster randomised trial and nested process evaluation in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Desai, Sapna; Mahal, Ajay; Sinha, Tara; Schellenberg, Joanna; Cousens, Simon</p> <p>2017-12-01</p> <p>A community-based health insurance scheme operated by the Self-Employed Women's Association in <span class="hlt">Gujarat</span>, <span class="hlt">India</span> reported that the leading reasons for inpatient hospitalisation claims by its members were diarrhoea, fever and hysterectomy - the latter at the average age of 37. This claims pattern raised concern regarding potentially unnecessary hospitalisation amongst low-income women. A cluster randomised trial and mixed methods process evaluation were designed to evaluate whether and how a community health worker-led education intervention amongst insured and uninsured adult women could reduce insurance claims, as well as hospitalisation and morbidity, related to diarrhoea, fever and hysterectomy. The 18-month intervention consisted of health workers providing preventive care information to women in a group setting in 14 randomly selected clusters, while health workers continued with regular activities in 14 comparison clusters. Claims data were collected from an administrative database, and four household surveys were conducted amongst a cohort of 1934 randomly selected adult women. 30% of insured women and 18% of uninsured women reported attending sessions. There was no evidence of an intervention effect on the primary outcome, insurance claims (risk ratio (RR) = 1.03; 95% confidence interval (CI) 0.81, 1.30) or secondary outcomes amongst insured and uninsured women, hospitalisation (RR = 1.05; 95% CI 0.58, 1.90) and morbidity (RR = 1.09; 95% CI 0.87, 1.38) related to the three conditions. The process evaluation suggested that participants retained knowledge from the sessions, but barriers to behaviour change were not overcome. We detected no evidence of an effect of this health worker-led intervention to decrease claims, hospitalisation and morbidity related to diarrhoea, fever and hysterectomy. Strategies that capitalise on health workers' role in the community and knowledge, as well as those that address the social determinants of diarrhoea, fever</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28830500','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28830500"><span>Trade in medicines and the public's health: a time series analysis of import disruptions during the 2015 <span class="hlt">India</span>-Nepal border blockade.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sharma, Abhishek; Mishra, Shiva Raj; Kaplan, Warren A</p> <p>2017-08-22</p> <p>Nepal was struck by devastating <span class="hlt">earthquakes</span> in April-May 2015, followed by the <span class="hlt">India</span>-Nepal border blockade later that year. We used the United Nations Commodity Trade Statistics (UN Comtrade) database to analyse exports of various health commodities from <span class="hlt">India</span> to Nepal from January 2011-September 2016. We used time-series regressions of trading volume vs. unit price to ask how well Nepal's trading history with <span class="hlt">India</span> prior to the <span class="hlt">earthquake</span> and blockade was able to predict unit prices of health commodities imported into Nepal during and after the <span class="hlt">earthquake</span> and the blockade. Regression residuals were used to quantify the extent to which the blockade impacted the price of healthcare commodities crossing into Nepal. During the blockade period (September 2015-early February 2016), the volume of all retail medicines traded across the <span class="hlt">India</span>-Nepal border was reduced by 46.5% compared to same months in 2014-2015. For medical dressings, large volumes were exported from <span class="hlt">India</span> to Nepal during and shortly after the <span class="hlt">earthquakes</span> (May-June 2015), but decreased soon thereafter. During the <span class="hlt">earthquake</span>, the difference between observed and predicted values of unit price (residuals) for all commodities show no statistical outliers. However, during the border blockade, Nepal paid USD 22.3 million more for retail medicines than one would have predicted based on its prior trading history with <span class="hlt">India</span>, enough to provide healthcare to nearly half of Kathmandu's citizens for 1 year. The <span class="hlt">India</span>-Nepal blockade was a geopolitical natural experiment demonstrating how a land-locked country is vulnerable to the vagaries of its primary trading partner. Although short-lived, the blockade had an immediate impact on traded medicine volumes and prices, and provided a large opportunity cost with implications for public health.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006AGUFM.T51D1553G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006AGUFM.T51D1553G"><span>Evidence for Tectonic Activity During the Mature Harappan Civilization, 2600-1800 BCE</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Grijalva, K. A.; Kovach, R. L.; Nur, A. M.</p> <p>2006-12-01</p> <p>The mature Harappan civilization located in Pakistan and <span class="hlt">India</span> dates from 2600 to 1800 BCE. By combining seismic data, three-dimensional elastic dislocation modeling, and archaeological findings we examined the role that <span class="hlt">earthquakes</span> played in the demise of Harappan settlements. The study focuses on three different geographical regions: <span class="hlt">Gujarat</span>, the Sarasvati-Ghaggar-Hakra River valley, and the Makran coast of Pakistan. In <span class="hlt">Gujarat</span>, the fluvial system of the Rann of Kachchh has undergone significant changes. The Rann of Kachchh formed as a delta for three rivers, becoming an inland sea during the time of Alexander the Great, and ultimately a salty marsh. These changes were brought about by a combination of sea level changes, the truncation of the three rivers by tectonic uplift and the deepening of the Rann by <span class="hlt">earthquake</span> induced subsidence. Events analogous to the 1819 Allah Bund <span class="hlt">earthquake</span>, which dammed the Puran River for seven years, would have significantly altered the water source for downstream settlements. Data from the recent 2001 Bhuj event shows that Harappan settlements would have suffered considerable shaking damage from an analogous historical event. Archaeological studies to date have found direct evidence for of at least one large <span class="hlt">earthquake</span> at Dholavira in 2200 BCE. A number of the mature Harappan settlements are located along the dry Sarasvati-Ghaggar-Hakra river system. The decline of these sites coincides with the divergence of the Sarasvati-Ghaggar-Hakra system to the Indus and Ganga river systems. A succession of <span class="hlt">earthquakes</span>, along with a period of aridity, likely led to the disappearance of the Sarasvati-Ghaggar-Hakra system. Although this region has not had any large <span class="hlt">earthquakes</span> in historic times, there is archaeological evidence of two large events at the Harappan site of Kalibangan, at 2900 and 2700 BCE. Along the Makran coast two settlements, believed to have been Harappan seaports, are now located tens of kilometers inland. Changes in sea</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017Tectp.714...21M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Tectp.714...21M"><span>Source modeling of the 2015 Mw 7.8 Nepal (Gorkha) <span class="hlt">earthquake</span> sequence: Implications for geodynamics and <span class="hlt">earthquake</span> hazards</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McNamara, D. E.; Yeck, W. L.; Barnhart, W. D.; Schulte-Pelkum, V.; Bergman, E.; Adhikari, L. B.; Dixit, A.; Hough, S. E.; Benz, H. M.; Earle, P. S.</p> <p>2017-09-01</p> <p>The Gorkha <span class="hlt">earthquake</span> on April 25th, 2015 was a long anticipated, low-angle thrust-faulting event on the shallow décollement between the <span class="hlt">India</span> and Eurasia plates. We present a detailed multiple-event hypocenter relocation analysis of the Mw 7.8 Gorkha Nepal <span class="hlt">earthquake</span> sequence, constrained by local seismic stations, and a geodetic rupture model based on InSAR and GPS data. We integrate these observations to place the Gorkha <span class="hlt">earthquake</span> sequence into a seismotectonic context and evaluate potential <span class="hlt">earthquake</span> hazard. Major results from this study include (1) a comprehensive catalog of calibrated hypocenters for the Gorkha <span class="hlt">earthquake</span> sequence; (2) the Gorkha <span class="hlt">earthquake</span> ruptured a 150 × 60 km patch of the Main Himalayan Thrust (MHT), the décollement defining the plate boundary at depth, over an area surrounding but predominantly north of the capital city of Kathmandu (3) the distribution of aftershock seismicity surrounds the mainshock maximum slip patch; (4) aftershocks occur at or below the mainshock rupture plane with depths generally increasing to the north beneath the higher Himalaya, possibly outlining a 10-15 km thick subduction channel between the overriding Eurasian and subducting Indian plates; (5) the largest Mw 7.3 aftershock and the highest concentration of aftershocks occurred to the southeast the mainshock rupture, on a segment of the MHT décollement that was positively stressed towards failure; (6) the near surface portion of the MHT south of Kathmandu shows no aftershocks or slip during the mainshock. Results from this study characterize the details of the Gorkha <span class="hlt">earthquake</span> sequence and provide constraints on where <span class="hlt">earthquake</span> hazard remains high, and thus where future, damaging <span class="hlt">earthquakes</span> may occur in this densely populated region. Up-dip segments of the MHT should be considered to be high hazard for future damaging <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70175400','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70175400"><span>Source modeling of the 2015 Mw 7.8 Nepal (Gorkha) <span class="hlt">earthquake</span> sequence: Implications for geodynamics and <span class="hlt">earthquake</span> hazards</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>McNamara, Daniel E.; Yeck, William; Barnhart, William D.; Schulte-Pelkum, V.; Bergman, E.; Adhikari, L. B.; Dixit, Amod; Hough, S.E.; Benz, Harley M.; Earle, Paul</p> <p>2017-01-01</p> <p>The Gorkha <span class="hlt">earthquake</span> on April 25th, 2015 was a long anticipated, low-angle thrust-faulting event on the shallow décollement between the <span class="hlt">India</span> and Eurasia plates. We present a detailed multiple-event hypocenter relocation analysis of the Mw 7.8 Gorkha Nepal <span class="hlt">earthquake</span> sequence, constrained by local seismic stations, and a geodetic rupture model based on InSAR and GPS data. We integrate these observations to place the Gorkha <span class="hlt">earthquake</span> sequence into a seismotectonic context and evaluate potential <span class="hlt">earthquake</span> hazard.Major results from this study include (1) a comprehensive catalog of calibrated hypocenters for the Gorkha <span class="hlt">earthquake</span> sequence; (2) the Gorkha <span class="hlt">earthquake</span> ruptured a ~ 150 × 60 km patch of the Main Himalayan Thrust (MHT), the décollement defining the plate boundary at depth, over an area surrounding but predominantly north of the capital city of Kathmandu (3) the distribution of aftershock seismicity surrounds the mainshock maximum slip patch; (4) aftershocks occur at or below the mainshock rupture plane with depths generally increasing to the north beneath the higher Himalaya, possibly outlining a 10–15 km thick subduction channel between the overriding Eurasian and subducting Indian plates; (5) the largest Mw 7.3 aftershock and the highest concentration of aftershocks occurred to the southeast the mainshock rupture, on a segment of the MHT décollement that was positively stressed towards failure; (6) the near surface portion of the MHT south of Kathmandu shows no aftershocks or slip during the mainshock. Results from this study characterize the details of the Gorkha <span class="hlt">earthquake</span> sequence and provide constraints on where <span class="hlt">earthquake</span> hazard remains high, and thus where future, damaging <span class="hlt">earthquakes</span> may occur in this densely populated region. Up-dip segments of the MHT should be considered to be high hazard for future damaging <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16..798S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16..798S"><span>Geological indicators of a suspected seismic source from Peninsular <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Singh, Yogendra; John, Biju; P, Ganapathy G.; S, Divyalakshmi K.</p> <p>2014-05-01</p> <p>An increase in seismicity in Peninsular <span class="hlt">India</span> during the last few decades has initiated various studies for identifying seismogenic structures and their behaviour. Even though few <span class="hlt">earthquakes</span> occurred at well defined structures many of them occurred at unexpected locations where no previous seismicity reported. However, studies subsequent to the 1993 Latur <span class="hlt">earthquake</span> as well as the studies at different parts of peninsular <span class="hlt">India</span>, have led to the identification of pre-existing faults that have activated in the past. Studies elsewhere in the cratonic hinderland also show that the damaging <span class="hlt">earthquakes</span> occur on pre-existing faults with a recurrence period of tens of thousands of year Studies subsequent to 1989 Wadakkancheri <span class="hlt">earthquake</span> (M=4.3) identified Desamangalam fault which are capable of generating <span class="hlt">earthquakes</span>. However, it is noted that a number of later events are occurring much south of the Desamangalam fault. We identified a set of NW-SE trending lineaments which are influencing the drainage pattern of the area. A network of paleochannels is also observed in the remote sensing analysis and field studies in this area. Regionally these lineaments meeting one of the major lineaments in central Kerala called Periyar lineament, in the south. Charnockite rocks constitutes the major rock type of the region. These rocks at places developed strong foliation similar to the lineament direction. Detailed field studies identified oblique movement (reverse and strike slip component) along NW-SE trending faults which are dipping south-west. The studies also find NNE-SSW trending vertical faults showing strike-slip movement. The damage zones of each of these faults bears different mineral precipitations and gouge injections of episodic nature. The presence of loose gouge may indicate the faulting is a much later development in the brittle regime. The sense of movement of the observed faults may indicate that the various river/drainage abandonment observed in the area are due to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016ThApC.124..593M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016ThApC.124..593M"><span>Characterizing rainfall of hot arid region by using time-series modeling and sustainability approaches: a case study from <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Machiwal, Deepesh; Kumar, Sanjay; Dayal, Devi</p> <p>2016-05-01</p> <p>This study aimed at characterization of rainfall dynamics in a hot arid region of <span class="hlt">Gujarat</span>, <span class="hlt">India</span> by employing time-series modeling techniques and sustainability approach. Five characteristics, i.e., normality, stationarity, homogeneity, presence/absence of trend, and persistence of 34-year (1980-2013) period annual rainfall time series of ten stations were identified/detected by applying multiple parametric and non-parametric statistical tests. Furthermore, the study involves novelty of proposing sustainability concept for evaluating rainfall time series and demonstrated the concept, for the first time, by identifying the most sustainable rainfall series following reliability ( R y), resilience ( R e), and vulnerability ( V y) approach. Box-whisker plots, normal probability plots, and histograms indicated that the annual rainfall of Mandvi and Dayapar stations is relatively more positively skewed and non-normal compared with that of other stations, which is due to the presence of severe outlier and extreme. Results of Shapiro-Wilk test and Lilliefors test revealed that annual rainfall series of all stations significantly deviated from normal distribution. Two parametric t tests and the non-parametric Mann-Whitney test indicated significant non-stationarity in annual rainfall of Rapar station, where the rainfall was also found to be non-homogeneous based on the results of four parametric homogeneity tests. Four trend tests indicated significantly increasing rainfall trends at Rapar and Gandhidham stations. The autocorrelation analysis suggested the presence of persistence of statistically significant nature in rainfall series of Bhachau (3-year time lag), Mundra (1- and 9-year time lag), Nakhatrana (9-year time lag), and Rapar (3- and 4-year time lag). Results of sustainability approach indicated that annual rainfall of Mundra and Naliya stations ( R y = 0.50 and 0.44; R e = 0.47 and 0.47; V y = 0.49 and 0.46, respectively) are the most sustainable and dependable</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25108445','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25108445"><span>Towards seasonal forecasting of malaria in <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lauderdale, Jonathan M; Caminade, Cyril; Heath, Andrew E; Jones, Anne E; MacLeod, David A; Gouda, Krushna C; Murty, Upadhyayula Suryanarayana; Goswami, Prashant; Mutheneni, Srinivasa R; Morse, Andrew P</p> <p>2014-08-10</p> <p>Malaria presents public health challenge despite extensive intervention campaigns. A 30-year hindcast of the climatic suitability for malaria transmission in <span class="hlt">India</span> is presented, using meteorological variables from a state of the art seasonal forecast model to drive a process-based, dynamic disease model. The spatial distribution and seasonal cycles of temperature and precipitation from the forecast model are compared to three observationally-based meteorological datasets. These time series are then used to drive the disease model, producing a simulated forecast of malaria and three synthetic malaria time series that are qualitatively compared to contemporary and pre-intervention malaria estimates. The area under the Relative Operator Characteristic (ROC) curve is calculated as a quantitative metric of forecast skill, comparing the forecast to the meteorologically-driven synthetic malaria time series. The forecast shows probabilistic skill in predicting the spatial distribution of Plasmodium falciparum incidence when compared to the simulated meteorologically-driven malaria time series, particularly where modelled incidence shows high seasonal and interannual variability such as in Orissa, West Bengal, and Jharkhand (North-east <span class="hlt">India</span>), and <span class="hlt">Gujarat</span>, Rajastan, Madhya Pradesh and Maharashtra (North-west <span class="hlt">India</span>). Focusing on these two regions, the malaria forecast is able to distinguish between years of "high", "above average" and "low" malaria incidence in the peak malaria transmission seasons, with more than 70% sensitivity and a statistically significant area under the ROC curve. These results are encouraging given that the three month forecast lead time used is well in excess of the target for early warning systems adopted by the World Health Organization. This approach could form the basis of an operational system to identify the probability of regional malaria epidemics, allowing advanced and targeted allocation of resources for combatting malaria in <span class="hlt">India</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://medlineplus.gov/druginfo/natural/953.html','NIH-MEDLINEPLUS'); return false;" href="https://medlineplus.gov/druginfo/natural/953.html"><span>Ashwagandha</span></a></p> <p><a target="_blank" href="http://medlineplus.gov/">MedlinePlus</a></p> <p></p> <p></p> <p>... specific ashwagandha root extract (KSM66, Ixoreal Biomed, Hyderabad, <span class="hlt">India</span>) 300 mg twice daily after food for 60 ... Cap Strelaxin, M/s Pharmanza Herbal Pvt. Ltd., <span class="hlt">Gujarat</span>, <span class="hlt">India</span>) 400 mg three times daily for one month ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22312805','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22312805"><span>Physico-chemical characteristics of groundwater in and around Surat City (<span class="hlt">India</span>).</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Raval, Viral H; Malik, G M</p> <p>2010-10-01</p> <p>Groundwater samples were collected from different locations of Surat city, <span class="hlt">Gujarat</span> (<span class="hlt">India</span>). These samples from 32 locations of Surat city were analysed for their physico-chemical characteristics involving pH, colour, odour, hardness, chloride, alkalinity, COD, sulfate, TDS, SS, iron, Cu, boron, chromium, temperature and Langelier Saturation Index. On comparing the results against drinking water quality standards laid by Indian Council of Medical Research (ICMR) and World Health Organization (WHO), it is found that most of the water samples are non-potable. Most of the samples indicated Total Alkalinity, Hardness, Chloride and TDS values much higher than the permissible level stipulated by ICMR and WHO. Even at some places Langelier Saturation Index values found higher too. The high values of these parameters may have health implications and therefore these need attention.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017InJPh..91.1467P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017InJPh..91.1467P"><span>Anomalous behavior of the ionosphere before strong <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Peddi Naidu, P.; Madhavi Latha, T.; Madhusudhana Rao, D. N.; Indira Devi, M.</p> <p>2017-12-01</p> <p>In the recent years, the seismo-ionospheric coupling has been studied using various ionospheric parameters like Total Electron Content, Critical frequencies, Electron density and Phase and amplitude of Very Low Frequency waves. The present study deals with the behavior of the ionosphere in the pre-<span class="hlt">earthquake</span> period of 3-4 days at various stations adopting the critical frequencies of Es and F2 layers. The relative phase measurements of 16 kHz VLF wave transmissions from Rugby (UK), received at Visakhapatnam (<span class="hlt">India</span>) are utilized to study the D-region during the seismically active periods. The results show that, f0Es increases a few hours before the time of occurrence of the <span class="hlt">earthquake</span> and day time values f0F2 are found to be high during the sunlit hours in the pre-<span class="hlt">earthquake</span> period of 2-3 days. Anomalous VLF phase fluctuations are observed during the sunset hours before the <span class="hlt">earthquake</span> event. The results are discussed in the light of the probable mechanism proposed by previous investigators.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001AGUFM.S11D..02S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001AGUFM.S11D..02S"><span>Regional crustal structures along several paths in <span class="hlt">India</span> and its surrounding regions using local P- and S-wave travel times and regional waveforms recorded from the March 28, 1999 Chamoli <span class="hlt">earthquake</span> sequence</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Saikia, C. K.; Ichinose, G. A.; Kayal, J. R.; Bhattacharya, S. N.; Shukla, A. K.</p> <p>2001-12-01</p> <p>The March 28, 1999 Chamoli <span class="hlt">earthquake</span> (Mw 6.8) in northwest <span class="hlt">India</span> generated a large sequence of aftershocks (M_ w> 4.0) which were recorded by a temporary network ofshort-period stations deployed by various organizations, namely <span class="hlt">India</span> Meteorological Department (IMD), Geological Survey of <span class="hlt">India</span> (GSI), National Geophysical Research Institute (NGRI) and Wadia Institute of Himalayan Geology (WIHG) in <span class="hlt">India</span>. We inverted the local P- and S-wave arrival times from about 20 local stations jointly for all available aftershocks implementing a technique which optimizes both <span class="hlt">earthquake</span> locations and crustal velocity model. Of these, seven events were recorded by more than 5 stations locating within 5o of the epicenters withazimuthal gap not greater than 90o. We used these events to compute the station correctionsfor local stations and applied these station corrections to relocate the entire sequence of the Chamoli aftershocks. The relocation vectors which indicate the direction toward which the events would move from the reference locations (in this case the GSI locations) suggest that for the majority of the seismic events they show movement towards the epicentral locations of the mainshock. The new locations of these events also show improvements in the error ellipse measurements. We have also investigated variations in crustal models using regional broadband seismograms from the mainshock recorded by the IMD stations in <span class="hlt">India</span> (IMD, 2000). Using a crustal model developed earlier by Bhattacharya using surface-wave dispersion for northern <span class="hlt">India</span> as a starting model, we conducted a systematic analysis of surface-wave dispersion characteristics recorded at these broadband stations. We synthesized f-k seismograms andexamined the relative amplitude of the Pnl waves to the surface waves and their absolutetravel-time differences. We used focal mechanism and depth that were independently determined by modeling teleseismic depth phases, pP and sP, and by modeling regional seismograms</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=PIA02796&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dearthquakes','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=PIA02796&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dearthquakes"><span>SRTM Stereo Pair: Bhuj, <span class="hlt">India</span>, Two Weeks After <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2001-01-01</p> <p>On January 26, 2001, the city of Bhuj suffered the most deadly <span class="hlt">earthquake</span> in <span class="hlt">India</span>'s history. About 20,000 people were killed, and more than one million homes were damaged or destroyed. Shortly after the quake, geologists conducted field investigations to inventory and analyze the natural effects of the event. Stereoscopic views, similar to this image, aided the geologists in locating landforms indicative of long-term (and possibly ongoing) deformation. Soon, elevation data from the Shuttle Radar Topography Mission (SRTM) will be used in the study of a wide variety of natural hazards worldwide.<p/>In this image, the city of Bhuj appears as a gray area at the scene center, and the city airport is toward the north (top). Vegetation appears green. Rugged but low relief hills of previously folded and faulted bedrock appear south (bottom) and northwest (upper-left) of the city.<p/>This stereoscopic image was generated by draping a Landsat satellite image (taken just two weeks after the <span class="hlt">earthquake</span>) over a preliminary SRTM elevation model. Two differing perspectives were then calculated, one for each eye. They can be seen in 3-D by viewing the left image with the right eye and the right image with the left eye (cross-eyed viewing) or by downloading and printing the image pair and viewing them with a stereoscope. When stereoscopically merged, the result is a vertically exaggerated view of the Earth's surface in its full three dimensions.<p/>Landsat has been providing visible and infrared views of the Earth since 1972. SRTM elevation data matches the 30-meter resolution of most Landsat images and will substantially help in analyses of the large and growing Landsat image archive. The Landsat 7 Thematic Mapper image used here was provided to the SRTM project by the United States Geological Survey, Earth Resources Observation Systems (EROS) Data Center, Sioux Falls, South Dakota.<p/>Elevation data used in this image was acquired by the Shuttle Radar Topography Mission (SRTM</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23359666','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23359666"><span>Coverage gap in maternal and child health services in <span class="hlt">India</span>: assessing trends and regional deprivation during 1992-2006.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kumar, Chandan; Singh, Prashant Kumar; Rai, Rajesh Kumar</p> <p>2013-12-01</p> <p>Increasing the coverage of key maternal, newborn and child health interventions is essential, if <span class="hlt">India</span> has to attain Millennium Development Goals 4 and 5. This study assesses the coverage gap in maternal and child health services across states in <span class="hlt">India</span> during 1992-2006 emphasizing the rural-urban disparities. Additionally, association between the coverage gap and under-5 mortality rate across states are illustrated. The three waves of National Family Health Survey (NFHS) conducted during 1992-1993 (NFHS-1), 1998-1999 (NFHS-2) and 2005-2006 (NFHS-3) were used to construct a composite index of coverage gap in four areas of health-care interventions: family planning, maternal and newborn care, immunization and treatment of sick children. The central, eastern and northeastern regions of <span class="hlt">India</span> reported a higher coverage gap in maternal and child health care services during 1992-2006, while the rural-urban difference in the coverage gap has increased in <span class="hlt">Gujarat</span>, Haryana, Rajasthan and Kerala over the period. The analysis also shows a significant positive relationship between the coverage gap index and under-five mortality rate across states. Region or area-specific focus in order to increase the coverage of maternal and child health care services in <span class="hlt">India</span> should be the priority of the policy-makers and programme executors.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_12 --> <div id="page_13" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="241"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014ClDy...42..749A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014ClDy...42..749A"><span>Documentary reconstruction of monsoon rainfall variability over western <span class="hlt">India</span>, 1781-1860</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Adamson, George C. D.; Nash, David J.</p> <p>2014-02-01</p> <p>Investigations into the climatic forcings that affect the long-term variability of the Indian summer monsoon are constrained by a lack of reliable rainfall data prior to the late nineteenth century. Extensive qualitative and quantitative meteorological information for the pre-instrumental period exists within historical documents, although these materials have been largely unexplored. This paper presents the first reconstruction of monsoon variability using documentary sources, focussing on western <span class="hlt">India</span> for the period 1781-1860. Three separate reconstructions are generated, for (1) Mumbai, (2) Pune and (3) the area of <span class="hlt">Gujarat</span> bordering the Gulf of Khambat. A composite chronology is then produced from the three reconstructions, termed the Western <span class="hlt">India</span> Monsoon Rainfall reconstruction (WIMR). The WIMR exhibits four periods of generally deficient monsoon rainfall (1780-1785, 1799-1806, 1830-1838 and 1845-1857) and three of above-normal rainfall (1788-1794, 1813-1828 and 1839-1844). The WIMR shows good correspondence with a dendroclimatic drought reconstruction for Kerala, although agreement with the western Indian portion of the tree-ring derived Monsoon Asia Drought Atlas is less strong. The reconstruction is used to examine the long-term relationship between the El Nino-Southern Oscillation (ENSO) and monsoon rainfall over western <span class="hlt">India</span>. This exhibits peaks and troughs in correlation over time, suggesting a regular long-term fluctuation. This may be an internal oscillation in the ENSO-monsoon system or may be related to volcanic aerosol forcings. Further reconstructions of monsoon rainfall are necessary to validate this. The study highlights uncertainties in existing published rainfall records for 1817-1846 for western <span class="hlt">India</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFMPA11A..03T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFMPA11A..03T"><span>Initiatives to Reduce <span class="hlt">Earthquake</span> Risk of Developing Countries</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tucker, B. E.</p> <p>2008-12-01</p> <p>The seventeen-year-and-counting history of the Palo Alto-based nonprofit organization GeoHazards International (GHI) is the story of many initiatives within a larger initiative to increase the societal impact of geophysics and civil engineering. GHI's mission is to reduce death and suffering due to <span class="hlt">earthquakes</span> and other natural hazards in the world's most vulnerable communities through preparedness, mitigation and advocacy. GHI works by raising awareness in these communities about their risk and about affordable methods to manage it, identifying and strengthening institutions in these communities to manage their risk, and advocating improvement in natural disaster management. Some of GHI's successful initiatives include: (1) creating an <span class="hlt">earthquake</span> scenario for Quito, Ecuador that describes in lay terms the consequences for that city of a probable <span class="hlt">earthquake</span>; (2) improving the curricula of Pakistani university courses about seismic retrofitting; (3) training employees of the Public Works Department of Delhi, <span class="hlt">India</span> on assessing the seismic vulnerability of critical facilities such as a school, a hospital, a police headquarters, and city hall; (4) assessing the vulnerability of the Library of Tibetan Works and Archives in Dharamsala, <span class="hlt">India</span>; (5) developing a seismic hazard reduction plan for a nonprofit organization in Kathmandu, Nepal that works to manage Nepal's seismic risk; and (6) assisting in the formulation of a resolution by the Council of the Organization for Economic Cooperation and Development (OECD) to promote school <span class="hlt">earthquake</span> safety among OECD member countries. GHI's most important resource, in addition to its staff and Board of Trustees, is its members and volunteer advisors, who include some of the world's leading earth scientists, <span class="hlt">earthquake</span> engineers, urban planners and architects, from the academic, public, private and nonprofit sectors. GHI is planning several exciting initiatives in the near future. One would oversee the design and construction of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.S53A2830K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.S53A2830K"><span>Microseismicity, Tectonics and Seismic Potential in the Western Himalayan Segment, NW Himalaya (<span class="hlt">india</span>) Region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kumar, S.; Parija, M. P.; Biswal, S.</p> <p>2016-12-01</p> <p>The NW Himalaya (<span class="hlt">India</span>) region covering Garhwal and Himachal province of <span class="hlt">India</span> is characterised by sustained seismicity during the past decades. We have relocated 423 <span class="hlt">earthquakes</span> in the NW Himalaya between 2004 and 2013 using more than 4495 P and 4453 S accurate P and S differential travel-times. We also have determined moment tensors for 8 (Mw >= 4.0) of these <span class="hlt">earthquakes</span> using their broadband regional waveforms. The geometry of the MHT plane has also been deduced in this study which varies along the strike of the Himalaya in flat and ramp segments with a dip range from 4° to 19° below the HFT in south to STD in the north. There are also two crustal ramps reported from this study having a depth variance below the MCT and STD between 12 to 22 km and 28 to 40 km depth respectively. The <span class="hlt">earthquake</span> potential prevailing in the western Himalaya seismic gap that lies between the epicentral zone of the 1905 Kangra <span class="hlt">earthquake</span> and the 1975 Kinnaur <span class="hlt">earthquake</span> has also been estimated and it is inferred that the total amount of energy released since the last great event is only a fraction (3-5%) of the accommodated energy (95-98%) i.e. if an <span class="hlt">earthquake</span> hits this NW Himalayan segment in future it's magnitude can be equivalent to a Mw³ 8.0. So the energy dissipated through previous <span class="hlt">earthquakes</span> is not sufficient to prevent an upcoming giant event.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2996570','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2996570"><span>Usage trends for memory and vitality-enhancing medicines: A pharmacoepidemiological study involving pharmacists of the <span class="hlt">Gujarat</span> region</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Shah, Jigna Samir; Goyal, R. K.</p> <p>2010-01-01</p> <p>Objective: The aim of the study was to explore the trends and rationale of use of memory and vitality-enhancing medicines (MVEM) in the <span class="hlt">Gujarat</span> region. Materials and Methods: A prospective pharmacoepidemiological study involving pharmacists of <span class="hlt">Gujarat</span> region was carried out in the year 2005. Pharmacists (n = 351) working in general and Ayurvedic medical stores were selected from 12 districts of <span class="hlt">Gujarat</span> region. The pharmacists were explained about the objective of the study and were given a pretested, validated questionnaire. Outcome Measures: The questionnaire included the questions regarding herbal MVEM used most commonly, percentage sale of herbal MVEM – sold with or without prescriptions – age group of patients and professional groups who used these drugs most commonly. Results: The number of individuals using MVEM was highest in the age group of 11–20 years (17.54%), followed by the 21–40 years group (17.12%), supporting the results that the professional group of students (17.29%) and the persons of business or service class (15.29%) are the highest users of these medicines. Evaluation of various constituents in the marketed polyherbal MVEM revealed that Brahmi (Bacopa monniera), Shankhpushpi (Evolvulus alsinoides), Ashwangandha (Withania somnifera), Jatamansi (Nardostychos jatamansi), Vacha (Acorus calamus) and Amla (Phyllanthus emblica) were the common ingredients in the polyherbal preparations. Conclusions: This study highlights commonly used Ayurvedic medicines that can be explored for safely enhancing memory and vitality performance. Hence, detailed and scientifically designed research on these drugs would help to identify safe and effective drugs for enhancing the same. PMID:21170204</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JSeis..22...35N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JSeis..22...35N"><span><span class="hlt">Earthquake</span> induced liquefaction hazard, probability and risk assessment in the city of Kolkata, <span class="hlt">India</span>: its historical perspective and deterministic scenario</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nath, Sankar Kumar; Srivastava, Nishtha; Ghatak, Chitralekha; Adhikari, Manik Das; Ghosh, Ambarish; Sinha Ray, S. P.</p> <p>2018-01-01</p> <p>Liquefaction-induced ground failure is one amongst the leading causes of infrastructure damage due to the impact of large <span class="hlt">earthquakes</span> in unconsolidated, non-cohesive, water saturated alluvial terrains. The city of Kolkata is located on the potentially liquefiable alluvial fan deposits of Ganga-Bramhaputra-Meghna Delta system with subsurface litho-stratigraphic sequence comprising of varying percentages of clay, cohesionless silt, sand, and gravel interbedded with decomposed wood and peat. Additionally, the region has moderately shallow groundwater condition especially in the post-monsoon seasons. In view of burgeoning population, there had been unplanned expansion of settlements in the hazardous geological, geomorphological, and hydrological conditions exposing the city to severe liquefaction hazard. The 1897 Shillong and 1934 Bihar-Nepal <span class="hlt">earthquakes</span> both of M w 8.1 reportedly induced Modified Mercalli Intensity of IV-V and VI-VII respectively in the city reportedly triggering widespread to sporadic liquefaction condition with surface manifestation of sand boils, lateral spreading, ground subsidence, etc., thus posing a strong case for liquefaction potential analysis in the terrain. With the motivation of assessing seismic hazard, vulnerability, and risk of the city of Kolkata through a consorted federal funding stipulated for all the metros and upstart urban centers in <span class="hlt">India</span> located in BIS seismic zones III, IV, and V with population more than one million, an attempt has been made here to understand the liquefaction susceptibility condition of Kolkata under the impact of <span class="hlt">earthquake</span> loading employing modern multivariate techniques and also to predict deterministic liquefaction scenario of the city in the event of a probabilistic seismic hazard condition with 10% probability of exceedance in 50 years and a return period of 475 years. We conducted in-depth geophysical and geotechnical investigations in the city encompassing 435 km2 area. The stochastically</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18..532B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18..532B"><span>Prediction of <span class="hlt">earthquake</span>-triggered landslide event sizes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Braun, Anika; Havenith, Hans-Balder; Schlögel, Romy</p> <p>2016-04-01</p> <p> contribution for the prediction of the number (and concentration) of induced landslides. This, for instance, partly explains why the Wenchuan 2008 <span class="hlt">earthquake</span> triggered far more landslides than the Nepal 2015 <span class="hlt">earthquake</span>. Moreover, according to our prediction the most severe <span class="hlt">earthquake</span>-triggered landslide event would have been the Assam 1950 <span class="hlt">earthquake</span> (<span class="hlt">India</span>), followed by the 2008 Wenchuan <span class="hlt">earthquake</span>. Regarding the overall performance of our prediction method it can be seen that the number of landslides is overestimated for a series of <span class="hlt">earthquakes</span>, while the size of the affected area is often underestimated. Especially for older events the incompleteness of the published catalogues can partly explain the overestimation of the landslide numbers. The underestimation of the affected area however is real and must be attributed to particular remote effects of <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3954798','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3954798"><span>Heat-Related Mortality in <span class="hlt">India</span>: Excess All-Cause Mortality Associated with the 2010 Ahmedabad Heat Wave</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Azhar, Gulrez Shah; Mavalankar, Dileep; Nori-Sarma, Amruta; Rajiva, Ajit; Dutta, Priya; Jaiswal, Anjali; Sheffield, Perry; Knowlton, Kim; Hess, Jeremy J.; Azhar, Gulrez Shah; Deol, Bhaskar; Bhaskar, Priya Shekhar; Hess, Jeremy; Jaiswal, Anjali; Khosla, Radhika; Knowlton, Kim; Mavalankar, Mavalankar; Rajiva, Ajit; Sarma, Amruta; Sheffield, Perry</p> <p>2014-01-01</p> <p>Introduction In the recent past, spells of extreme heat associated with appreciable mortality have been documented in developed countries, including North America and Europe. However, far fewer research reports are available from developing countries or specific cities in South Asia. In May 2010, Ahmedabad, <span class="hlt">India</span>, faced a heat wave where the temperatures reached a high of 46.8°C with an apparent increase in mortality. The purpose of this study is to characterize the heat wave impact and assess the associated excess mortality. Methods We conducted an analysis of all-cause mortality associated with a May 2010 heat wave in Ahmedabad, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, to determine whether extreme heat leads to excess mortality. Counts of all-cause deaths from May 1–31, 2010 were compared with the mean of counts from temporally matched periods in May 2009 and 2011 to calculate excess mortality. Other analyses included a 7-day moving average, mortality rate ratio analysis, and relationship between daily maximum temperature and daily all-cause death counts over the entire year of 2010, using month-wise correlations. Results The May 2010 heat wave was associated with significant excess all-cause mortality. 4,462 all-cause deaths occurred, comprising an excess of 1,344 all-cause deaths, an estimated 43.1% increase when compared to the reference period (3,118 deaths). In monthly pair-wise comparisons for 2010, we found high correlations between mortality and daily maximum temperature during the locally hottest “summer” months of April (r = 0.69, p<0.001), May (r = 0.77, p<0.001), and June (r = 0.39, p<0.05). During a period of more intense heat (May 19–25, 2010), mortality rate ratios were 1.76 [95% CI 1.67–1.83, p<0.001] and 2.12 [95% CI 2.03–2.21] applying reference periods (May 12–18, 2010) from various years. Conclusion The May 2010 heat wave in Ahmedabad, <span class="hlt">Gujarat</span>, <span class="hlt">India</span> had a substantial effect on all-cause excess mortality, even in this city where hot</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.S41B2773P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.S41B2773P"><span>Seismotectonics of the Trans-Himalaya, Eastern Ladakh, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Paul, A.</p> <p>2016-12-01</p> <p>The eastern Ladakh-Karakoram zone is the northwest part of the trans-Himalayan belt which bears signature of the <span class="hlt">India</span>-Asia collision process in the form of suture zones and exhumed blocks that underwent deep subduction and intra-continental crustal scale fault zones.The seismotectonic scenario of northwest part of <span class="hlt">India</span>-Asia collision zone has been studied by analyzing the local <span class="hlt">earthquake</span> data (M 1.4-4.3) recorded by a broadband seismological network consisting of 14 stations. Focal Mechanism Solution (FPS) of 13 selected <span class="hlt">earthquakes</span> were computed through waveform inversion of three-component broadband records. Depth distribution of the <span class="hlt">earthquakes</span> and FPS of local <span class="hlt">earthquakes</span> obtained through waveform inversion reveal the kinematics of the major fault zones present in Eastern Ladakh. The most pronounced cluster of seismicity is observed in the Karakoram Fault (KF) zone up to a depth of 65 km. The FPS reveals transpressive environment with the strike of inferred fault plane roughly parallel to the KF. It is inferred that the KF at least penetrates up to the lower crust and is a manifestation of active under thrusting of Indian lower crust beneath Tibet. Two clusters of micro seismicity is observed at a depth range of 5-20 km at north western and southeastern fringe of the Tso Morari gneiss dome which can be correlated to the activities along the Zildat fault and Karzok fault respectively. The FPSs estimated for representative <span class="hlt">earthquakes</span> show thrust fault solutions for the Karzok fault and normal fault solution for the Zildat fault. It is inferred that the Zildat fault is acting as detachment, facilitating the exhumation of the Tso Morari dome. On the other hand, the Tso Morari dome is thrusting over the Karzok ophiolite on its southern margin along the Karzokfault, due to gravity collapse.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5039870','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5039870"><span>Spine surgery in Nepal: the 2015 <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2015-01-01</p> <p>At noon on Saturday, 25 April 2015, a 7.8 magnitude <span class="hlt">earthquake</span> struck Nepal. It was centered in the Himalaya northwest of Kathmandu, the capital of over 1 million people. The violent tremors were felt as far away as New Delhi, <span class="hlt">India</span> 1,000 km from the epicenter, but the worst of its destructive force was experienced in the heavily populated Kathmandu valley and in the remote mountainous villages of the Himalaya. Ancient temples crumbled; poorly constructed buildings collapsed; men, women, and children were trapped and injured, sometimes fatally. Avalanches killed mountain climbers, Sherpa guides, and porters at Everest base camp (EBC). The death toll to date exceeds 8,600 with as many as 20,000 injured. Spinal Health International (SHI), a nonprofit volunteer organization, has been active in Nepal in past years and responded to requests by Nepali spine surgeons for assistance with traumatic spine injury victims following the <span class="hlt">earthquake</span>. SHI volunteers were present during the 2nd major <span class="hlt">earthquake</span> of magnitude 7.3 on 12 May 2015. Past and current experiences in Nepal will be presented. PMID:27683676</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19810040','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19810040"><span>Isolation and identification of a Candida digboiensis strain from an extreme acid mine drainage of the Lignite Mine, <span class="hlt">Gujarat</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Patel, Mitesh J; Tipre, Devayani R; Dave, Shailesh R</p> <p>2009-12-01</p> <p>An extremely acidic mine drainage (AMD) water sample was collected in 1998 and 2008 from Panandhro lignite mine, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. The yeast isolated from this sample was identified using mini API identification system, as a member of genus Candida. The major cellular fatty acids detected by FAME from the isolate are C(16:0) and C(18:2) (cis 9,12)/C(18:0alpha) as 25.23 and 19.5%, respectively. The isolate was identified as Candida digboiensis by 18S rRNA gene sequence analysis and designated as Candida digboiensis SRDyeast1. Phylogenetic analysis using D1/D2 variable domains showed that the closest relative of this strain is Candida blankii with 3% divergence. This organism has been reported for the first time from the lignite mine AMD sample, and for cellular fatty acid analysis. This yeast is able to survive in the AMD sample preserved at 10-42 degrees C temperature since last 10 years along with iron oxidizing microorganisms. It can grow in the presence of 40% glucose, 10% NaCl and in the pH range of 1 to 10. The isolate is capable of producing enzymes like protease and lipase. This isolate differs from the type strain Candida digboiensis in as many as six physiological and metabolic characteristics.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007Tectp.431..221P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007Tectp.431..221P"><span>Specific variations of air temperature and relative humidity around the time of Michoacan <span class="hlt">earthquake</span> M8.1 Sept. 19, 1985 as a possible indicator of interaction between tectonic plates</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pulinets, S. A.; Dunajecka, M. A.</p> <p>2007-02-01</p> <p>The recent development of the Lithosphere-Atmosphere-Ionosphere (LAI) coupling model and experimental data of remote sensing satellites on thermal anomalies before major strong <span class="hlt">earthquakes</span> have demonstrated that radon emanations in the area of <span class="hlt">earthquake</span> preparation can produce variations of the air temperature and relative humidity. Specific repeating pattern of humidity and air temperature variations was revealed as a result of analysis of the meteorological data for several tens of strong <span class="hlt">earthquakes</span> all over the world. The main physical process responsible for the observed variations is the latent heat release due to water vapor condensation on ions produced as a result of air ionization by energetic α-particles emitted by 222Rn. The high effectiveness of this process was proved by the laboratory and field experiments; hence the specific variations of air humidity and temperature can be used as indicator of radon variations before <span class="hlt">earthquakes</span>. We analyzed the historical meteorological data all over the Mexico around the time of one of the most destructive <span class="hlt">earthquakes</span> (Michoacan <span class="hlt">earthquake</span> M8.1) that affected the Mexico City on September 19, 1985. Several distinct zones of specific variations of the air temperature and relative humidity were revealed that may indicate the different character of radon variations in different parts of Mexico before the Michoacan <span class="hlt">earthquake</span>. The most interesting result on the specific variations of atmosphere parameters was obtained at Baja California region close to the border of Cocos and Rivera tectonic plates. This result demonstrates the possibility of the increased radon variations not only in the vicinity of the <span class="hlt">earthquake</span> source but also at the border of interacting tectonic plates. Recent results on Thermal InfraRed (TIR) anomalies registered by Meteosat 5 before the <span class="hlt">Gujarat</span> <span class="hlt">earthquake</span> M7.9 on 26 of January 2001 supports the idea on the possibility of thermal effects at the border of interacting tectonic plates.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70025916','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70025916"><span>Estimation of ground motion for Bhuj (26 January 2001; Mw 7.6 and for future <span class="hlt">earthquakes</span> in <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Singh, S.K.; Bansal, B.K.; Bhattacharya, S.N.; Pacheco, J.F.; Dattatrayam, R.S.; Ordaz, M.; Suresh, G.; ,; Hough, S.E.</p> <p>2003-01-01</p> <p>Only five moderate and large <span class="hlt">earthquakes</span> (Mw ???5.7) in <span class="hlt">India</span>-three in the Indian shield region and two in the Himalayan arc region-have given rise to multiple strong ground-motion recordings. Near-source data are available for only two of these events. The Bhuj <span class="hlt">earthquake</span> (Mw 7.6), which occurred in the shield region, gave rise to useful recordings at distances exceeding 550 km. Because of the scarcity of the data, we use the stochastic method to estimate ground motions. We assume that (1) S waves dominate at R < 100 km and Lg waves at R ??? 100 km, (2) Q = 508f0.48 is valid for the Indian shield as well as the Himalayan arc region, (3) the effective duration is given by fc-1 + 0.05R, where fc is the corner frequency, and R is the hypocentral distance in kilometer, and (4) the acceleration spectra are sharply cut off beyond 35 Hz. We use two finite-source stochastic models. One is an approximate model that reduces to the ??2-source model at distances greater that about twice the source dimension. This model has the advantage that the ground motion is controlled by the familiar stress parameter, ????. In the other finite-source model, which is more reliable for near-source ground-motion estimation, the high-frequency radiation is controlled by the strength factor, sfact, a quantity that is physically related to the maximum slip rate on the fault. We estimate ???? needed to fit the observed Amax and Vmax data of each <span class="hlt">earthquake</span> (which are mostly in the far field). The corresponding sfact is obtained by requiring that the predicted curves from the two models match each other in the far field up to a distance of about 500 km. The results show: (1) The ???? that explains Amax data for shield events may be a function of depth, increasing from ???50 bars at 10 km to ???400 bars at 36 km. The corresponding sfact values range from 1.0-2.0. The ???? values for the two Himalayan arc events are 75 and 150 bars (sfact = 1.0 and 1.4). (2) The ???? required to explain Vmax data</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1452697','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1452697"><span>Greening the Grid: Pathways to Integrate 175 Gigawatts of Renewable Energy into <span class="hlt">India</span>'s Electric Grid, Regional Study: <span class="hlt">Gujarat</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Cochran, Jaquelin M; Palchak, Joseph D; Ehlen, Annaliese K</p> <p></p> <p>This chapter on Andhra Pradesh is one of six state chapters included in Appendix C of 'Greening the Grid: Pathways to Integrate 175 Gigawatts of Renewable Energy into <span class="hlt">India</span>'s Electric Grid, Vol. II - Regional Study' (the Regional Study). The objective of the state chapters is to provide modeling assumptions, results, and next steps to use and improve the model specific to each state. The model has inherent uncertainties, particularly in how the intrastate transmission network and RE generation projects will develop (e.g., locations, capacities). The model also does not include information on contracts or must-run status of particular plantsmore » for reliability purposes. By providing details on the higher spatial resolution model of 'Greening the Grid: Pathways to Integrate 175 Gigawatts of Renewable Energy into <span class="hlt">India</span>'s Electric Grid, Vol. II - Regional Study' (the Regional Study), which better represents the impact of congestion on least-cost scheduling and dispatch, provides a deeper understanding of the relationship among renewable energy (RE) location, transmission, and system flexibility with regard to RE integration, compared to 'Greening the Grid: Pathways to Integrate 175 Gigawatts of Renewable Energy into <span class="hlt">India</span>'s Electric Grid, Vol. I - National Study.'« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/21148982-interaction-between-himalaya-flexed-indian-plate-spatial-fluctuations-seismic-hazard-india-past-millennium','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/21148982-interaction-between-himalaya-flexed-indian-plate-spatial-fluctuations-seismic-hazard-india-past-millennium"><span>Interaction Between the Himalaya and the Flexed Indian Plate--Spatial Fluctuations in Seismic Hazard in <span class="hlt">India</span> in the Past Millennium?</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Bilham, Roger; Szeliga, Walter</p> <p>2008-07-08</p> <p>Between the tenth and early 16th centuries three megaquakes allowed most of the northern edge of the Indian plate to slip 20-24 m northward relative to the overlying Himalaya. Although the renewal time for <span class="hlt">earthquakes</span> with this large amount of slip is less than 1300 years given a geodetic convergence rate of 16-20 mm/yr, recently developed scaling laws for the Himalaya suggest that the past 200 years of great <span class="hlt">earthquakes</span> may be associated with slip of less than 10 m and renewal times of approximately 500 years. These same theoretical models show that the rupture lengths of the Himalaya's Medievalmore » <span class="hlt">earthquakes</span> (300-600 km) are too short to permit 24 m of slip given the relationships demonstrated by recent events. There is thus reason to suppose that recent <span class="hlt">earthquakes</span> may have responded to different elastic driving forces from those that drove the megaquakes of Medieval times.An alternative source of energy to drive Himalayan <span class="hlt">earthquakes</span> exists in the form of the elastic and gravitational energy stored in flexure of the Indian plate. The flexure is manifest in the form of a 200-450 m high bulge in central <span class="hlt">India</span>, which is sustained by the forces of collision and by the end-loading of the plate by the Himalaya and southern Tibet. These flexural stresses are responsible for <span class="hlt">earthquakes</span> in the sub-continent. The abrupt release of stress associated with the northward translation of the northern edge of the Indian plate by 24 m, were the process entirely elastic, would result in a deflation of the crest of the bulge by roughly 0.8 m. Geometrical changes, however, would be moderated by viscous rheologies in the plate and by viscous flow in the mantle in the following centuries.The hypothesized relaxation of flexural geometry following the Himalayan megaquake sequence would have the effect of backing-off stresses throughout central <span class="hlt">India</span> resulting in quiescence both in the Himalaya and the Indian plate. The historical record shows an absence of great Himalayan</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23520740','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23520740"><span>Epidemiological survey of equine influenza in horses in <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mavadiya, S V; Raval, S K; Mehta, S A; Kanani, A N; Vagh, A A; Tank, P H; Patel, P R</p> <p>2012-12-01</p> <p>A highly contagious virus infection in horses, influenza is the single most important equine respiratory disease in the world. This paper presents details of a one-year study (1 June 2008 to 31 May 2009) to determine the prevalence of equine influenza in the horses of <span class="hlt">Gujarat</span> State in <span class="hlt">India</span>. The prevalence of equine influenza A/equi-2 was 12.02%, but none of the samples were positive for equine influenza A/equi-1. The prevalence of equine influenza (A/equi-2) was 15.38%, 11.94%, 10.18%, and 9.09% in horses of the Kathiyawari breed, a non-descript breed, the Marwari breed and the Indian Thoroughbred breed, respectively. The highest prevalence of influenza was observed in yearlings (17.48%) and prevalence was at its highest in the month of April (28.89%). The prevalence rate in males, females and geldings was 11.95%, 10.38% and 8.47%, respectively. The mortality rate and case fatality rate were 1.28% and 10.64%, respectively.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JAESc.146..296A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JAESc.146..296A"><span>Lignite deposits of the Kutch Basin, western <span class="hlt">India</span>: Carbon isotopic and palynological signatures of the early Eocene hyperthermal event ETM2</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Agrawal, Shailesh; Verma, Poonam; Rao, M. R.; Garg, Rahul; Kapur, Vivesh V.; Bajpai, Sunil</p> <p>2017-09-01</p> <p>This study presents new results of combined palynological and stable carbon isotope (δ13C) investigations carried out in the well known lignite sequence at Panandhro, District Kutch, in the <span class="hlt">Gujarat</span> state of western <span class="hlt">India</span>. Dinoflagellate cysts and associated spore-pollen assemblage assign an early Eocene (Ypresian) age to the lignitic succession at Panandhro. Furthermore, a pronounced negative Carbon Isotope Excursion (CIE) of about 2.7‰, correlated to the Second Eocene Thermal Maximum (53.7 Ma), a globally recognized hyperthermal event, was discovered in the middle part of the succession, consistent with the palynological constraints. This is the first record of an Eocene hyperthermal event (ETM2) from the Kutch Basin. Our data has regional implications for the age of the lignitic sequences across western <span class="hlt">India</span> as it demonstrates that there is no significant age difference between the lignite deposits of the Kutch and Cambay basins. Our results also support a Lutetian age for the previously described vertebrate fossils, including whales, from the Panandhro mine section.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014ISPAr.XL8..411C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014ISPAr.XL8..411C"><span>Energy Balance of Rural Ecosystems In <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chhabra, A.; Madhava Rao, V.; Hermon, R. R.; Garg, A.; Nag, T.; Bhaskara Rao, N.; Sharma, A.; Parihar, J. S.</p> <p>2014-11-01</p> <p><span class="hlt">India</span> is predominantly an agricultural and rural country. Across the country, the villages vary in geographical location, area, human and livestock population, availability of resources, agricultural practices, livelihood patterns etc. This study presents an estimation of net energy balance resulting from primary production vis-a-vis energy consumption through various components in a "Rural Ecosystem". Seven sites located in different agroclimatic regions of <span class="hlt">India</span> were studied. An end use energy accounting "Rural Energy Balance Model" is developed for input-output analysis of various energy flows of production, consumption, import and export through various components of crop, trees outside forest plantations, livestock, rural households, industry or trade within the village system boundary. An integrated approach using field, ancillary, GIS and high resolution IRS-P6 Resourcesat-2 LISS IV data is adopted for generation of various model inputs. The primary and secondary field data collection of various energy uses at household and village level were carried out using structured schedules and questionnaires. High resolution multi-temporal Resourcesat-2 LISS IV data (2013-14) was used for generating landuse/landcover maps and estimation of above-ground Trees Outside Forests phytomass. The model inputs were converted to energy equivalents using country-specific energy conversion factors. A comprehensive geotagged database of sampled households and available resources at each study site was also developed in ArcGIS framework. Across the study sites, the estimated net energy balance ranged from -18.8 Terra Joules (TJ) in a high energy consuming Hodka village, <span class="hlt">Gujarat</span> to 224.7 TJ in an agriculture, aquaculture and plantation intensive Kollaparru village, Andhra Pradesh. The results indicate that the net energy balance of a Rural Ecosystem is largely driven by primary production through crops and natural vegetation. This study provides a significant insight to policy</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26688974','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26688974"><span>Bioaccumulation of heavy metals by freshwater algal species of Bhavnagar, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Jaiswar, Santial; Kazi, Mudassar Anisoddin; Mehta, Shailesh</p> <p>2015-11-01</p> <p>The present study investigated copper, cadmium, lead and zinc accumulation in algal species Oedogonium, Cladophora, Oscillatoria and Spirogyra from freshwater habitats of Bhavnagar, <span class="hlt">India</span>. Eight different locations were periodically sampled during August 2009 to March 2011. The general trend of heavy metal concentrations in all the algal species in present study (except at few stations), were found to be in the following order: Zn > Cu > Pb > Cd. Highest accumulation of Cu was recorded in Oedogonium, while Cladophora showed highest accumulation of Pb signifying a good bioaccumulator. Oscillatoria and Oedogonium were highest Zn accumulating algae which showed significant difference between the means at P < 0.05. ANOVA was performed for comparing significance mean between the groups and within the group for heavy metals in water. The concentration of heavy metals in water was in the following order: Zn > Cu > Pb > Cd. The present study showed that Oedogonium, Cladophora, Oscillatoria and Spirogyra were excellent bioaccumulator and could be utilized as biomonitoring agents in water bodies receiving waste contaminated by metals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25389183','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25389183"><span>Barriers to use of oral rehydration salts for child diarrhea in the private sector: evidence from <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wagner, Zachary; Shah, Manan; Sood, Neeraj</p> <p>2015-02-01</p> <p>Diarrhea is the second leading cause of child mortality in <span class="hlt">India</span>. Most deaths are cheaply preventable with the use of oral rehydration salts (ORS), yet many health providers still fail to provide ORS to children seeking diarrheal care. In this study, we use survey data to assess whether children visiting private providers for diarrheal care were less likely to use ORS than those visiting public providers. Results suggest that children who visited private providers were 9.5 percentage points less likely to have used ORS than those who visited public providers (95% CI 5-14). We complimented these results with in-depth interviews of 21 public and 17 private doctors in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, assessing potential drivers of public-private disparities in ORS use. Interview results suggested that lack of direct medication dispensing in the private sector might be a key barrier to ORS use in the private sector. © The Author [2014]. Published by Oxford University Press. All rights reserved. For Permissions, please email: journals.permissions@oup.com.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4036042','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4036042"><span>Carbonate-Dissolving Bacteria from ‘Miliolite’, a Bioclastic Limestone, from Gopnath, <span class="hlt">Gujarat</span>, Western <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Subrahmanyam, Gangavarapu; Vaghela, Ravi; Bhatt, Nilesh Pinakinprasad; Archana, Gattupalli</p> <p>2012-01-01</p> <p>In the present investigation, the abundance and molecular phylogeny of part of the culturable bacterial population involved in the dissolution of “miliolite”, a bioclastic limestone, from Gopnath, <span class="hlt">India</span>, was studied. Carbonate-dissolving bacteria were isolated, enumerated and screened for their ability to dissolve miliolite. Amplified ribosomal DNA restriction analysis (ARDRA) indicated 14 operational taxonomic units (OTUs) to be distributed in 5 different clades at a similarity coefficient of 0.85. Then, 16S rRNA sequence analysis helped to decipher that the majority of carbonate-dissolving bacteria were affiliated to phyla Firmicutes (Families Bacillaceae and Staphylococcaceae) and Actinobacteria (Family Promicromonosporaceae) indicating their role in miliolite weathering. PMID:22446314</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_13 --> <div id="page_14" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="261"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4664396','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4664396"><span>Effect of Climate Change on Invasion Risk of Giant African Snail (Achatina fulica Férussac, 1821: Achatinidae) in <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Rekha Sarma, Roshmi; Munsi, Madhushree; Neelavara Ananthram, Aravind</p> <p>2015-01-01</p> <p>The Giant African Snail (Achatina fulica) is considered to be one the world’s 100 worst invasive alien species. The snail has an impact on native biodiversity, and on agricultural and horticultural crops. In <span class="hlt">India</span>, it is known to feed on more than fifty species of native plants and agricultural crops and also outcompetes the native snails. It was introduced into <span class="hlt">India</span> in 1847 and since then it has spread all across the country. In this paper, we use ecological niche modeling (ENM) to assess the distribution pattern of Giant African Snail (GAS) under different climate change scenarios. The niche modeling results indicate that under the current climate scenario, Eastern <span class="hlt">India</span>, peninsular <span class="hlt">India</span> and the Andaman and Nicobar Islands are at high risk of invasion. The three different future climate scenarios show that there is no significant change in the geographical distribution of invasion prone areas. However, certain currently invaded areas will be more prone to invasion in the future. These regions include parts of Bihar, Southern Karnataka, parts of <span class="hlt">Gujarat</span> and Assam. The Andaman and Nicobar and Lakshadweep Islands are highly vulnerable to invasion under changed climate. The Central Indian region is at low risk due to high temperature and low rainfall. An understanding of the invasion pattern can help in better management of this invasive species and also in formulating policies for its control. PMID:26618637</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26618637','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26618637"><span>Effect of Climate Change on Invasion Risk of Giant African Snail (Achatina fulica Férussac, 1821: Achatinidae) in <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sarma, Roshmi Rekha; Munsi, Madhushree; Ananthram, Aravind Neelavara</p> <p>2015-01-01</p> <p>The Giant African Snail (Achatina fulica) is considered to be one the world's 100 worst invasive alien species. The snail has an impact on native biodiversity, and on agricultural and horticultural crops. In <span class="hlt">India</span>, it is known to feed on more than fifty species of native plants and agricultural crops and also outcompetes the native snails. It was introduced into <span class="hlt">India</span> in 1847 and since then it has spread all across the country. In this paper, we use ecological niche modeling (ENM) to assess the distribution pattern of Giant African Snail (GAS) under different climate change scenarios. The niche modeling results indicate that under the current climate scenario, Eastern <span class="hlt">India</span>, peninsular <span class="hlt">India</span> and the Andaman and Nicobar Islands are at high risk of invasion. The three different future climate scenarios show that there is no significant change in the geographical distribution of invasion prone areas. However, certain currently invaded areas will be more prone to invasion in the future. These regions include parts of Bihar, Southern Karnataka, parts of <span class="hlt">Gujarat</span> and Assam. The Andaman and Nicobar and Lakshadweep Islands are highly vulnerable to invasion under changed climate. The Central Indian region is at low risk due to high temperature and low rainfall. An understanding of the invasion pattern can help in better management of this invasive species and also in formulating policies for its control.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003AGUFM.S41B..01K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003AGUFM.S41B..01K"><span>Energy Partition and Variability of <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kanamori, H.</p> <p>2003-12-01</p> <p> mechanically dissipated during faulting. In the context of the slip-weakening model, EG can be estimated from Δ W0 and ER. Alternatively, EG can be estimated from the laboratory data on the surface energy, the grain size and the total volume of newly formed fault gouge. This method suggests that, for crustal <span class="hlt">earthquakes</span>, EG/E_R is very small, less than 0.2 even for extreme cases, for <span class="hlt">earthquakes</span> with MW>7. This is consistent with the EG estimated with seismological methods, and the fast rupture speeds during most large <span class="hlt">earthquakes</span>. For shallow subduction-zone <span class="hlt">earthquakes</span>, EG/E_R varies substantially depending on the tectonic environments. EH: Direct estimation of EH is difficult. However, even with modest friction, EH can be very large, enough to melt or even dissociate a significant amount of material near the slip zone for large events with large slip, and the associated thermal effects may have significant effects on fault dynamics. The energy partition varies significantly for different types of <span class="hlt">earthquakes</span>, e.g. large <span class="hlt">earthquakes</span> on mature faults, large <span class="hlt">earthquakes</span> on faults with low slip rates, subduction-zone <span class="hlt">earthquakes</span>, deep focus <span class="hlt">earthquakes</span> etc; this variability manifests itself in the difference in the evolution of seismic slip pattern. The different behaviors will be illustrated using the examples for large <span class="hlt">earthquakes</span>, including, the 2001 Kunlun, the 1998 Balleny Is., the 1994 Bolivia, the 2001 <span class="hlt">India</span> <span class="hlt">earthquake</span>, the 1999 Chi-Chi, and the 2002 Denali <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18555497','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18555497"><span>Post-<span class="hlt">earthquake</span> outbreak of rotavirus gastroenteritis in Kashmir (<span class="hlt">India</span>): an epidemiological analysis.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Karmakar, Somenath; Rathore, Abhilakh Singh; Kadri, Syed Manzoor; Dutt, Som; Khare, Shashi; Lal, Shiv</p> <p>2008-10-01</p> <p>An <span class="hlt">earthquake</span> struck Kashmir on 8 October 2005. A central team of public health specialists was sent to Kashmir to assess the public health measures required following the <span class="hlt">earthquake</span>, and to assist in institution of public health measures. Epidemiological and environmental investigation in Tangdar block (Kupwara district) and Uri Tehsil (Baramula district). Visits to villages affected by the <span class="hlt">earthquake</span>, rehabilitation camps and health care, examination of cases with acute diarrhoeal disease (ADD), environmental observations, collection of clinical samples from ADD cases and environmental samples from drinking water sources, and laboratory methods. In total, 1783 cases of ADD were reported between 14 October and 17 December 2005 in Tangdar (population 65000). The overall attack rate was 20% in children under 4 years of age. Twelve cases of ADD with loose motions without blood were studied, and 11 rectal swabs and one stool sample were processed. No bacterial enteropathogens could be isolated, but three of the 12 samples yielded rotavirus antigen on enzyme-linked immunosorbent assay. Twelve of 13 (92.3%) water samples, collected from various stream or tap water (source: spring/stream) sources, were unsatisfactory (P=0.001) using the H(2)S strip method compared with other sources (well/mineral water). All eight water sources in Tangdar block were unsatisfactory, indicated by blackening of H(2)S filter paper strips. Following the <span class="hlt">earthquake</span>, drinking stream water or tap water without boiling or chlorination may have led to a common source water-borne outbreak of rotavirus gastroenteritis. Other contributing factors were: overcrowding; poor sanitation; open-air defaecation; poor hygiene; and living in makeshift camps near streams. Person-to-person transmission may also have contributed to perpetuation of the outbreak. Following the establishment of medical camps and information, education and communication regarding the need to drink boiled water and follow safer</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002AGUFM.S12C..01B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002AGUFM.S12C..01B"><span>No Great <span class="hlt">Earthquake</span> in the Central Himalaya Since 1505: a Possible Future M>=8.2 event?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bilham, R.; Ambraseys, N.</p> <p>2002-12-01</p> <p>The re-evaluation of the past several centuries of damaging Himalayan <span class="hlt">earthquakes</span> has largely decreased their magnitudes and/or rupture areas, with one exception. An <span class="hlt">earthquake</span> in 1505 that simultaneously destroyed Indian cities near Agra, and Tibetan monasteries between longitudes 78° and 84° appears to be larger than any known hitherto. It occurred exactly one month after a catastrophic <span class="hlt">earthquake</span> in Kabul, and accounts from the two <span class="hlt">earthquakes</span> have sometimes been confused. Although the data in Tibetan accounts are sparse the event appears to have had equal violence along the 600 km northern Himalaya and in the northern plains of <span class="hlt">India</span>. From this we infer a rupture zone possibly twice as long as that associated with recent Himalayan <span class="hlt">earthquakes</span>, corresponding to the segment that has hitherto been termed the Central Himalayan Gap. An enigmatic observation is that surface ruptures have been exhumed in trench investigations but have not been reported from the past two centuries of 7.8<M<8.1 <span class="hlt">earthquakes</span> in the western and central Himalaya. These ruptures are unlikely to have developed aseismically since recent geodetic data indicate that creep processes beneath the Lesser Himalaya are negligible. A possible interpretation of the absence of recent surface ruptures is that they are associated only with the very largest Himalayan <span class="hlt">earthquakes</span>, such as is inferred to have occurred in 1505. Geodetic data suggest that present convergence between <span class="hlt">India</span> and southern Tibet of 16-18 mm/year is developing as elastic strain in the Greater Himalaya. Should this have prevailed since 1505 the so-called Central Himalayan Gap may have accumulated as much as 9 m of potential slip, sufficient to drive a Mw=8.2 <span class="hlt">earthquake</span>. The infancy of systematic trench investigations, and the absence of a long continuous written history in the Himalaya, prevents conclusions about the timing of this inferred future M=8.2 event. No forecast is currently possible, but since convergence adds roughly 1</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010cosp...38..895K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010cosp...38..895K"><span>Anomalous variation in GPS based TEC measurements prior to the 30 September 2009 Sumatra <span class="hlt">Earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Karia, Sheetal; Pathak, Kamlesh</p> <p></p> <p>This paper investigates the features of pre-<span class="hlt">earthquake</span> ionospheric anomalies in the total elec-tron content (TEC) data obtained on the basis of regular GPS observations from the GPS receiver at SVNIT Surat (21.16 N, 72.78 E Geog) located at the northern crest of equatorial anomaly region. The data has been analysed for 5 different <span class="hlt">earthquakes</span> that occurred during 2009 in <span class="hlt">India</span> and its neighbouring regions. Our observation shows that for the cases of the <span class="hlt">earthquake</span>, in which the preparation area lies between the crests of the equatorial anomaly close to the geomagnetic equator the enhancement in TEC was followed by a depletion in TEC on the day of <span class="hlt">earthquake</span>, which may be connected to the equatorial anomaly shape distortions. For the analysis of the ionospheric effects of one of such case-the 30 September 2009 Sumatra <span class="hlt">earthquake</span>, Global Ionospheric Maps of TEC were used. The possible influence of the <span class="hlt">earth-quake</span> preparation processes on the main low-latitude ionosphere peculiarity—the equatorial anomaly—is discussed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=india&pg=2&id=EJ1170333','ERIC'); return false;" href="https://eric.ed.gov/?q=india&pg=2&id=EJ1170333"><span>Writing against Culture: Unveiling Education and Modernity for Hindu Indian and Muslim Pakistani Women through an "Ethnography of the Particular"</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Shah, Payal P.; Khurshid, Ayesha</p> <p>2018-01-01</p> <p>In this article, we analyze our experiences engaging in a collaborative ethnographic project. This project brings together two ethnographic studies undertaken independently from the other in <span class="hlt">Gujarat</span>, <span class="hlt">India</span> and Punjab, Pakistan. We integrate the narratives of young, rural Hindu women in <span class="hlt">India</span> with those of young, rural Muslim women in Pakistan to…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27418504','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27418504"><span>Connecting slow <span class="hlt">earthquakes</span> to huge <span class="hlt">earthquakes</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Obara, Kazushige; Kato, Aitaro</p> <p>2016-07-15</p> <p>Slow <span class="hlt">earthquakes</span> are characterized by a wide spectrum of fault slip behaviors and seismic radiation patterns that differ from those of traditional <span class="hlt">earthquakes</span>. However, slow <span class="hlt">earthquakes</span> and huge megathrust <span class="hlt">earthquakes</span> can have common slip mechanisms and are located in neighboring regions of the seismogenic zone. The frequent occurrence of slow <span class="hlt">earthquakes</span> may help to reveal the physics underlying megathrust events as useful analogs. Slow <span class="hlt">earthquakes</span> may function as stress meters because of their high sensitivity to stress changes in the seismogenic zone. Episodic stress transfer to megathrust source faults leads to an increased probability of triggering huge <span class="hlt">earthquakes</span> if the adjacent locked region is critically loaded. Careful and precise monitoring of slow <span class="hlt">earthquakes</span> may provide new information on the likelihood of impending huge <span class="hlt">earthquakes</span>. Copyright © 2016, American Association for the Advancement of Science.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27498498','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27498498"><span>Assessment of microbial quality of fish processing industrial effluent in bar-mouth at Bhidia landing site, Veraval, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sivaraman, G K; Visnuvinayagam, S; Jha, Ashish Kumar; Renuka, V; Remya, S; Vanik, Deesha</p> <p>2016-07-01</p> <p>The present study was carried out to assess the microbial quality of fish processing industries effluent at Bhidia bar-mouth, Veraval, <span class="hlt">Gujarat</span> during April, 2012 to March 2013. The total viable bacterial count (TVBC), total Enterobacteriaceae count, E. coli count (EC), Staphylococcus aureus and Fecal Streptococcal count in effluent ranged from 3.0 x 10(-1) to 6.8 x 10(6), 9.0 x 10(1) to 2.9 x 10(4), 0 to 0. 5 x 10(4), 0 to 0. 4 x 102 and 0.3 x 10(1) to 0. 1 x 10(4) cfu.(-1)respectively. Significantly higher load of TEC, E. coli, S.aureus, Fecal Streptococci, Total coliforms and Fecal coliforms were higher during summer whereas, TVBC was higher in the month of Sept.-Oct. Furthermore, the total coliform and fecal coliform counts were found to be higher with 1400+ /100 ml MPN value throughout the year of the study, except in the month of August. Overall occurrence of pathogenic strains of E. coli, S. aureus and Fecal streptococci were 41.67%, 25.00% and 66.67% respectively during this period. The antibiogram of the isolated E. coli isolates show that almost 50% were resistant to Cefazidime/Clavulanic acid (CAC), Amoxyclav (AMC), Ciprofloxacin (CIF) and Ampicillin (AMP). The present study indicated that the effluent of fish processing industry was heavily contaminated with E. coli, S. aureus and Fecal Streptococci which confirmed improper treatment of fish processing effluent. Moreover, the precedence of antibiotic resistant E. coli may pose threat to public health safety.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013PApGe.170.2139M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013PApGe.170.2139M"><span>A New Insight into Probabilistic Seismic Hazard Analysis for Central <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mandal, H. S.; Shukla, A. K.; Khan, P. K.; Mishra, O. P.</p> <p>2013-12-01</p> <p>The Son-Narmada-Tapti lineament and its surroundings of Central <span class="hlt">India</span> (CI) is the second most important tectonic regime following the converging margin along Himalayas-Myanmar-Andaman of the Indian sub-continent, which attracted several geoscientists to assess its seismic hazard potential. Our study area, a part of CI, is bounded between latitudes 18°-26°N and longitudes 73°-83°E, representing a stable part of Peninsular <span class="hlt">India</span>. Past damaging moderate magnitude <span class="hlt">earthquakes</span> as well as continuing microseismicity in the area provided enough data for seismological study. Our estimates based on regional Gutenberg-Richter relationship showed lower b values (i.e., between 0.68 and 0.76) from the average for the study area. The Probabilistic Seismic Hazard Analysis carried out over the area with a radius of ~300 km encircling Bhopal yielded a conspicuous relationship between <span class="hlt">earthquake</span> return period ( T) and peak ground acceleration (PGA). Analyses of T and PGA shows that PGA value at bedrock varies from 0.08 to 0.15 g for 10 % ( T = 475 years) and 2 % ( T = 2,475 years) probabilities exceeding 50 years, respectively. We establish the empirical relationships and between zero period acceleration (ZPA) and shear wave velocity up to a depth of 30 m [ V s (30)] for the two different return periods. These demonstrate that the ZPA values decrease with increasing shear wave velocity, suggesting a diagnostic indicator for designing the structures at a specific site of interest. The predictive designed response spectra generated at a site for periods up to 4.0 s at 10 and 2 % probability of exceedance of ground motion for 50 years can be used for designing duration dependent structures of variable vertical dimension. We infer that this concept of assimilating uniform hazard response spectra and predictive design at 10 and 2 % probability of exceedance in 50 years at 5 % damping at bedrocks of different categories may offer potential inputs for designing <span class="hlt">earthquake</span> resistant</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/945662','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/945662"><span>REGIONAL SEISMIC AMPLITUDE MODELING AND TOMOGRAPHY FOR <span class="hlt">EARTHQUAKE</span>-EXPLOSION DISCRIMINATION</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Walter, W R; Pasyanos, M E; Matzel, E</p> <p>2008-07-08</p> <p>We continue exploring methodologies to improve <span class="hlt">earthquake</span>-explosion discrimination using regional amplitude ratios such as P/S in a variety of frequency bands. Empirically we demonstrate that such ratios separate explosions from <span class="hlt">earthquakes</span> using closely located pairs of <span class="hlt">earthquakes</span> and explosions recorded on common, publicly available stations at test sites around the world (e.g. Nevada, Novaya Zemlya, Semipalatinsk, Lop Nor, <span class="hlt">India</span>, Pakistan, and North Korea). We are also examining if there is any relationship between the observed P/S and the point source variability revealed by longer period full waveform modeling (e. g. Ford et al 2008). For example, regional waveform modeling showsmore » strong tectonic release from the May 1998 <span class="hlt">India</span> test, in contrast with very little tectonic release in the October 2006 North Korea test, but the P/S discrimination behavior appears similar in both events using the limited regional data available. While regional amplitude ratios such as P/S can separate events in close proximity, it is also empirically well known that path effects can greatly distort observed amplitudes and make <span class="hlt">earthquakes</span> appear very explosion-like. Previously we have shown that the MDAC (Magnitude Distance Amplitude Correction, Walter and Taylor, 2001) technique can account for simple 1-D attenuation and geometrical spreading corrections, as well as magnitude and site effects. However in some regions 1-D path corrections are a poor approximation and we need to develop 2-D path corrections. Here we demonstrate a new 2-D attenuation tomography technique using the MDAC <span class="hlt">earthquake</span> source model applied to a set of events and stations in both the Middle East and the Yellow Sea Korean Peninsula regions. We believe this new 2-D MDAC tomography has the potential to greatly improve <span class="hlt">earthquake</span>-explosion discrimination, particularly in tectonically complex regions such as the Middle East. Monitoring the world for potential nuclear explosions requires characterizing</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED301522.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED301522.pdf"><span>Household Resources and Their Changing Relationships: Case Studies in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. International Agriculture Publications General Series Number 3.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Magrabi, Frances M., Ed.; Verma, Amita, Ed.</p> <p></p> <p>This publication contains case studies based on rural life in northern <span class="hlt">India</span>. The titles include: (1) "Profiles of Two Indian Rural Settings"; (2) "Visitors View a Village"; (3) "Village Households"; (4) "Agriculture"; (5) "Women's Needs: Health and Nutrition"; (6) "Meal Pattern, Nutrient…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-PIA03300.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-PIA03300.html"><span>SRTM Colored and Shaded Topography: Haro and Kas Hills, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2001-04-12</p> <p>On January 26, 2001, the Kachchh region in western <span class="hlt">India</span> suffered the most deadly <span class="hlt">earthquake</span> in <span class="hlt">India</span>'s history. This shaded topography view of landforms northeast of the city of Bhuj depicts geologic structures that are of interest in the study the tectonic processes that may have led to that <span class="hlt">earthquake</span>. However, preliminary field studies indicate that these structures are composed of Mesozoic rocks that are overlain by younger rocks showing little deformation. Thus these structures may be old, not actively growing, and not directly related to the recent <span class="hlt">earthquake</span>. The Haro Hills are on the left and the Kas Hills are on the right. The Haro Hills are an "anticline," which is an upwardly convex elongated fold of layered rocks. In this view, the anticline is distinctly ringed by an erosion resistant layer of sandstone. The east-west orientation of the anticline may relate to the crustal compression that has occurred during <span class="hlt">India</span>'s northward movement toward, and collision with, Asia. In contrast, the largest of the Kas Hills appears to be a tilted (to the south) and faulted (on the north) block of layered rocks. Also seen here, the linear feature trending toward the southwest from the image center is an erosion-resistant "dike," which is an igneous intrusion into older "host" rocks along a fault plane or other crack. These features are simple examples of how shaded topography can provide a direct input to geologic studies. In this image, colors show the elevation as measured by the Shuttle Radar Topography Mission (SRTM). Colors range from green at the lowest elevations, through yellow and red, to purple at the highest elevations. Elevations here range from near sea level to about 300 meters (about 1000 feet). Shading has been added, with illumination from the north (image top). http://photojournal.jpl.nasa.gov/catalog/PIA03300</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5719613','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5719613"><span>Sustained progress, but no room for complacency: Results of 2015 HIV estimations in <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Pandey, Arvind; Dhingra, Neeraj; Kumar, Pradeep; Sahu, Damodar; Reddy, D.C.S.; Narayan, Padum; Raj, Yujwal; Sangal, Bhavna; Chandra, Nalini; Nair, Saritha; Singh, Jitenkumar; Chavan, Laxmikant; Srivastava, Deepika Joshi; Jha, Ugra Mohan; Verma, Vinita; Kant, Shashi; Bhattacharya, Madhulekha; Swain, Pushpanjali; Haldar, Partha; Singh, Lucky; Bakkali, Taoufik; Stover, John; Ammassari, Savina</p> <p>2017-01-01</p> <p>Background & objectives: Evidence-based planning has been the cornerstone of <span class="hlt">India</span>'s response to HIV/AIDS. Here we describe the process, method and tools used for generating the 2015 HIV estimates and provide a summary of the main results. Methods: Spectrum software supported by the UNAIDS was used to produce HIV estimates for <span class="hlt">India</span> as a whole and its States/Union Territories. This tool takes into consideration the size and HIV prevalence of defined population groups and programme data to estimate HIV prevalence, incidence and mortality over time as well as treatment needs. Results: <span class="hlt">India</span>'s national adult prevalence of HIV was 0.26 per cent in 2015. Of the 2.1 million people living with HIV/AIDS, the largest numbers were in Andhra Pradesh, Maharashtra and Karnataka. New HIV infections were an estimated 86,000 in 2015, reflecting a decline by around 32 per cent from 2007. The declining trend in incidence was mirrored in most States, though an increasing trend was detected in Assam, Chandigarh, Chhattisgarh, <span class="hlt">Gujarat</span>, Sikkim, Tripura and Uttar Pradesh. AIDS-related deaths were estimated to be 67,600 in 2015, reflecting a 54 per cent decline from 2007. There were variations in the rate and trend of decline across <span class="hlt">India</span> for this indicator also. Interpretation & conclusions: While key indicators measured through Spectrum modelling confirm success of the National AIDS Control Programme, there is no room for complacency as rising incidence trends in some geographical areas and population pockets remain the cause of concern. Progress achieved so far in responding to HIV/AIDS needs to be sustained to end the HIV epidemic. PMID:29168464</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1987GMS....41..207S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1987GMS....41..207S"><span>New evidence for paleobiogeographic intercontinental Gondwana relationships based on Late Cretaceous-earliest Paleocene coastal faunas from peninsular <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sahni, Ashok; Rana, R. S.; Prasad, G. V. R.</p> <p></p> <p>A number of localities for freshwater microvertebrate assemblages of Late Cretaceous-early Paleocene age fringing the Deccan Basalt outcrops of Peninsular <span class="hlt">India</span> have been studied during the last 4 years. The diversified vertebrate assemblages recovered by bulk wet screening at the localities of Rahioli (<span class="hlt">Gujarat</span>), Jabalpur (Madhya Pradesh), Nagpur, Umrer, Pisdura (Maharashtra), and Asifabad (Andhra Pradesh) clearly suggest lack of faunal endemism for the drifting Indian island subcontinent. On the contrary, at the generic level, the fauna from the peninsular Indian localities is cosmopolitan in nature. The presence of a number of Laurasiatic elements, such as pelobatid frogs, suggests that a dispersal corridor was maintained with Laurasia throughout the drifting phase of <span class="hlt">India</span>. The coastal plain faunas contain a mixed assemblage of freshwater and marine forms represented by 62 genera and 79 species. There is a striking similarity at the generic level between the fish and turtle faunas of the Upper Cretaceous of Peninsular <span class="hlt">India</span> and those of Niger. Similarly, the few data now available from south central Bolivia, South America, also suggest interesting similarities to the corresponding faunas of Peninsular <span class="hlt">India</span>. The lack of faunal endemism in <span class="hlt">India</span> during the temporal span of <span class="hlt">India</span>'s northward drift as an island subcontinent can be attributed to a land contact maintained with Madagascar and the east African region by such aseismic elements as the Mascarene plateau and the Chagos-Laccadive Ridge. A more northerly contact with Laurasia may have been established by an island arc system represented at present by the Dras volcanics of Kashmir. The proximity of the Iran-Afghan plate to the drifting Indian landmass may have further contributed as a corridor for the dispersal of Laurasiatic elements into the subcontinent. By the middle Eocene, with the establishment of a firm dispersal corridor with central and east Asia, faunal affinities changed from Gondwanic to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/sir/2017/5013/sir20175013ah_v1.1.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/sir/2017/5013/sir20175013ah_v1.1.pdf"><span>The HayWired <span class="hlt">Earthquake</span> Scenario—<span class="hlt">Earthquake</span> Hazards</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Detweiler, Shane T.; Wein, Anne M.</p> <p>2017-04-24</p> <p>The HayWired scenario is a hypothetical <span class="hlt">earthquake</span> sequence that is being used to better understand hazards for the San Francisco Bay region during and after an <span class="hlt">earthquake</span> of magnitude 7 on the Hayward Fault. The 2014 Working Group on California <span class="hlt">Earthquake</span> Probabilities calculated that there is a 33-percent likelihood of a large (magnitude 6.7 or greater) <span class="hlt">earthquake</span> occurring on the Hayward Fault within three decades. A large Hayward Fault <span class="hlt">earthquake</span> will produce strong ground shaking, permanent displacement of the Earth’s surface, landslides, liquefaction (soils becoming liquid-like during shaking), and subsequent fault slip, known as afterslip, and <span class="hlt">earthquakes</span>, known as aftershocks. The most recent large <span class="hlt">earthquake</span> on the Hayward Fault occurred on October 21, 1868, and it ruptured the southern part of the fault. The 1868 magnitude-6.8 <span class="hlt">earthquake</span> occurred when the San Francisco Bay region had far fewer people, buildings, and infrastructure (roads, communication lines, and utilities) than it does today, yet the strong ground shaking from the <span class="hlt">earthquake</span> still caused significant building damage and loss of life. The next large Hayward Fault <span class="hlt">earthquake</span> is anticipated to affect thousands of structures and disrupt the lives of millions of people. <span class="hlt">Earthquake</span> risk in the San Francisco Bay region has been greatly reduced as a result of previous concerted efforts; for example, tens of billions of dollars of investment in strengthening infrastructure was motivated in large part by the 1989 magnitude 6.9 Loma Prieta <span class="hlt">earthquake</span>. To build on efforts to reduce <span class="hlt">earthquake</span> risk in the San Francisco Bay region, the HayWired <span class="hlt">earthquake</span> scenario comprehensively examines the <span class="hlt">earthquake</span> hazards to help provide the crucial scientific information that the San Francisco Bay region can use to prepare for the next large <span class="hlt">earthquake</span>, The HayWired <span class="hlt">Earthquake</span> Scenario—<span class="hlt">Earthquake</span> Hazards volume describes the strong ground shaking modeled in the scenario and the hazardous movements of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28235678','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28235678"><span>Kerosene-a toddler's sin: A five years study at tertiary care hospital in western <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Parekh, Utsav; Gupta, Sanjay</p> <p>2017-04-01</p> <p>Acute kerosene poisoning is a preventable health problem in children perceived mainly in developing countries. It influences socioeconomic and cultural status of country due to its contribution in morbidity and mortality. As kerosene is widely used as household energy source in <span class="hlt">India</span> at rural areas as well as urban, it accounts for significant number of poisoning cases mainly accidental in manner. As there are only handful studies from <span class="hlt">India</span> on kerosene poisoning in children, we planned this study to evaluate incidence of kerosene poisoning in Western Indian population and its clinico-epidemiotoxicological profile. In this retrospective cross-sectional study, we collected data of all the cases of kerosene poisoning diagnosed during five years from 2009 to 2013 at Shri Krishna hospital situated at Karamsad, <span class="hlt">Gujarat</span> state of Western <span class="hlt">India</span>. We observed among total 42 cases, all victims were under 3 years of age. Evening in summer months, rural areas, storage of kerosene in household containers, inadequate parental supervision and door-to-hospitalization period emerged as most serious associated factors. Fever, cough, vomiting, tachypnoea and leucocytosis were commonest manifestations while pneumonia was the most common complication. Signs of central nervous system involvement, leucocytosis and vomiting were significantly correlated with pneumonia. Deaths occurred due to pneumonia. Early diagnosis and treatment of pneumonia may reduce mortality and recommendations are made to reduce the incidence of kerosene poisoning. Copyright © 2017 Elsevier Ltd and Faculty of Forensic and Legal Medicine. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27385849','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27385849"><span>Prevalence of premenstrual syndrome and premenstrual dysphoric disorder among college students of Bhavnagar, <span class="hlt">Gujarat</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Raval, Chintan Madhusudan; Panchal, Bharat Navinchandra; Tiwari, Deepak Sachidanand; Vala, Ashok Ukabhai; Bhatt, Renish Bhupendrabhai</p> <p>2016-01-01</p> <p>Premenstrual dysphoric disorder (PMDD) is a severe form of premenstrual syndrome (PMS) characterized by mood changes, anxiety, and somatic symptoms experienced during the specific time of menstrual cycle. Prevalence data of PMS and PMDD is sparse among college girls in <span class="hlt">India</span>. The aim of this study is to study the prevalence of PMS and PMDD among college students of Bhavnagar (<span class="hlt">Gujarat</span>), its associated demographic and menstrual factors, to rank common symptoms and compare premenstrual symptom screening tool (PSST) with Structured Clinical Interview for DSM-IV-TR defined PMDD (SCID-PMDD) for sensitivity and specificity. A cross-sectional survey was done in five colleges of Bhavnagar. Of 529 subjects approached, 489 college girls were finally analyzed for sociodemographic data, menstrual history, and PSST. SCID-PMDD was applied among those who were positive on PSST and 20% of those who were negative. The data were analyzed using OpenEpi Version 2. Chi-square test was done for qualitative variables and analysis of variance for quantitative variables. Sensitivity, specificity, and predictive values were calculated for PSST. The prevalence of PMS was 18.4%. Moderate to severe PMS was 14.7% and PMDD was 3.7% according to DSM IV-TR and 91% according to International Classification of Diseases, 10(th) edition criteria. The symptoms commonly reported were "fatigue/lack of energy," "decrease interest in work," and "anger/irritability." The most common functional impairment item was "school/work efficiency and productivity." PSST has 90.9% sensitivity, 57.01% specificity, and 97.01% predictive value of negative test. Prevalence of PMS among college students is similar to other studies from Asia. PSST is a useful screening tool for PMS, and it should be confirmed by more specific tool as by SCID-PMDD. Routine screening with PSST can identify college girls who can improve with treatment.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70024458','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70024458"><span>The 26 January 2001 M 7.6 Bhuj, <span class="hlt">India</span>, <span class="hlt">earthquake</span>: Observed and predicted ground motions</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hough, S.E.; Martin, S.; Bilham, R.; Atkinson, G.M.</p> <p>2002-01-01</p> <p> the average effects. The discrepancy may also be partly attributable to the inadequacy of the empirical relationship between MMI and peak ground acceleration (PGA), when applied to <span class="hlt">India</span>. The MMI-PGA relationship was developed using data from California <span class="hlt">earthquakes</span>, which might have a systematically different stress drop and therefore, a different frequency content than intraplate events. When a relationship between response spectra and MMI is used, we obtain larger predicted MMI values, in better agreement with the observations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016PApGe.173.2653D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016PApGe.173.2653D"><span>Probabilistic Seismic Hazard Assessment for Northeast <span class="hlt">India</span> Region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Das, Ranjit; Sharma, M. L.; Wason, H. R.</p> <p>2016-08-01</p> <p>Northeast <span class="hlt">India</span> bounded by latitudes 20°-30°N and longitudes 87°-98°E is one of the most seismically active areas in the world. This region has experienced several moderate-to-large-sized <span class="hlt">earthquakes</span>, including the 12 June, 1897 Shillong <span class="hlt">earthquake</span> ( M w 8.1) and the 15 August, 1950 Assam <span class="hlt">earthquake</span> ( M w 8.7) which caused loss of human lives and significant damages to buildings highlighting the importance of seismic hazard assessment for the region. Probabilistic seismic hazard assessment of the region has been carried out using a unified moment magnitude catalog prepared by an improved General Orthogonal Regression methodology (Geophys J Int, 190:1091-1096, 2012; Probabilistic seismic hazard assessment of Northeast <span class="hlt">India</span> region, Ph.D. Thesis, Department of <span class="hlt">Earthquake</span> Engineering, IIT Roorkee, Roorkee, 2013) with events compiled from various databases (ISC, NEIC,GCMT, IMD) and other available catalogs. The study area has been subdivided into nine seismogenic source zones to account for local variation in tectonics and seismicity characteristics. The seismicity parameters are estimated for each of these source zones, which are input variables into seismic hazard estimation of a region. The seismic hazard analysis of the study region has been performed by dividing the area into grids of size 0.1° × 0.1°. Peak ground acceleration (PGA) and spectral acceleration ( S a) values (for periods of 0.2 and 1 s) have been evaluated at bedrock level corresponding to probability of exceedance (PE) of 50, 20, 10, 2 and 0.5 % in 50 years. These exceedance values correspond to return periods of 100, 225, 475, 2475, and 10,000 years, respectively. The seismic hazard maps have been prepared at the bedrock level, and it is observed that the seismic hazard estimates show a significant local variation in contrast to the uniform hazard value suggested by the Indian standard seismic code [Indian standard, criteria for <span class="hlt">earthquake</span>-resistant design of structures, fifth edition, Part</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_14 --> <div id="page_15" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="281"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMNH21A3830K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMNH21A3830K"><span>Influence of <span class="hlt">Earthquake</span> Parameters on Tsunami Wave Height and Inundation</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kulangara Madham Subrahmanian, D.; Sri Ganesh, J.; Venkata Ramana Murthy, M.; V, R. M.</p> <p>2014-12-01</p> <p>After Indian Ocean Tsunami (IOT) on 26th December, 2004, attempts are being made to assess the threat of tsunami originating from different sources for different parts of <span class="hlt">India</span>. The Andaman - Sumatra trench is segmented by transcurrent faults and differences in the rate of subduction which is low in the north and increases southward. Therefore key board model with initial deformation calculated using different strike directions, slip rates, are used. This results in uncertainties in the <span class="hlt">earthquake</span> parameters. This study is made to identify the location of origin of most destructive tsunami for Southeast coast of <span class="hlt">India</span> and to infer the influence of the <span class="hlt">earthquake</span> parameters in tsunami wave height travel time in deep ocean as well as in the shelf and inundation in the coast. Five tsunamigenic sources were considered in the Andaman - Sumatra trench taking into consideration the tectonic characters of the trench described by various authors and the modeling was carried out using TUNAMI N2 code. The model results were validated using the travel time and runup in the coastal areas and comparing the water elevation along Jason - 1's satellite track. The inundation results are compared from the field data. The assessment of the tsunami threat for the area south of Chennai city the metropolitan city of South <span class="hlt">India</span> shows that a tsunami originating in Car Nicobar segment of the Andaman - Sumatra subduction zone can generate the most destructive tsunami. Sensitivity analysis in the modelling indicates that fault length influences the results significantly and the tsunami reaches early and with higher amplitude. Strike angle is also modifying the tsunami followed by amount of slip.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ready.gov/earthquakes','NIH-MEDLINEPLUS'); return false;" href="https://www.ready.gov/earthquakes"><span><span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://medlineplus.gov/">MedlinePlus</a></p> <p></p> <p></p> <p>... Search Term(s): Main Content Home Be Informed <span class="hlt">Earthquakes</span> <span class="hlt">Earthquakes</span> An <span class="hlt">earthquake</span> is the sudden, rapid shaking of the earth, ... by the breaking and shifting of underground rock. <span class="hlt">Earthquakes</span> can cause buildings to collapse and cause heavy ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017Geomo.297....1B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Geomo.297....1B"><span>Sedimentology, geochemistry and OSL dating of the alluvial succession in the northern <span class="hlt">Gujarat</span> alluvial plain (western <span class="hlt">India</span>) - A record to evaluate the sensitivity of a semiarid fluvial system to the climatic and tectonic forcing since the late Marine Isotopic Stage 3</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bhattacharya, Falguni; Shukla, Anil D.; Patel, R. C.; Rastogi, B. K.; Juyal, Navin</p> <p>2017-11-01</p> <p>The alluvial successions in the northern <span class="hlt">Gujarat</span> alluvial plain (western <span class="hlt">India</span>) have been investigated for reconstructing the climatic fluctuations during the last 40 ka. Alluvial architecture and geochemical proxies indicate prevalence of a strengthened Indian Summer Monsoon (ISM) with fluctuations between the late Marine Isotopic Stage 3 (MIS 3; 37 ka) to the early MIS 2 (27 ka). A gradual onset of aridity (declining ISM) after 27 ka with peak aridity at 22 ka is observed. A gradual strengthening of ISM at around 18 and > 12 ka followed by a short reversal in ISM intensity between 12 and 11 ka, is attributed to the Younger-Dryas (YD) cooling event. The aeolian sand sheet dated to 6 and 3.5 ka represents the onset of regional aridity. Following this, a short-lived humid phase was observed after 2 ka, which includes the Medieval Warm Period (MWP). The study suggests that the variability in the ISM to the latitudinal migration of the Inter Tropical Convergence Zone was caused by insolation-driven cooling and warming events in the North Atlantic. The incision of the valley fill alluvium occurred in two distinct phases. The older incision phase occurred after 11 ka and before 6 ka, whereas the younger incision phase that led to the development of present day topography is bracketed between 3.5 ka and before 1 ka. The older incision phase is ascribed to the early to mid-Holocene enhanced ISM (climatically driven), whereas the younger incision seems to be modulated by the activation of basement faults (tectonically driven).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26487318','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26487318"><span>Bio-Mimetics of Disaster Anticipation-Learning Experience and Key-Challenges.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tributsch, Helmut</p> <p>2013-03-19</p> <p>Anomalies in animal behavior and meteorological phenomena before major <span class="hlt">earthquakes</span> have been reported throughout history. Bio-mimetics or bionics aims at learning disaster anticipation from animals. Since modern science is reluctant to address this problem an effort has been made to track down the knowledge available to ancient natural philosophers. Starting with an archaeologically documented human sacrifice around 1700 B.C. during the Minoan civilization immediately before a large <span class="hlt">earthquake</span>, which killed the participants, <span class="hlt">earthquake</span> prediction knowledge throughout antiquity is evaluated. Major practical experience with this phenomenon has been gained from a Chinese <span class="hlt">earthquake</span> prediction initiative nearly half a century ago. Some quakes, like that of Haicheng, were recognized in advance. However, the destructive Tangshan <span class="hlt">earthquake</span> was not predicted, which was interpreted as an inherent failure of prediction based on animal phenomena. This is contradicted on the basis of reliable Chinese documentation provided by the responsible <span class="hlt">earthquake</span> study commission. The Tangshan <span class="hlt">earthquake</span> was preceded by more than 2,000 reported animal anomalies, some of which were of very dramatic nature. They are discussed here. Any physical phenomenon, which may cause animal unrest, must involve energy turnover before the main <span class="hlt">earthquake</span> event. The final product, however, of any energy turnover is heat. Satellite based infrared measurements have indeed identified significant thermal anomalies before major <span class="hlt">earthquakes</span>. One of these cases, occurring during the 2001 Bhuj <span class="hlt">earthquake</span> in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, is analyzed together with parallel animal anomalies observed in the Gir national park. It is suggested that the time window is identical and that both phenomena have the same geophysical origin. It therefore remains to be demonstrated that energy can be released locally before major <span class="hlt">earthquake</span> events. It is shown that by considering appropriate geophysical feedback processes, this is</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20821893','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20821893"><span>Social capital and basic goods: the cautionary tale of drinking water in <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Motiram, Sripad; Osberg, Lars</p> <p>2010-01-01</p> <p>This study uses micro-data from the 1998-99 Indian Time Use Survey (ITUS; covering 77,593 persons in 18,591 households in <span class="hlt">Gujarat</span>, Tamil Nadu, Madhya Pradesh, Meghalaya, Orissa, and Haryana) to argue that time use data provides a natural metric for measuring "social capital" building activities and for distinguishing between the relative importance of "bonding" into groups or "bridging" within communities. The study examines the correlation between inequality in landownership, caste status, measures of local social capital, and whether or not a household will have to collect water. In <span class="hlt">India</span>, the probability that a rural household fetches water is 4.8% and 9.1% lower in communities in which the average time spent on social interaction and community-based activities at the district-level doubles, but it is 18.9% greater when the time in group-based activities doubles. Inequalities in landownership and home ownership are associated with considerably larger differences in local tap water availability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=earth+AND+quakes&id=EJ194839','ERIC'); return false;" href="https://eric.ed.gov/?q=earth+AND+quakes&id=EJ194839"><span><span class="hlt">Earthquakes</span>.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Walter, Edward J.</p> <p>1977-01-01</p> <p>Presents an analysis of the causes of <span class="hlt">earthquakes</span>. Topics discussed include (1) geological and seismological factors that determine the effect of a particular <span class="hlt">earthquake</span> on a given structure; (2) description of some large <span class="hlt">earthquakes</span> such as the San Francisco quake; and (3) prediction of <span class="hlt">earthquakes</span>. (HM)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED241329.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED241329.pdf"><span><span class="hlt">Earthquakes</span>.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Pakiser, Louis C.</p> <p></p> <p>One of a series of general interest publications on science topics, the booklet provides those interested in <span class="hlt">earthquakes</span> with an introduction to the subject. Following a section presenting an historical look at the world's major <span class="hlt">earthquakes</span>, the booklet discusses <span class="hlt">earthquake</span>-prone geographic areas, the nature and workings of <span class="hlt">earthquakes</span>, earthquake…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23778061','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23778061"><span>A cross-sectional, randomized cluster sample survey of household vulnerability to extreme heat among slum dwellers in ahmedabad, <span class="hlt">india</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tran, Kathy V; Azhar, Gulrez S; Nair, Rajesh; Knowlton, Kim; Jaiswal, Anjali; Sheffield, Perry; Mavalankar, Dileep; Hess, Jeremy</p> <p>2013-06-18</p> <p>Extreme heat is a significant public health concern in <span class="hlt">India</span>; extreme heat hazards are projected to increase in frequency and severity with climate change. Few of the factors driving population heat vulnerability are documented, though poverty is a presumed risk factor. To facilitate public health preparedness, an assessment of factors affecting vulnerability among slum dwellers was conducted in summer 2011 in Ahmedabad, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. Indicators of heat exposure, susceptibility to heat illness, and adaptive capacity, all of which feed into heat vulnerability, was assessed through a cross-sectional household survey using randomized multistage cluster sampling. Associations between heat-related morbidity and vulnerability factors were identified using multivariate logistic regression with generalized estimating equations to account for clustering effects. Age, preexisting medical conditions, work location, and access to health information and resources were associated with self-reported heat illness. Several of these variables were unique to this study. As sociodemographics, occupational heat exposure, and access to resources were shown to increase vulnerability, future interventions (e.g., health education) might target specific populations among Ahmedabad urban slum dwellers to reduce vulnerability to extreme heat. Surveillance and evaluations of future interventions may also be worthwhile.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018IJEaS.107..191J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018IJEaS.107..191J"><span>Subsurface profiling of granite pluton using microtremor method: southern Aravalli, <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Joshi, Aditya U.; Sant, Dhananjay A.; Parvez, Imtiyaz A.; Rangarajan, Govindan; Limaye, Manoj A.; Mukherjee, Soumyajit; Charola, Mitesh J.; Bhatt, Meghnath N.; Mistry, Sagar P.</p> <p>2018-01-01</p> <p>We report, using the microtremor method, a subsurface granitic pluton underneath the Narukot Dome and in its western extension along a WNW profile, in proximity of eastern fringe of Cambay Rift, <span class="hlt">India</span>. The dome and its extension is a part of the Champaner Group of rocks belonging to the Mesoproterozoic Aravalli Supergroup. The present finding elucidates development of an asymmetric double plunge along Narukot Dome. Microtremor measurements at 32 sites were carried out along the axial trace (N95°) of the dome. Fourier amplitude spectral studies were applied to obtain the ratio between the horizontal and vertical components of persisting Rayleigh waves as local ambient noise. Fundamental resonant frequencies with amplitude ≥1-sigma for each site are considered to distinguish rheological boundary. Two distinct rheological boundaries are identified based on frequency ranges determined in the terrain: (1) 0.2219-10.364 Hz recorded at 31 stations identified as the Champaner metasediment and granite boundary, and (2) 10.902-27.1119 Hz recorded at 22 stations identified as the phyllite and quartzite boundary. The proposed equation describing frequency-depth relationship between granite and overlaying regolith matches with those already published in the literature. The morphology of granite pluton highlights the rootless character of Champaner Group showing sharp discordance with granitic pluton. The findings of manifestation of pluton at a shallower depth imply a steep easterly plunge within the Champaner metasediments, whereas signature of pluton at a deeper level implies a gentle westerly plunge. The present method enables to assess how granite emplacement influences the surface structure.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JSeis..21.1001A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JSeis..21.1001A"><span>Empirical models for the prediction of ground motion duration for intraplate <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Anbazhagan, P.; Neaz Sheikh, M.; Bajaj, Ketan; Mariya Dayana, P. J.; Madhura, H.; Reddy, G. R.</p> <p>2017-07-01</p> <p>Many empirical relationships for the <span class="hlt">earthquake</span> ground motion duration were developed for interplate region, whereas only a very limited number of empirical relationships exist for intraplate region. Also, the existing relationships were developed based mostly on the scaled recorded interplate <span class="hlt">earthquakes</span> to represent intraplate <span class="hlt">earthquakes</span>. To the author's knowledge, none of the existing relationships for the intraplate regions were developed using only the data from intraplate regions. Therefore, an attempt is made in this study to develop empirical predictive relationships of <span class="hlt">earthquake</span> ground motion duration (i.e., significant and bracketed) with <span class="hlt">earthquake</span> magnitude, hypocentral distance, and site conditions (i.e., rock and soil sites) using the data compiled from intraplate regions of Canada, Australia, Peninsular <span class="hlt">India</span>, and the central and southern parts of the USA. The compiled <span class="hlt">earthquake</span> ground motion data consists of 600 records with moment magnitudes ranging from 3.0 to 6.5 and hypocentral distances ranging from 4 to 1000 km. The non-linear mixed-effect (NLMEs) and logistic regression techniques (to account for zero duration) were used to fit predictive models to the duration data. The bracketed duration was found to be decreased with an increase in the hypocentral distance and increased with an increase in the magnitude of the <span class="hlt">earthquake</span>. The significant duration was found to be increased with the increase in the magnitude and hypocentral distance of the <span class="hlt">earthquake</span>. Both significant and bracketed durations were predicted higher in rock sites than in soil sites. The predictive relationships developed herein are compared with the existing relationships for interplate and intraplate regions. The developed relationship for bracketed duration predicts lower durations for rock and soil sites. However, the developed relationship for a significant duration predicts lower durations up to a certain distance and thereafter predicts higher durations compared to the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/20995674-evaluation-numerical-simulation-tsunami-coastal-nuclear-power-plants-india','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/20995674-evaluation-numerical-simulation-tsunami-coastal-nuclear-power-plants-india"><span>Evaluation and Numerical Simulation of Tsunami for Coastal Nuclear Power Plants of <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Sharma, Pavan K.; Singh, R.K.; Ghosh, A.K.</p> <p>2006-07-01</p> <p>Recent tsunami generated on December 26, 2004 due to Sumatra <span class="hlt">earthquake</span> of magnitude 9.3 resulted in inundation at the various coastal sites of <span class="hlt">India</span>. The site selection and design of Indian nuclear power plants demand the evaluation of run up and the structural barriers for the coastal plants: Besides it is also desirable to evaluate the early warning system for tsunami-genic <span class="hlt">earthquakes</span>. The tsunamis originate from submarine faults, underwater volcanic activities, sub-aerial landslides impinging on the sea and submarine landslides. In case of a submarine <span class="hlt">earthquake</span>-induced tsunami the wave is generated in the fluid domain due to displacement of themore » seabed. There are three phases of tsunami: generation, propagation, and run-up. Reactor Safety Division (RSD) of Bhabha Atomic Research Centre (BARC), Trombay has initiated computational simulation for all the three phases of tsunami source generation, its propagation and finally run up evaluation for the protection of public life, property and various industrial infrastructures located on the coastal regions of <span class="hlt">India</span>. These studies could be effectively utilized for design and implementation of early warning system for coastal region of the country apart from catering to the needs of Indian nuclear installations. This paper presents some results of tsunami waves based on different analytical/numerical approaches with shallow water wave theory. (authors)« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012JSeis..16..345H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012JSeis..16..345H"><span>Stochastic ground-motion simulation of two Himalayan <span class="hlt">earthquakes</span>: seismic hazard assessment perspective</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Harbindu, Ashish; Sharma, Mukat Lal; Kamal</p> <p>2012-04-01</p> <p>The <span class="hlt">earthquakes</span> in Uttarkashi (October 20, 1991, M w 6.8) and Chamoli (March 8, 1999, M w 6.4) are among the recent well-documented <span class="hlt">earthquakes</span> that occurred in the Garhwal region of <span class="hlt">India</span> and that caused extensive damage as well as loss of life. Using strong-motion data of these two <span class="hlt">earthquakes</span>, we estimate their source, path, and site parameters. The quality factor ( Q β ) as a function of frequency is derived as Q β ( f) = 140 f 1.018. The site amplification functions are evaluated using the horizontal-to-vertical spectral ratio technique. The ground motions of the Uttarkashi and Chamoli <span class="hlt">earthquakes</span> are simulated using the stochastic method of Boore (Bull Seismol Soc Am 73:1865-1894, 1983). The estimated source, path, and site parameters are used as input for the simulation. The simulated time histories are generated for a few stations and compared with the observed data. The simulated response spectra at 5% damping are in fair agreement with the observed response spectra for most of the stations over a wide range of frequencies. Residual trends closely match the observed and simulated response spectra. The synthetic data are in rough agreement with the ground-motion attenuation equation available for the Himalayas (Sharma, Bull Seismol Soc Am 98:1063-1069, 1998).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AGUFM.S51C0170K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AGUFM.S51C0170K"><span>The 2004 Parkfield, CA <span class="hlt">Earthquake</span>: A Teachable Moment for Exploring <span class="hlt">Earthquake</span> Processes, Probability, and <span class="hlt">Earthquake</span> Prediction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kafka, A.; Barnett, M.; Ebel, J.; Bellegarde, H.; Campbell, L.</p> <p>2004-12-01</p> <p>The occurrence of the 2004 Parkfield <span class="hlt">earthquake</span> provided a unique "teachable moment" for students in our science course for teacher education majors. The course uses seismology as a medium for teaching a wide variety of science topics appropriate for future teachers. The 2004 Parkfield <span class="hlt">earthquake</span> occurred just 15 minutes after our students completed a lab on <span class="hlt">earthquake</span> processes and <span class="hlt">earthquake</span> prediction. That lab included a discussion of the Parkfield <span class="hlt">Earthquake</span> Prediction Experiment as a motivation for the exercises they were working on that day. Furthermore, this <span class="hlt">earthquake</span> was recorded on an AS1 seismograph right in their lab, just minutes after the students left. About an hour after we recorded the <span class="hlt">earthquake</span>, the students were able to see their own seismogram of the event in the lecture part of the course, which provided an excellent teachable moment for a lecture/discussion on how the occurrence of the 2004 Parkfield <span class="hlt">earthquake</span> might affect seismologists' ideas about <span class="hlt">earthquake</span> prediction. The specific lab exercise that the students were working on just before we recorded this <span class="hlt">earthquake</span> was a "sliding block" experiment that simulates <span class="hlt">earthquakes</span> in the classroom. The experimental apparatus includes a flat board on top of which are blocks of wood attached to a bungee cord and a string wrapped around a hand crank. Plate motion is modeled by slowly turning the crank, and <span class="hlt">earthquakes</span> are modeled as events in which the block slips ("blockquakes"). We scaled the <span class="hlt">earthquake</span> data and the blockquake data (using how much the string moved as a proxy for time) so that we could compare blockquakes and <span class="hlt">earthquakes</span>. This provided an opportunity to use interevent-time histograms to teach about <span class="hlt">earthquake</span> processes, probability, and <span class="hlt">earthquake</span> prediction, and to compare <span class="hlt">earthquake</span> sequences with blockquake sequences. We were able to show the students, using data obtained directly from their own lab, how global <span class="hlt">earthquake</span> data fit a Poisson exponential distribution better</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18403792','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18403792"><span>Commitment among state health officials & its implications for health sector reform: lessons from <span class="hlt">Gujarat</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Maheshwari, Sunil; Bhat, Ramesh; Saha, Somen</p> <p>2008-02-01</p> <p>Commitment, competencies and skills of people working in the health sector can significantly impact the performance and its reform process. In this study we attempted to analyse the commitment of state health officials and its implications for human resource practices in <span class="hlt">Gujarat</span>. A self-administered questionnaire was used to measure commitment and its relationship with human resource (HR) variables. Employee's organizational commitment (OC) and professional commitment (PC) were measured using OC and PC scale. Fifty five medical officers from <span class="hlt">Gujarat</span> participated in the study. Professional commitment of doctors (3.21 to 4.01) was found to be higher than their commitment to the organization (3.01 to 3.61). Doctors did not perceive greater fairness in the system on promotion (on the scale of 5, score: 2.55) and were of the view that the system still followed seniority based promotion (score: 3.42). Medical officers were upset about low autonomy in the department with regard to reward and recognition, accounting procedure, prioritization and synchronization of health programme and other administrative activities. Our study provided some support for positive effects of progressive HR practices on OC, specifically on affective and normative OC. Following initiatives were identified to foster a development climate among the health officials: providing opportunities for training, professional competency development, developing healthy relationship between superiors and subordinates, providing useful performance feedback, and recognising and rewarding performance. For reform process in the health sector to succeed, there is a need to promote high involvement of medical officers. There is a need to invest in developing leadership quality, supervision skills and developing autonomy in its public health institutions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.T11A1765D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.T11A1765D"><span>Three dimensional surface slip partitioning of the Sichuan <span class="hlt">earthquake</span> from Synthetic Aperture Radar</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>de Michele, M.; Raucoules, D.; de Sigoyer, J.; Pubellier, M.; Lasserre, C.; Pathier, E.; Klinger, Y.; van der Woerd, J.</p> <p>2009-12-01</p> <p>The Sichuan <span class="hlt">earthquake</span>, Mw 7.9, struck the Longmen Shan range front, in the western Sichuan province, China, on 12 May 2008. It severely affected an area where little historical seismicity and little or no significant active shortening were reported before the <span class="hlt">earthquake</span> (e.g. Gu et al., 1989; Chen et al., 1994; Gan et al., 2007). The Longmen Shan thrust system bounds the eastern margin of the Tibetan plateau and is considered as a transpressive zone since Triassic time that was reactivated during the <span class="hlt">India</span>-Asia collision (e.g., Tapponnier and Molnar, 1977, Chen and Wilson 1996; Arne et al., 1997, Godard et al., 2009). However, contrasting geological evidences of sparse thrusting and marked dextral strike-slip faulting during the Quaternary along with high topography (Burchfiel et al., 1995; Densmore et al., 2007) have led to models of dynamically driven and sustained topography (Royden et al., 1997) limiting the role of <span class="hlt">earthquakes</span> in relief building and leaving the mechanism of long term strain distribution in this area as an open question. Here we combine C and L band Synthetic Aperture Radar (SAR) offsets data from ascending and descending paths to retrieve the three dimensional surface slips distribution all along the <span class="hlt">earthquake</span> ruptures of the Sichuan <span class="hlt">earthquake</span>. We show a quantitative assessment of the amount of co-seismic slip and its partitioning at the surface.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/18420','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/18420"><span>Decarbonisation strategies : how much, how, where and who pays for [delta] [less than or equal-to] 2* Celsius?</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2010-03-01</p> <p>This paper was written for the conference presidential address delivered on January 23 2010 at the 40th Annual : Meeting of the <span class="hlt">Gujarat</span> Economic Association in Kim (Surat District), <span class="hlt">India</span>. The paper has been motivated primarily to outline and : delve...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://medlineplus.gov/earthquakes.html','NIH-MEDLINEPLUS'); return false;" href="https://medlineplus.gov/earthquakes.html"><span><span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://medlineplus.gov/">MedlinePlus</a></p> <p></p> <p></p> <p>An <span class="hlt">earthquake</span> happens when two blocks of the earth suddenly slip past one another. <span class="hlt">Earthquakes</span> strike suddenly, violently, and without warning at any time of the day or night. If an <span class="hlt">earthquake</span> occurs in a populated area, it may cause ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70144681','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70144681"><span>The 21 May 2014 Mw 5.9 Bay of Bengal <span class="hlt">earthquake</span>: macroseismic data suggest a high‐stress‐drop event</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Martin, Stacey; Hough, Susan E.</p> <p>2015-01-01</p> <p>A modest but noteworthy Mw 5.9 <span class="hlt">earthquake</span> occurred in the Bay of Bengal beneath the central Bengal fan at 21:51 Indian Standard Time (16:21 UTC) on 21 May 2014. Centered over 300 km from the eastern coastline of <span class="hlt">India</span> (Fig. 1), it caused modest damage by virtue of its location and magnitude. However, shaking was very widely felt in parts of eastern <span class="hlt">India</span> where <span class="hlt">earthquakes</span> are uncommon. Media outlets reported as many as four fatalities. Although most deaths were blamed on heart attacks, the death of one woman was attributed by different sources to either a roof collapse or a stampede (see Table S1, available in the electronic supplement to this article). Across the state of Odisha, as many as 250 people were injured (see Table S1), most after jumping from balconies or terraces. Light damage was reported from a number of towns on coastal deltaic sediments, including collapsed walls and damage to pukka and thatched dwellings. Shaking was felt well inland into east‐central <span class="hlt">India</span> and was perceptible in multistoried buildings as far as Chennai, Delhi, and Jaipur at distances of ≈1600  km (Table 1).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25329274','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25329274"><span>Probing the phylogenetic relationships of a few newly recorded intertidal zoanthids of <span class="hlt">Gujarat</span> coast (<span class="hlt">India</span>) with mtDNA COI sequences.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Joseph, Sneha; Poriya, Paresh; Kundu, Rahul</p> <p>2016-11-01</p> <p>The present study reports the phylogenetic relationship of six zoanthid species belonging to three genera, Isaurus, Palythoa, and Zoanthus identified using systematic computational analysis of mtDNA gene sequences. All six species are first recorded from the coasts of Kathiawar Peninsula, <span class="hlt">India</span>. Genus: Isaurus is represented by Isaurus tuberculatus, genus Zoanthus is represented by Zoanthus kuroshio and Zoanthus sansibaricus, while genus Palythoa is represented by Palythoa tuberculosa, P. sp. JVK-2006 and Palythoa heliodiscus. Results of the present study revealed that among the various species observed along the coastline, a minimum of 99% sequence divergence and a maximum of 96% sequence divergence were seen. An interspecific divergence of 1-4% and negligible intraspecific divergence was observed. These results not only highlighted the efficiency of the COI gene region in species identification but also demonstrated the genetic variability of zoanthids along the Saurashtra coastline of the west coast of <span class="hlt">India</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4919960','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4919960"><span>Prevalence of premenstrual syndrome and premenstrual dysphoric disorder among college students of Bhavnagar, <span class="hlt">Gujarat</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Raval, Chintan Madhusudan; Panchal, Bharat Navinchandra; Tiwari, Deepak Sachidanand; Vala, Ashok Ukabhai; Bhatt, Renish Bhupendrabhai</p> <p>2016-01-01</p> <p>Background: Premenstrual dysphoric disorder (PMDD) is a severe form of premenstrual syndrome (PMS) characterized by mood changes, anxiety, and somatic symptoms experienced during the specific time of menstrual cycle. Prevalence data of PMS and PMDD is sparse among college girls in <span class="hlt">India</span>. Aims: The aim of this study is to study the prevalence of PMS and PMDD among college students of Bhavnagar (<span class="hlt">Gujarat</span>), its associated demographic and menstrual factors, to rank common symptoms and compare premenstrual symptom screening tool (PSST) with Structured Clinical Interview for DSM-IV-TR defined PMDD (SCID-PMDD) for sensitivity and specificity. Materials and Methods: A cross-sectional survey was done in five colleges of Bhavnagar. Of 529 subjects approached, 489 college girls were finally analyzed for sociodemographic data, menstrual history, and PSST. SCID-PMDD was applied among those who were positive on PSST and 20% of those who were negative. The data were analyzed using OpenEpi Version 2. Chi-square test was done for qualitative variables and analysis of variance for quantitative variables. Sensitivity, specificity, and predictive values were calculated for PSST. Results: The prevalence of PMS was 18.4%. Moderate to severe PMS was 14.7% and PMDD was 3.7% according to DSM IV-TR and 91% according to International Classification of Diseases, 10th edition criteria. The symptoms commonly reported were “fatigue/lack of energy,” “decrease interest in work,” and “anger/irritability.” The most common functional impairment item was “school/work efficiency and productivity.” PSST has 90.9% sensitivity, 57.01% specificity, and 97.01% predictive value of negative test. Conclusion: Prevalence of PMS among college students is similar to other studies from Asia. PSST is a useful screening tool for PMS, and it should be confirmed by more specific tool as by SCID-PMDD. Routine screening with PSST can identify college girls who can improve with treatment. PMID:27385849</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_15 --> <div id="page_16" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="301"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29270160','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29270160"><span>Antibacterial and Antioxidant Activities of Novel Actinobacteria Strain Isolated from Gulf of Khambhat, <span class="hlt">Gujarat</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dholakiya, Riddhi N; Kumar, Raghawendra; Mishra, Avinash; Mody, Kalpana H; Jha, Bhavanath</p> <p>2017-01-01</p> <p>Bacterial secondary metabolites possess a wide range of biologically active compounds including antibacterial and antioxidants. In this study, a Gram-positive novel marine Actinobacteria was isolated from sea sediment which showed 84% 16S rRNA gene sequence (KT588655) similarity with Streptomyces variabilis (EU841661) and designated as Streptomyces variabilis RD-5. The genus Streptomyces is considered as a promising source of bioactive secondary metabolites. The isolated novel bacterial strain was characterized by antibacterial characteristics and antioxidant activities. The BIOLOG based analysis suggested that S. variabilis RD-5 utilized a wide range of substrates compared to the reference strain. The result is further supported by statistical analysis such as AWCD (average well color development), heat-map and PCA (principal component analysis). The whole cell fatty acid profiling showed the dominance of iso/anteiso branched C15-C17 long chain fatty acids. The identified strain S. variabilis RD-5 exhibited a broad spectrum of antibacterial activities for the Gram-negative bacteria ( Escherichia coli NCIM 2065, Shigella boydii NCIM, Klebsiella pneumoniae, Enterobacter cloacae, Pseudomonas sp. NCIM 2200 and Salmonella enteritidis NCIM), and Gram-positive bacteria ( Bacillus subtilis NCIM 2920 and Staphylococcus aureus MTCC 96). Extract of S. variabilis strain RD-5 showed 82.86 and 89% of 2,2-diphenyl-1-picrylhydrazyl (DPPH) free radical scavenging and metal chelating activity, respectively, at 5.0 mg/mL. While H 2 O 2 scavenging activity was 74.5% at 0.05 mg/mL concentration. Furthermore, polyketide synthases (PKSs types I and II), an enzyme complex that produces polyketides, the encoding gene(s) detected in the strain RD-5 which may probably involve for the synthesis of antibacterial compound(s). In conclusion, a novel bacterial strain of Actinobacteria , isolated from the unexplored sea sediment of Alang, Gulf of Khambhat (<span class="hlt">Gujarat</span>), <span class="hlt">India</span> showed promising</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5725476','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5725476"><span>Antibacterial and Antioxidant Activities of Novel Actinobacteria Strain Isolated from Gulf of Khambhat, <span class="hlt">Gujarat</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Dholakiya, Riddhi N.; Kumar, Raghawendra; Mishra, Avinash; Mody, Kalpana H.; Jha, Bhavanath</p> <p>2017-01-01</p> <p>Bacterial secondary metabolites possess a wide range of biologically active compounds including antibacterial and antioxidants. In this study, a Gram-positive novel marine Actinobacteria was isolated from sea sediment which showed 84% 16S rRNA gene sequence (KT588655) similarity with Streptomyces variabilis (EU841661) and designated as Streptomyces variabilis RD-5. The genus Streptomyces is considered as a promising source of bioactive secondary metabolites. The isolated novel bacterial strain was characterized by antibacterial characteristics and antioxidant activities. The BIOLOG based analysis suggested that S. variabilis RD-5 utilized a wide range of substrates compared to the reference strain. The result is further supported by statistical analysis such as AWCD (average well color development), heat-map and PCA (principal component analysis). The whole cell fatty acid profiling showed the dominance of iso/anteiso branched C15–C17 long chain fatty acids. The identified strain S. variabilis RD-5 exhibited a broad spectrum of antibacterial activities for the Gram-negative bacteria (Escherichia coli NCIM 2065, Shigella boydii NCIM, Klebsiella pneumoniae, Enterobacter cloacae, Pseudomonas sp. NCIM 2200 and Salmonella enteritidis NCIM), and Gram-positive bacteria (Bacillus subtilis NCIM 2920 and Staphylococcus aureus MTCC 96). Extract of S. variabilis strain RD-5 showed 82.86 and 89% of 2,2-diphenyl-1-picrylhydrazyl (DPPH) free radical scavenging and metal chelating activity, respectively, at 5.0 mg/mL. While H2O2 scavenging activity was 74.5% at 0.05 mg/mL concentration. Furthermore, polyketide synthases (PKSs types I and II), an enzyme complex that produces polyketides, the encoding gene(s) detected in the strain RD-5 which may probably involve for the synthesis of antibacterial compound(s). In conclusion, a novel bacterial strain of Actinobacteria, isolated from the unexplored sea sediment of Alang, Gulf of Khambhat (<span class="hlt">Gujarat</span>), <span class="hlt">India</span> showed promising</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19636478','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19636478"><span>Behavioral emergencies in <span class="hlt">India</span>: a population based epidemiological study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Saddichha, Sahoo; Vibha, Pandey; Saxena, Mukul Kumar; Methuku, Mithilesh</p> <p>2010-05-01</p> <p>Behavioral emergencies constitute an important but neglected part of emergencies seen worldwide in both emergency departments and by emergency services. Yet research on behavioral emergencies in <span class="hlt">India</span> has been scarce. The study aimed to evaluate the occurrence of acute behavioral problems as an emergency attended by our emergency management service-108 services. During the period of August 1st 2007-July 31st 2008, all behavioral emergencies presenting to our emergency services in the states of <span class="hlt">Gujarat</span> and Andhra Pradesh, which together account for more than 15% of <span class="hlt">India</span>'s population, were reviewed for data completeness and validity. Key word analysis of recorded case details was carried out to determine cause of emergency. Survival to hospital and 48-h outcome was also evaluated to study risk factors for mortality. A total of 40,541 cases of behavioral emergencies were recorded, in which the male:female ratio was 1.3:1. Most victims were in the 20 and 30 years (42%), from a poor socio-economic background (93%), rural area (74.3%), and backward caste (42.6%). Suicidal attempts, whether in the form of poisoning (60.5%) or otherwise (30.7%) was the most common emergency, followed by acute psychiatric causes (4%) and alcohol intoxication (3%). Victims, who met a fatal outcome, were more likely to be male (p = 0.02), having a better socio-economic condition (p < 0.001) and older (p < 0.001). Suicidal attempts, which form the largest chunk of behavioral emergencies, need to be tackled on a war-footing, given the sensitivity it deserves. Acute psychiatric emergencies, which form about 9% of all emergencies, require the emerging role of emergency psychiatric services.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ThApC.tmp...86S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ThApC.tmp...86S"><span>Recent trends in rainfall and temperature over North West <span class="hlt">India</span> during 1871-2016</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Saxena, Rani; Mathur, Prasoon</p> <p>2018-03-01</p> <p>Rainfall and temperature are the most important environmental factors influencing crop growth, development, and yield. The northwestern (NW) part of <span class="hlt">India</span> is one of the main regions of food grain production of the country. It comprises of six meteorological subdivisions (Haryana, Punjab, West Rajasthan, East Rajasthan, <span class="hlt">Gujarat</span> and Saurashtra, Kutch and Diu). In this study, attempts were made to study variability and trends in rainfall and temperature during 30-year climate normal periods (CN) and 10-year decadal excess or deficit rainfall frequency during the historical period from 1871 to 2016. The Mann-Kendall and Spearman's rank correlation (Spearman's rho) tests were used to determine significance of trends. Least square linear fitting method was adopted to find out the slopes of the trend lines. The long-term mean annual rainfall over North West <span class="hlt">India</span> is 587.7 mm (standard deviation of 153.0 mm and coefficient of variation 26.0). There was increasing trend in minimum and maximum temperatures during post monsoon season in entire study period and current climate normal period (1991-2016) due to which the sowing of rabi season crops may be delayed and there may be germination problem too. There was a non-significant decreasing trend in rainfall during monsoon season and an increasing trend in rainfall during post monsoon over North West <span class="hlt">India</span> during entire study period. During current CN5 (1991-2016), all the subdivision (except the Saurashtra region) showed a decreasing trend in rainfall during monsoon season which is a matter of concern for kharif crops and those rabi crops which are grown as rainfed on conserved soil moisture. The decadal annual and seasonal frequencies of excess and deficit years results revealed that the annual total deficit rainfall years (24) exceeded total excess rainfall years (22) in North West <span class="hlt">India</span> during the entire study period. While during the current decadal period (2011 to 2016), single year was the excess year and 2 years were</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.S14B..07B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.S14B..07B"><span>The 1868 Hayward <span class="hlt">Earthquake</span> Alliance: A Case Study - Using an <span class="hlt">Earthquake</span> Anniversary to Promote <span class="hlt">Earthquake</span> Preparedness</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brocher, T. M.; Garcia, S.; Aagaard, B. T.; Boatwright, J. J.; Dawson, T.; Hellweg, M.; Knudsen, K. L.; Perkins, J.; Schwartz, D. P.; Stoffer, P. W.; Zoback, M.</p> <p>2008-12-01</p> <p>Last October 21st marked the 140th anniversary of the M6.8 1868 Hayward <span class="hlt">Earthquake</span>, the last damaging <span class="hlt">earthquake</span> on the southern Hayward Fault. This anniversary was used to help publicize the seismic hazards associated with the fault because: (1) the past five such <span class="hlt">earthquakes</span> on the Hayward Fault occurred about 140 years apart on average, and (2) the Hayward-Rodgers Creek Fault system is the most likely (with a 31 percent probability) fault in the Bay Area to produce a M6.7 or greater <span class="hlt">earthquake</span> in the next 30 years. To promote <span class="hlt">earthquake</span> awareness and preparedness, over 140 public and private agencies and companies and many individual joined the public-private nonprofit 1868 Hayward <span class="hlt">Earthquake</span> Alliance (1868alliance.org). The Alliance sponsored many activities including a public commemoration at Mission San Jose in Fremont, which survived the 1868 <span class="hlt">earthquake</span>. This event was followed by an <span class="hlt">earthquake</span> drill at Bay Area schools involving more than 70,000 students. The anniversary prompted the Silver Sentinel, an <span class="hlt">earthquake</span> response exercise based on the scenario of an <span class="hlt">earthquake</span> on the Hayward Fault conducted by Bay Area County Offices of Emergency Services. 60 other public and private agencies also participated in this exercise. The California Seismic Safety Commission and KPIX (CBS affiliate) produced professional videos designed forschool classrooms promoting Drop, Cover, and Hold On. Starting in October 2007, the Alliance and the U.S. Geological Survey held a sequence of press conferences to announce the release of new research on the Hayward Fault as well as new loss estimates for a Hayward Fault <span class="hlt">earthquake</span>. These included: (1) a ShakeMap for the 1868 Hayward <span class="hlt">earthquake</span>, (2) a report by the U. S. Bureau of Labor Statistics forecasting the number of employees, employers, and wages predicted to be within areas most strongly shaken by a Hayward Fault <span class="hlt">earthquake</span>, (3) new estimates of the losses associated with a Hayward Fault <span class="hlt">earthquake</span>, (4) new ground motion</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1038308','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1038308"><span>Market-Based Indian Grid Integration Study Options: Preprint</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Stoltenberg, B.; Clark, K.; Negi, S. K.</p> <p>2012-03-01</p> <p>The Indian state of <span class="hlt">Gujarat</span> is forecasting solar and wind generation expansion from 16% to 32% of installed generation capacity by 2015. Some states in <span class="hlt">India</span> are already experiencing heavy wind power curtailment. Understanding how to integrate variable generation (VG) into the grid is of great interest to local transmission companies and <span class="hlt">India</span>'s Ministry of New and Renewable Energy. This paper describes the nature of a market-based integration study and how this approach, while new to Indian grid operation and planning, is necessary to understand how to operate and expand the grid to best accommodate the expansion of VG. Second,more » it discusses options in defining a study's scope, such as data granularity, generation modeling, and geographic scope. The paper also explores how <span class="hlt">Gujarat</span>'s method of grid operation and current system reliability will affect how an integration study can be performed.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.S43D2840S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.S43D2840S"><span>Predicted Attenuation Relation and Observed Ground Motion of Gorkha Nepal <span class="hlt">Earthquake</span> of 25 April 2015</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Singh, R. P.; Ahmad, R.</p> <p>2015-12-01</p> <p>A comparison of recent observed ground motion parameters of recent Gorkha Nepal <span class="hlt">earthquake</span> of 25 April 2015 (Mw 7.8) with the predicted ground motion parameters using exitsing attenuation relation of the Himalayan region will be presented. The recent <span class="hlt">earthquake</span> took about 8000 lives and destroyed thousands of poor quality of buildings and the <span class="hlt">earthquake</span> was felt by millions of people living in Nepal, China, <span class="hlt">India</span>, Bangladesh, and Bhutan. The knowledge of ground parameters are very important in developing seismic code of seismic prone regions like Himalaya for better design of buildings. The ground parameters recorded in recent <span class="hlt">earthquake</span> event and aftershocks are compared with attenuation relations for the Himalayan region, the predicted ground motion parameters show good correlation with the observed ground parameters. The results will be of great use to Civil engineers in updating existing building codes in the Himlayan and surrounding regions and also for the evaluation of seismic hazards. The results clearly show that the attenuation relation developed for the Himalayan region should be only used, other attenuation relations based on other regions fail to provide good estimate of observed ground motion parameters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017IJEaS.106.2371K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017IJEaS.106.2371K"><span>Variable anelastic attenuation and site effect in estimating source parameters of various major <span class="hlt">earthquakes</span> including M w 7.8 Nepal and M w 7.5 Hindu kush <span class="hlt">earthquake</span> by using far-field strong-motion data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kumar, Naresh; Kumar, Parveen; Chauhan, Vishal; Hazarika, Devajit</p> <p>2017-10-01</p> <p>Strong-motion records of recent Gorkha Nepal <span class="hlt">earthquake</span> ( M w 7.8), its strong aftershocks and seismic events of Hindu kush region have been analysed for estimation of source parameters. The M w 7.8 Gorkha Nepal <span class="hlt">earthquake</span> of 25 April 2015 and its six aftershocks of magnitude range 5.3-7.3 are recorded at Multi-Parametric Geophysical Observatory, Ghuttu, Garhwal Himalaya (<span class="hlt">India</span>) >600 km west from the epicentre of main shock of Gorkha <span class="hlt">earthquake</span>. The acceleration data of eight <span class="hlt">earthquakes</span> occurred in the Hindu kush region also recorded at this observatory which is located >1000 km east from the epicentre of M w 7.5 Hindu kush <span class="hlt">earthquake</span> on 26 October 2015. The shear wave spectra of acceleration record are corrected for the possible effects of anelastic attenuation at both source and recording site as well as for site amplification. The strong-motion data of six local <span class="hlt">earthquakes</span> are used to estimate the site amplification and the shear wave quality factor ( Q β) at recording site. The frequency-dependent Q β( f) = 124 f 0.98 is computed at Ghuttu station by using inversion technique. The corrected spectrum is compared with theoretical spectrum obtained from Brune's circular model for the horizontal components using grid search algorithm. Computed seismic moment, stress drop and source radius of the <span class="hlt">earthquakes</span> used in this work range 8.20 × 1016-5.72 × 1020 Nm, 7.1-50.6 bars and 3.55-36.70 km, respectively. The results match with the available values obtained by other agencies.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20040171836&hterms=electro-chemical+activity&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Delectro-chemical%2Bactivity','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20040171836&hterms=electro-chemical+activity&qs=N%3D0%26Ntk%3DAll%26Ntx%3Dmode%2Bmatchall%26Ntt%3Delectro-chemical%2Bactivity"><span>Progress in Understanding the Pre-<span class="hlt">Earthquake</span> Associated Events by Analyzing IR Satellite Data</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ouzounov, Dimitar; Taylor, Patrick; Bryant, Nevin</p> <p>2004-01-01</p> <p>We present latest result in understanding the potential relationship between tectonic stress, electro-chemical and thermodynamic processes in the Earths crust and atmosphere with an increase in IR flux as a potential signature of electromagnetic (EM) phenomena that are related to <span class="hlt">earthquake</span> activity, either pre-, co- or post seismic. Thermal infra-red (TIR) surveys performed by the polar orbiting (NOAA/AVHRR MODIS) and geosynchronous weather satellites (GOES, METEOSAT) gave an indication of the appearance (from days to weeks before the event) of "anomalous" space-time TIR transients that are associated with the location (epicenter and local tectonic structures) and time of a number of major <span class="hlt">earthquakes</span> with M>5 and focal depths less than 50km. We analyzed broad category of associated pre-<span class="hlt">earthquake</span> events, which provided evidence for changes in surface temperature, surface latent heat flux, chlorophyll concentrations, soil moisture, brightness temperature, emissivity of surface, water vapour in the atmosphere prior to the <span class="hlt">earthquakes</span> occurred in Algeria, <span class="hlt">India</span>, Iran, Italy, Mexico and Japan. The cause of such anomalies has been mainly related to the change of near-surface thermal properties due to complex lithosphere-hydrosphere-atmospheric interactions. As final results we present examples from the most recent (2000-2004) worldwide strong <span class="hlt">earthquakes</span> and the techniques used to capture the tracks of EM emission mid-IR anomalies and a methodology for practical future use of such phenomena in the early warning systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/pp/pp1550/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/pp/pp1550/"><span>The Loma Prieta, California, <span class="hlt">Earthquake</span> of October 17, 1989: <span class="hlt">Earthquake</span> Occurrence</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Coordinated by Bakun, William H.; Prescott, William H.</p> <p>1993-01-01</p> <p>Professional Paper 1550 seeks to understand the M6.9 Loma Prieta <span class="hlt">earthquake</span> itself. It examines how the fault that generated the <span class="hlt">earthquake</span> ruptured, searches for and evaluates precursors that may have indicated an <span class="hlt">earthquake</span> was coming, reviews forecasts of the <span class="hlt">earthquake</span>, and describes the geology of the <span class="hlt">earthquake</span> area and the crustal forces that affect this geology. Some significant findings were: * Slip during the <span class="hlt">earthquake</span> occurred on 35 km of fault at depths ranging from 7 to 20 km. Maximum slip was approximately 2.3 m. The <span class="hlt">earthquake</span> may not have released all of the strain stored in rocks next to the fault and indicates a potential for another damaging <span class="hlt">earthquake</span> in the Santa Cruz Mountains in the near future may still exist. * The <span class="hlt">earthquake</span> involved a large amount of uplift on a dipping fault plane. Pre-<span class="hlt">earthquake</span> conventional wisdom was that large <span class="hlt">earthquakes</span> in the Bay area occurred as horizontal displacements on predominantly vertical faults. * The fault segment that ruptured approximately coincided with a fault segment identified in 1988 as having a 30% probability of generating a M7 <span class="hlt">earthquake</span> in the next 30 years. This was one of more than 20 relevant <span class="hlt">earthquake</span> forecasts made in the 83 years before the <span class="hlt">earthquake</span>. * Calculations show that the Loma Prieta <span class="hlt">earthquake</span> changed stresses on nearby faults in the Bay area. In particular, the <span class="hlt">earthquake</span> reduced stresses on the Hayward Fault which decreased the frequency of small <span class="hlt">earthquakes</span> on it. * Geological and geophysical mapping indicate that, although the San Andreas Fault can be mapped as a through going fault in the epicentral region, the southwest dipping Loma Prieta rupture surface is a separate fault strand and one of several along this part of the San Andreas that may be capable of generating <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14.3638Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14.3638Z"><span>Revisiting the November 27, 1945 Makran (Mw=8.2) interplate <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zarifi, Z.; Raeesi, M.</p> <p>2012-04-01</p> <p>Makran Subduction Zone (MSZ) in southern Iran and southwestern Pakistan is a zone of convergence, where the remnant oceanic crust of Arabian plate is subducting beneath the Eurasian plate with a rate of less than 30 mm/yr. The November 27, 1945 <span class="hlt">earthquake</span> (Mw=8.2) in eastern section of Makran followed by a tsunami, at some points 15 meters high. More than 4000 victims and widespread devastation along the coastal area of Pakistan, Iran, Oman and <span class="hlt">India</span> are reported for this <span class="hlt">earthquake</span>. We have collected the old seismograms of the 1945 <span class="hlt">earthquake</span> and its largest following <span class="hlt">earthquake</span> (August 5, 1947, Mw=7.3) from a number of stations around the globe. Using ISS data, we relocated these two events. We used the teleseismic body-waveform inversion code of Kikuchi and Kanamori to determine the slip distribution of these two <span class="hlt">earthquakes</span> for the first time. The results show that the extent of rupture of the 1945 <span class="hlt">earthquake</span> is larger than what previously had been approximated in other studies. The slip distribution suggests two distinct sets of asperities with different behavior in the west close to Pasni and in the east close to Ormara. The highest slip was obtained for an area between these two cities which shows geological evidence of rapid uplift. To associate this behavior with the structure of slab interface we studied the TPGA (Trench Parallel Free-air Gravity Anomaly) and TPBA (Trench Parallel Bouguer Anomaly) in MSZ. The results of TPGA does not show the expected phenomenon, which is the correlation of asperities with the area of highly negative TPGA. However, TPBA can make correlation between the observed slip distribution and the structure of slab interface. Using the topography and gravity profiles perpendicular to trench and along the MSZ, we could observe the segmentation in the slab interface. This confirms that we barely expect that the whole interface releases energy in one single megathrust <span class="hlt">earthquake</span>. Current seismicity in MSZ, although sparse, can fairly</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=empowering+AND+india&pg=2&id=EJ580633','ERIC'); return false;" href="https://eric.ed.gov/?q=empowering+AND+india&pg=2&id=EJ580633"><span>Literacy for Migrants: An Ethnography of Literacy Acquisition among Nomads of Kutch.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Dyer, Caroline; Choksi, Archana</p> <p>1997-01-01</p> <p>Recounts the creation of an ethnographic study of literacy acquisition among nomadic pastoralists in <span class="hlt">Gujarat</span> (<span class="hlt">India</span>). Describes the project's goals and methods, research problems, and experiments with Regenerated Freirean Literacy Through Empowering Community Techniques (REFLECT) methods for literacy learning. Concludes with suggestions for future…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/fs/2010/3036/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/fs/2010/3036/"><span>PAGER--Rapid assessment of an <span class="hlt">earthquake?s</span> impact</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Wald, D.J.; Jaiswal, K.; Marano, K.D.; Bausch, D.; Hearne, M.</p> <p>2010-01-01</p> <p>PAGER (Prompt Assessment of Global <span class="hlt">Earthquakes</span> for Response) is an automated system that produces content concerning the impact of significant <span class="hlt">earthquakes</span> around the world, informing emergency responders, government and aid agencies, and the media of the scope of the potential disaster. PAGER rapidly assesses <span class="hlt">earthquake</span> impacts by comparing the population exposed to each level of shaking intensity with models of economic and fatality losses based on past <span class="hlt">earthquakes</span> in each country or region of the world. <span class="hlt">Earthquake</span> alerts--which were formerly sent based only on event magnitude and location, or population exposure to shaking--now will also be generated based on the estimated range of fatalities and economic losses.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017E%26ES...80a2054T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017E%26ES...80a2054T"><span>Natural disaster management in <span class="hlt">India</span> with focus on floods and cyclones</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Thattai, Deeptha V.; Sathyanathan, R.; Dinesh, R.; Harshit Kumar, L.</p> <p>2017-07-01</p> <p>Disasters are of two major kinds, natural and manmade, and affect the community. Natural disasters are caused by natural earth processes like floods, droughts, cyclones, tsunamis, <span class="hlt">earthquakes</span> and epidemics. Manmade disasters occur due to chemical spills, accidents, terrorism activities etc. <span class="hlt">India</span> is prone to almost all the major natural disasters. The high population density combined with poor preparedness, planning and management, and rescue and relief measures inevitably lead to huge losses of lives and property every year in the country. This paper analyses the disaster management policy of <span class="hlt">India</span> and its implementation using two recent case studies - one where a relative degree of success has been achieved (cyclones) and the other where we are still struggling to have even a basic preparedness system in place (floods).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/2008/1160/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/2008/1160/"><span>Creating a Global Building Inventory for <span class="hlt">Earthquake</span> Loss Assessment and Risk Management</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Jaiswal, Kishor; Wald, David J.</p> <p>2008-01-01</p> <p> contribution of building stock, its relative vulnerability, and distribution are vital components for determining the extent of casualties during an <span class="hlt">earthquake</span>. It is evident from large deadly historical <span class="hlt">earthquakes</span> that the distribution of vulnerable structures and their occupancy level during an <span class="hlt">earthquake</span> control the severity of human losses. For example, though the number of strong <span class="hlt">earthquakes</span> in California is comparable to that of Iran, the total <span class="hlt">earthquake</span>-related casualties in California during the last 100 years are dramatically lower than the casualties from several individual Iranian <span class="hlt">earthquakes</span>. The relatively low casualties count in California is attributed mainly to the fact that more than 90 percent of the building stock in California is made of wood and is designed to withstand moderate to large <span class="hlt">earthquakes</span> (Kircher, Seligson and others, 2006). In contrast, the 80 percent adobe and or non-engineered masonry building stock with poor lateral load resisting systems in Iran succumbs even for moderate levels of ground shaking. Consequently, the heavy death toll for the 2003 Bam, Iran <span class="hlt">earthquake</span>, which claimed 31,828 lives (Ghafory-Ashtiany and Mousavi, 2005), is directly attributable to such poorly resistant construction, and future events will produce comparable losses unless practices change. Similarly, multistory, precast-concrete framed buildings caused heavy casualties in the 1988 Spitak, Armenia <span class="hlt">earthquake</span> (Bertero, 1989); weaker masonry and reinforced-concrete framed construction designed for gravity loads with soft first stories dominated losses in the Bhuj, <span class="hlt">India</span> <span class="hlt">earthquake</span> of 2001 (Madabhushi and Haigh, 2005); and adobe and weak masonry dwellings in Peru controlled the death toll in the Peru <span class="hlt">earthquake</span> of 2007 (Taucer, J. and others, 2007). Spence (2007) after conducting a brief survey of most lethal <span class="hlt">earthquakes</span> since 1960 found that building collapses remains a major cause of <span class="hlt">earthquake</span> mortality and unreinforced masonry buildings are one of the mos</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70123309','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70123309"><span>Operational <span class="hlt">earthquake</span> forecasting can enhance <span class="hlt">earthquake</span> preparedness</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Jordan, T.H.; Marzocchi, W.; Michael, A.J.; Gerstenberger, M.C.</p> <p>2014-01-01</p> <p>We cannot yet predict large <span class="hlt">earthquakes</span> in the short term with much reliability and skill, but the strong clustering exhibited in seismic sequences tells us that <span class="hlt">earthquake</span> probabilities are not constant in time; they generally rise and fall over periods of days to years in correlation with nearby seismic activity. Operational <span class="hlt">earthquake</span> forecasting (OEF) is the dissemination of authoritative information about these time‐dependent probabilities to help communities prepare for potentially destructive <span class="hlt">earthquakes</span>. The goal of OEF is to inform the decisions that people and organizations must continually make to mitigate seismic risk and prepare for potentially destructive <span class="hlt">earthquakes</span> on time scales from days to decades. To fulfill this role, OEF must provide a complete description of the seismic hazard—ground‐motion exceedance probabilities as well as short‐term rupture probabilities—in concert with the long‐term forecasts of probabilistic seismic‐hazard analysis (PSHA).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28599674','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28599674"><span>Cluster randomized trial of a mHealth intervention "ImTeCHO" to improve delivery of proven maternal, neonatal, and child care interventions through community-based Accredited Social Health Activists (ASHAs) by enhancing their motivation and strengthening supervision in tribal areas of <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: study protocol for a randomized controlled trial.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Modi, Dhiren; Desai, Shrey; Dave, Kapilkumar; Shah, Shobha; Desai, Gayatri; Dholakia, Nishith; Gopalan, Ravi; Shah, Pankaj</p> <p>2017-06-09</p> <p>To facilitate the delivery of proven maternal, neonatal, and child health (MNCH) services, a new cadre of village-based frontline workers, called the Accredited Social Health Activists (ASHAs), was created in 2005 under the aegis of the National Rural Health Mission in <span class="hlt">India</span>. Evaluations have noted that coverage of selected MNCH services to be delivered by the ASHAs is low. Reasons for low coverage are inadequate supervision and support to ASHAs apart from insufficient skills, poor quality of training, and complexity of tasks to be performed. The proposed study aims to implement and evaluate an innovative intervention based on mobile phone technology (mHealth) to improve the performance of ASHAs through better supervision and support in predominantly tribal and rural communities of <span class="hlt">Gujarat</span>, <span class="hlt">India</span>. This is a two-arm, stratified, cluster randomized trial of 36 months in which the units of randomization will be Primary Health Centers (PHCs). There are 11 PHCs in each arm. The intervention is a newly built mobile phone application used in the public health system and evaluated in three ways: (1) mobile phone as a job aid to ASHAs to increase coverage of MNCH services; (2) mobile phone as a job aid to ASHAs and Auxiliary Nurse Midwives (ANMs) to increase coverage of care among complicated cases by facilitating referrals, if indicated and home-based care; (3) web interface as a job aid for medical officers and PHC staff to improve supervision and support to the ASHA program. Participants of the study are pregnant women, mothers, infants, ASHAs, and PHC staff. Primary outcome measures are a composite index made of critical, proven MNCH services and the proportion of neonates who were visited by ASHAs at home within the first week of birth. Secondary outcomes include coverage of selected MNCH services and care sought by complicated cases. Outcomes will be measured by conducting household surveys at baseline and post-intervention which will be compared with usual practice</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013JSeis..17..593M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013JSeis..17..593M"><span>Ground motion estimation in Delhi from postulated regional and local <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mittal, Himanshu; Kumar, Ashok; Kamal</p> <p>2013-04-01</p> <p>Ground motions are estimated at 55 sites in Delhi, the capital of <span class="hlt">India</span> from four postulated <span class="hlt">earthquakes</span> (three regional M w = 7.5, 8.0, and 8.5 and one local). The procedure consists of (1) synthesis of ground motion at a hard reference site (NDI) and (2) estimation of ground motion at other sites in the city via known transfer functions and application of the random vibration theory. This work provides a more extensive coverage than earlier studies (e.g., Singh et al., Bull Seism Soc Am 92:555-569, 2002; Bansal et al., J Seismol 13:89-105, 2009). The Indian code response spectra corresponding to Delhi (zone IV) are found to be conservative at hard soil sites for all postulated <span class="hlt">earthquakes</span> but found to be deficient for M w = 8.0 and 8.5 <span class="hlt">earthquakes</span> at soft soil sites. Spectral acceleration maps at four different natural periods are strongly influenced by the shallow geological and soil conditions. Three pockets of high acceleration values are seen. These pockets seem to coincide with the contacts of (a) Aravalli quartzite and recent Yamuna alluvium (towards the East), (b) Aravalli quartzite and older quaternary alluvium (towards the South), and (c) older quaternary alluvium and recent Yamuna alluvium (towards the North).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24135315','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24135315"><span>Coping with the challenges of early disaster response: 24 years of field hospital experience after <span class="hlt">earthquakes</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Bar-On, Elhanan; Abargel, Avi; Peleg, Kobi; Kreiss, Yitshak</p> <p>2013-10-01</p> <p>To propose strategies and recommendations for future planning and deployment of field hospitals after <span class="hlt">earthquakes</span> by comparing the experience of 4 field hospitals deployed by The Israel Defense Forces (IDF) Medical Corps in Armenia, Turkey, <span class="hlt">India</span> and Haiti. Quantitative data regarding the <span class="hlt">earthquakes</span> were collected from published sources; data regarding hospital activity were collected from IDF records; and qualitative information was obtained from structured interviews with key figures involved in the missions. The hospitals started operating between 89 and 262 hours after the <span class="hlt">earthquakes</span>. Their sizes ranged from 25 to 72 beds, and their personnel numbered between 34 and 100. The number of patients treated varied from 1111 to 2400. The proportion of <span class="hlt">earthquake</span>-related diagnoses ranged from 28% to 67% (P < .001), with hospitalization rates between 3% and 66% (P < .001) and surgical rates from 1% to 24% (P < .001). In spite of characteristic scenarios and injury patterns after <span class="hlt">earthquakes</span>, patient caseload and treatment requirements varied widely. The variables affecting the patient profile most significantly were time until deployment, total number of injured, availability of adjacent medical facilities, and possibility of evacuation from the disaster area. When deploying a field hospital in the early phase after an <span class="hlt">earthquake</span>, a wide variability in patient caseload should be anticipated. Customization is difficult due to the paucity of information. Therefore, early deployment necessitates full logistic self-sufficiency and operational versatility. Also, collaboration with local and international medical teams can greatly enhance treatment capabilities.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://earthquake.usgs.gov/learn/kids/','NIH-MEDLINEPLUS'); return false;" href="https://earthquake.usgs.gov/learn/kids/"><span><span class="hlt">Earthquakes</span> for Kids</span></a></p> <p><a target="_blank" href="http://medlineplus.gov/">MedlinePlus</a></p> <p></p> <p></p> <p>... across a fault to learn about past <span class="hlt">earthquakes</span>. Science Fair Projects A GPS instrument measures slow movements of the ground. Become an <span class="hlt">Earthquake</span> Scientist Cool <span class="hlt">Earthquake</span> Facts Today in <span class="hlt">Earthquake</span> History A scientist stands in ...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_16 --> <div id="page_17" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="321"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC33D1267J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC33D1267J"><span>Responses of nocturnal rodents to shrub encroachment in Banni grasslands, <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jayadevan, A.</p> <p>2016-12-01</p> <p>Shrub encroachment is one of the greatest threats to grasslands globally. These woodlands can strongly influence the behaviour of small mammals adapted to more open habitats, which rely on high visibility for early detection of predators. In semi-arid grasslands, rodents are considered keystone species. Although shrub encroachment is known to negatively affect rodent assemblages, its impact on the foraging behaviour of rodents, which is known to vary in response to risky situations, is unknown. Understanding whether shrub encroachment alters such antipredator behaviour is important as antipredator behaviour can alter the distribution, abundance and ultimately, survival of prey species. In this study, I explored the effects of shrub encroachment on the foraging behaviour of nocturnal rodent communities in the Banni grasslands, <span class="hlt">India</span>. I examined foraging behaviour, quantified using the giving-up density (GUD) framework and the number of rodent crossings around food patches, in two habitats that differed in the extent of shrub encroachment. Under the GUD framework, the amount of food left behind by a forager in a food patch reflects the costs of feeding at the patch. Higher GUDs imply higher foraging costs. I also investigated how removal of an invasive woody plant, Prosopis juliflora would affect foraging behaviour of nocturnal rodents. High shrub encroachment was associated with higher foraging costs (higher GUDs) and lower activity than the sparsely wooded habitat, likely due to low visibility in the densely wooded habitat. The dense habitat also supported a higher richness and relative abundance of generalist rodents than the sparse habitat, likely due to the increased heterogeneity of the habitat. The tree removal experiment revealed that rodents had lower GUDs (i.e., low foraging costs) after the event of tree cutting. This may be due to the reduction of cover in the habitat, leading to higher visibility and lower predation risk. My results suggest that shrub</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMNH51C1979S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMNH51C1979S"><span>Analyzing thermal anomaly of the Nepal Mw7.9 <span class="hlt">earthquake</span> on 25 April 2015 using OLR data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>SUN, K.; Shan, X.; Ouzounov, D.</p> <p>2016-12-01</p> <p>An Mw7.9 <span class="hlt">earthquake</span>, located at the front of the <span class="hlt">India</span>-Eurasia collision belt, hit Nepal on April 25th, 2015. The temporal and spatial variations of outgoing long wave radiation (OLR) around the time of Nepal <span class="hlt">earthquake</span> Mw7.9 April 25th, 2015 have been analyzed based on nine years data (2006-2014) using combined Robust Satellite Technique (RST) and vorticity methods. The results show that on April 4th an increase of emitted infrared radiation was observed from the satellite data and an anomaly developed on south of the epicenter. The maximum anomalies, located westward from the epicenter about 100 kilometers, were found on April 24th. Mechanisms for triggering the event are not yet known and still many theoretical questions on the quantitative link between long wave radiation and tectonic stress need to be answered. <span class="hlt">Earthquake</span> prediction is still a challenging work to us. Much work needs to be done in how to obtain the seismic precursor information.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28144801','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28144801"><span>A brief and critical review on hydrofluorosis in diverse species of domestic animals in <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Choubisa, Shanti Lal</p> <p>2018-02-01</p> <p><span class="hlt">India</span> is one of the fluoride-endemic countries where the maximum numbers of ground or drinking water sources are naturally fluoridated. In <span class="hlt">India</span>, a total of 23, out of 36 states and union territories have drinking water contaminated with fluoride in varying concentration. In the present scenario, especially in rural <span class="hlt">India</span>, besides the surface waters (perennial ponds, dams, rivers, etc.), bore wells and hand pumps are the principal drinking water sources for domestic animals such as cattle (Bos taurus), water buffaloes (Bubalus bubalis), sheep (Ovis aries), goats (Capra hircus), horses (Equus caballus), donkeys (Equus asinus) and dromedary camels (Camelus dromedarius). Out of 23 states, 17 states, namely Andhra Pradesh, Assam, Bihar, Chhattisgarh, <span class="hlt">Gujarat</span>, Haryana, Jharkhand, Karnataka, Kerala, Madhya Pradesh, Maharashtra, Odisha (Orissa), Punjab, Rajasthan, Telangana, Uttar Pradesh and West Bengal, have fluoride beyond the maximum permissible limit of 1.0 or 1.5 ppm in drinking water. This situation is a great concern for the animal health because fluoride is a slow toxicant and causes chronic diverse serious health hazards or toxic effects. Despite the fact that domestic animals are the basic income sources in rural areas and possess a significant contributory role not only in the agriculture sector but also in the strengthening of economy as well as in sustainable development of the country, research work on chronic fluoride intoxication (hydrofluorosis) due to drinking of fluoridated water in domestic animals rearing in various fluoride-endemic states is not enough as compared to work done in humans. However, some interesting and excellent research works conducted on different aspects of hydrofluorosis in domesticated animals rearing in different states are briefly and critically reviewed in the present communication. Author believes that this review paper not only will be more useful for researchers to do some more advance research work on fluoride</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21525704','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21525704"><span>Prevalence and socio-demographic correlates of dental anxiety among a group of adult patients attending a dental institution in Vadodara city, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Malvania, Ekta A; Ajithkrishnan, C G</p> <p>2011-01-01</p> <p>Anxiety is a subjective state of feelings. Dental anxiety is often reported as a cause of irregular dental attendance, delay in seeking dental care or even avoidance of dental care, resulting in poor oral health related quality of life. To assess the prevalence and socio-demographic correlates of dental anxiety among a group of adult patients attending a dental institution in Vadodara, <span class="hlt">Gujarat</span>. A total of 150 adult patients waiting in the out-patient Department of Oral Diagnosis of K.M. Shah Dental College and Hospital were included in the study. Subjects were selected by convenience sampling. Dental anxiety was assessed by using Modified Dental Anxiety Scale (MDAS) and self-designed, semi-structured questionnaire incorporating various demographic variables, type and nature of dental treatment. Statistical analysis was done using SPSS version 16. Descriptive analysis, unpaired t-test, one-way analysis of variance (ANOVA) test and multiple logistic regression were applied for statistical analysis. 46% of the participants were dentally anxious. Females were found to be significantly more anxious than males. Subjects residing in villages had significantly more score than those residing in city. Relative influence of age, education, type of dental treatment, and previous dental visit were not significantly associated with dental anxiety. However, those subjects who had past negative dental experience were found to be significantly more anxious. The study shows that dental anxiety was high among study subjects. It is recommended that this issue should be given due importance and addressed in a practical and meaningful manner.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T21C0576B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T21C0576B"><span>Morphometric study of the Habo dome, Kachchh, <span class="hlt">Gujarat</span>, <span class="hlt">India</span>: implications on neotectonic activity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bhattacharjee, N.; Mohanty, S. P.</p> <p>2017-12-01</p> <p>The Kachchh Basin of western <span class="hlt">India</span> was developed during the separation of the Indian plate from the Gondwanaland in Mesozoic. Series of E-W striking master faults were generated during this extensional phase. The collision of the Indian and Eurasian plates in Eocene time resulted in the change of stress regime to a compressional setting when the built-up stress developed NNW-SSE to NNE-SSW striking transverse faults and reactivated the earlier E-W master faults. The present work was carried out in the Habo dome, located in the central part of the Kachchh Basin, to analyse the morphometric features such as the bifurcation ratio, circulation ratio, drainage texture, asymmetric factor, hypsometric indices and mountain front sinuosity of selected sub-watersheds of the area to understand the effects of fault reactivation and neotectonic activities on the geometry of the dome. Shuttle Radar Topographic Mission (SRTM) Digital Elevation Model (DEM) data were used to extract drainage network for morphometric analysis of the Kaswati, Khari, and Pur river basins. The study area is elliptical in outline with the long axis trending approximately E-W. The evolution of this domal structure is interpreted to be the result of fault-bound nature of the block. The northern slope of the dome is bound by the Kachchh Mainland Fault and the eastern and western boundaries are marked by transverse faults. The undulating topography was developed by differential movements along several transverse faults striking NW-SE, N-S, and NE-SW. The earlier interpretation of laccolith intrusion into the sedimentary rocks is not supported by the data analysis and field mapping. Stress propagations from the Himalayan range in the northeast and Sulaiman range in the northwest are identified to be the causative factor for historical seismicity and drainage anomalies in the area. Keywords: Basin morphometry, Geographical Information System, Lineament patterns, Kachchh basin, Neotectonics, Fault reactivation</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25656835','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25656835"><span>Attitude and awareness towards organ donation in western <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Balwani, Manish R; Gumber, Manoj R; Shah, Pankaj R; Kute, Vivek B; Patel, Himanshu V; Engineer, Divyesh P; Gera, Dinesh N; Godhani, Umesh; Shah, Mehin; Trivedi, Hargovind L</p> <p>2015-05-01</p> <p>To determine the knowledge, attitudes and practices regarding organ donation in western <span class="hlt">India</span>. Convenience sampling was used to generate a sample of 250; 200 interviews were successfully completed and used for analysis. Data collection was carried out via face to face interviews based on a pre-tested questionnaire in selected public areas of Ahmedabad, <span class="hlt">Gujarat</span> state of <span class="hlt">India</span>. Data entry was made in excel software in codes and analysis was done by SPSS software. About 86% of participants were aware of the term organ donation but knowledge about its various aspects was low. About 48% aware people heard about organ donation through medical fraternity, whereas only about 21% became aware through mass media. About 59% of aware people believed there is a potential danger of donated organs being misused, abused or misappropriated. About 47% of aware people said they would consider donating organs, while only 16% said they would definitely donate irrespective of circumstances. Around 97.67% participants said they would prefer to donate to nonsmokers. About 74.41% participants were unaware about any legislation regarding organ donation. About 77% participants showed their will to donate to mentally sound persons, and 42.04% participants showed their will to donate even physically challenged people. Around 78 participants felt that they would donate organs to persons irrespective of their religion. About 81% of aware people were of the opinion that consent for organ donation after death should be given by family members. None of the interviewed participants had a donor card. Better knowledge and awareness will help in promoting organ donation. Effective campaign needs to be driven to educate people with relevant information with the involvement of media, doctors and religious scholars.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=PIA03304&hterms=1956&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3D%253F%253F%253F%253F%253F%253F%253F%253F%253F%253F%2B%253F.%2B%253F.%2B%253F%253F%253F%253F%253F%253F%253F%253F%2B%253F%253F%253F%253F%253F%253F%253F%253F%253F%253F.%2B%253F.%2B1956','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=PIA03304&hterms=1956&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3D%253F%253F%253F%253F%253F%253F%253F%253F%253F%253F%2B%253F.%2B%253F.%2B%253F%253F%253F%253F%253F%253F%253F%253F%2B%253F%253F%253F%253F%253F%253F%253F%253F%253F%253F.%2B%253F.%2B1956"><span>SRTM Perspective View with Landsat Overlay: Rann of Kachchh, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2001-01-01</p> <p><p/> The <span class="hlt">earthquake</span> that struck western <span class="hlt">India</span> on January 26,2001, was the country's strongest in the past 50 years. This perspective view shows the area of the <span class="hlt">earthquake</span>'s epicenter in the lower left corner. The southern Rann of Kachchh appears in the foreground. The Rann is an area of low-lying salt flats that shows up with various shades of white and blue in this false-color Landsat image. The gray area on the middle of the image is called the Banni plains.<p/>The darker blue spots and curving lines in the Rann and the Banni plains are features that appeared after the January <span class="hlt">earthquake</span>. Their true colors are shades of white and gray, but the infrared data used in the image gives them a blue or turquoise color. These features are the effects of liquefaction of wet soil, sand and mud layers caused by the shaking of the <span class="hlt">earthquake</span>. The liquefaction beneath the surface causes water to be squeezed out at the surface forming mud volcanoes, sand blows and temporary springs. Some of the residents of this dry area were hopeful that they could use the water, but they found that the water was too salty in almost every place where it came to the surface.<p/>The city of Bhuj, <span class="hlt">India</span>, appears as a gray area in the upper right of the image. Bhuj and many other towns and cities nearby were almost completely destroyed by the January 2001 <span class="hlt">earthquake</span>. This magnitude 7.7 <span class="hlt">earthquake</span> was the deadliest in the history of <span class="hlt">India</span> with some 20,000 fatalities and over a million homes damaged or destroyed. The city of Bhuj was the historical capital of the Kachchh region. Highways and rivers appear as dark lines. Vegetation appears bright green in this false-color Landsat image.<p/>The city of Anjar is in the dark gray area near the upper left of the image. Previously damaged by a magnitude 6.1 <span class="hlt">earthquake</span> in 1956 that killed 152people, Anjar suffered again in the larger 2001 <span class="hlt">earthquake</span>.<p/>The red hills in the center of the image are the Has and Karo Hills, which reach up to 300 m (900 feet</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=PIA03301&hterms=1956&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3D%253F%253F%253F%253F%253F%253F%253F%253F%253F%253F%2B%253F.%2B%253F.%2B%253F%253F%253F%253F%253F%253F%253F%253F%2B%253F%253F%253F%253F%253F%253F%253F%253F%253F%253F.%2B%253F.%2B1956','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=PIA03301&hterms=1956&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D60%26Ntt%3D%253F%253F%253F%253F%253F%253F%253F%253F%253F%253F%2B%253F.%2B%253F.%2B%253F%253F%253F%253F%253F%253F%253F%253F%2B%253F%253F%253F%253F%253F%253F%253F%253F%253F%253F.%2B%253F.%2B1956"><span>SRTM Perspective View with Landsat Overlay: Bhuj and Anjar, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p></p> <p>2001-01-01</p> <p><p/> This perspective view shows the city of Bhuj, <span class="hlt">India</span>, in the foreground near the right side (dark gray area). Bhuj and many other towns and cities nearby were almost completely destroyed by the January 26, 2001, <span class="hlt">earthquake</span> in western <span class="hlt">India</span>. This magnitude 7.6 <span class="hlt">earthquake</span> was the deadliest in the history of <span class="hlt">India</span> with some 20,000 fatalities and over a million homes damaged or destroyed. The epicenter of the <span class="hlt">earthquake</span> was in the area in the upper left corner of this view.<p/>The city of Anjar is in the dark gray area near the top center of the image. Anjar was previously damaged by a magnitude 6.1 <span class="hlt">earthquake</span> in 1956 that killed 152 people and suffered again in the larger 2001 <span class="hlt">earthquake</span>. The red hills to the left of the center of the image are the Has and Karo Hills, which reach up to 300 meter (900 feet) elevation. These hills are formed by folded red sandstone layers. Geologists are studying these folded layers to determine if they are related to the fault that broke in the 2001 <span class="hlt">earthquake</span>. The city of Bhuj was the historical capital of the Kachchh region. Highways and rivers appear as dark lines. Vegetation appears bright green in this false-color Landsat image. The Gulf of Kachchh (or Kutch) is the blue area in the upper right corner of the image, and the gray area on the left side of the image is called the Banni plains.<p/>This three-dimensional perspective view was generated using topographic data from the Shuttle Radar Topography Mission (SRTM) and an enhanced false-color Landsat 7 satellite image. Colors are from Landsat bands 5, 4, and 2 as red, green and blue, respectively. Topographic expression is exaggerated 5X.<p/>Landsat has been providing visible and infrared views of the Earth since 1972. SRTM elevation data matches the 30-meter resolution of most Landsat images and will substantially help in analyses of the large and growing Landsat image archive. The Landsat 7 Thematic Mapper image used here was provided to the SRTM by the United States</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23086467','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23086467"><span>Prevalence of β-thalassemia and other haemoglobinopathies in six cities in <span class="hlt">India</span>: a multicentre study.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mohanty, D; Colah, R B; Gorakshakar, A C; Patel, R Z; Master, D C; Mahanta, J; Sharma, S K; Chaudhari, U; Ghosh, M; Das, S; Britt, R P; Singh, S; Ross, C; Jagannathan, L; Kaul, R; Shukla, D K; Muthuswamy, V</p> <p>2013-01-01</p> <p>The population of <span class="hlt">India</span> is extremely diverse comprising of more than 3,000 ethnic groups who still follow endogamy. Haemoglobinopathies are the commonest hereditary disorders in <span class="hlt">India</span> and pose a major health problem. The data on the prevalence of β-thalassemias and other haemoglobinopathies in different caste/ethnic groups of <span class="hlt">India</span> is scarce. Therefore the present multicentre study was undertaken in six cities of six states of <span class="hlt">India</span> (Maharashtra, <span class="hlt">Gujarat</span>, West Bengal, Assam, Karnataka and Punjab) to determine the prevalence of haemoglobinopathies in different caste/ethnic groups using uniform methodology. Fifty-six thousand seven hundred eighty individuals (college students and pregnant women) from different caste/ethnic groups were screened. RBC indices were measured on an automated haematology counter while the percentage of HbA(2), HbF and other abnormal Hb variants were estimated by HPLC on the Variant Hemoglobin Testing System. The overall prevalence of β-thalassemia trait was 2.78 % and varied from 1.48 to 3.64 % in different states, while the prevalence of β-thalassemia trait in 59 ethnic groups varied from 0 to 9.3 %. HbE trait was mainly seen in Dibrugarh in Assam (23.9 %) and Kolkata in West Bengal (3.92 %). In six ethnic groups from Assam, the prevalence of HbE trait varied from 41.1 to 66.7 %. Few subjects with δβ-thalassemia, HPFH, HbS trait, HbD trait, HbE homozygous and HbE β-thalassemia as well as HbS homozygous and HbS-β-thalassemia (<1 %) were also identified. This is the first large multicentre study covering cities from different regions of the country for screening for β-thalassemia carriers and other haemoglobinopathies where uniform protocols and methodology was followed and quality control ensured by the co-ordinating centre. This study also shows that establishment of centres for screening for β-thalassemia and other haemoglobinopathies is possible in medical colleges. Creating awareness, screening and counselling can be</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70101108','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70101108"><span>Missing great <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hough, Susan E.</p> <p>2013-01-01</p> <p>The occurrence of three <span class="hlt">earthquakes</span> with moment magnitude (Mw) greater than 8.8 and six <span class="hlt">earthquakes</span> larger than Mw 8.5, since 2004, has raised interest in the long-term global rate of great <span class="hlt">earthquakes</span>. Past studies have focused on the analysis of <span class="hlt">earthquakes</span> since 1900, which roughly marks the start of the instrumental era in seismology. Before this time, the catalog is less complete and magnitude estimates are more uncertain. Yet substantial information is available for <span class="hlt">earthquakes</span> before 1900, and the catalog of historical events is being used increasingly to improve hazard assessment. Here I consider the catalog of historical <span class="hlt">earthquakes</span> and show that approximately half of all Mw ≥ 8.5 <span class="hlt">earthquakes</span> are likely missing or underestimated in the 19th century. I further present a reconsideration of the felt effects of the 8 February 1843, Lesser Antilles <span class="hlt">earthquake</span>, including a first thorough assessment of felt reports from the United States, and show it is an example of a known historical <span class="hlt">earthquake</span> that was significantly larger than initially estimated. The results suggest that incorporation of best available catalogs of historical <span class="hlt">earthquakes</span> will likely lead to a significant underestimation of seismic hazard and/or the maximum possible magnitude in many regions, including parts of the Caribbean.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24952120','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24952120"><span>Study on validity of a rapid diagnostic test kit versus light microscopy for malaria diagnosis in Ahmedabad city, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Vyas, S; Puwar, B; Patel, V; Bhatt, G; Kulkarni, S; Fancy, M</p> <p>2014-05-01</p> <p>Light microscopy of blood smears for diagnosis of malaria in the field has several limitations, notably delays in diagnosis. This study in Ahmedabad in <span class="hlt">Gujarat</span> State, <span class="hlt">India</span>, evaluated the diagnostic performance of a rapid diagnostic test for malaria (SD Bioline Malaria Ag P.f/Pan) versus blood smear examination as the gold standard. All fever cases presenting at 13 urban health centres were subjected to rapid diagnostic testing and thick and thin blood smears. A total of 677 cases with fever were examined; 135 (20.0%) tested positive by rapid diagnostic test and 86 (12.7%) by blood smear. The sensitivity of the rapid diagnostic test for malaria was 98.8%, specificity was 91.5%, positive predictive value 63.0% and negative predictive value 99.8%. For detection of Plasmodium falciparum the sensitivity of rapid diagnostic test was 100% and specificity was 97.3%. The results show the acceptability of the rapid test as an alternative to light microscopy in the field setting.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012JESS..121.1351K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012JESS..121.1351K"><span>Deterministic seismic hazard macrozonation of <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kolathayar, Sreevalsa; Sitharam, T. G.; Vipin, K. S.</p> <p>2012-10-01</p> <p><span class="hlt">Earthquakes</span> are known to have occurred in Indian subcontinent from ancient times. This paper presents the results of seismic hazard analysis of <span class="hlt">India</span> (6°-38°N and 68°-98°E) based on the deterministic approach using latest seismicity data (up to 2010). The hazard analysis was done using two different source models (linear sources and point sources) and 12 well recognized attenuation relations considering varied tectonic provinces in the region. The <span class="hlt">earthquake</span> data obtained from different sources were homogenized and declustered and a total of 27,146 <span class="hlt">earthquakes</span> of moment magnitude 4 and above were listed in the study area. The sesismotectonic map of the study area was prepared by considering the faults, lineaments and the shear zones which are associated with <span class="hlt">earthquakes</span> of magnitude 4 and above. A new program was developed in MATLAB for smoothing of the point sources. For assessing the seismic hazard, the study area was divided into small grids of size 0.1° × 0.1° (approximately 10 × 10 km), and the hazard parameters were calculated at the center of each of these grid cells by considering all the seismic sources within a radius of 300 to 400 km. Rock level peak horizontal acceleration (PHA) and spectral accelerations for periods 0.1 and 1 s have been calculated for all the grid points with a deterministic approach using a code written in MATLAB. Epistemic uncertainty in hazard definition has been tackled within a logic-tree framework considering two types of sources and three attenuation models for each grid point. The hazard evaluation without logic tree approach also has been done for comparison of the results. The contour maps showing the spatial variation of hazard values are presented in the paper.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/146985','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/146985"><span>Analog <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Hofmann, R.B.</p> <p>1995-09-01</p> <p>Analogs are used to understand complex or poorly understood phenomena for which little data may be available at the actual repository site. <span class="hlt">Earthquakes</span> are complex phenomena, and they can have a large number of effects on the natural system, as well as on engineered structures. Instrumental data close to the source of large <span class="hlt">earthquakes</span> are rarely obtained. The rare events for which measurements are available may be used, with modfications, as analogs for potential large <span class="hlt">earthquakes</span> at sites where no <span class="hlt">earthquake</span> data are available. In the following, several examples of nuclear reactor and liquified natural gas facility siting are discussed.more » A potential use of analog <span class="hlt">earthquakes</span> is proposed for a high-level nuclear waste (HLW) repository.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..11.6654D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..11.6654D"><span>Turkish Compulsory <span class="hlt">Earthquake</span> Insurance and "Istanbul <span class="hlt">Earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Durukal, E.; Sesetyan, K.; Erdik, M.</p> <p>2009-04-01</p> <p>The city of Istanbul will likely experience substantial direct and indirect losses as a result of a future large (M=7+) <span class="hlt">earthquake</span> with an annual probability of occurrence of about 2%. This paper dwells on the expected building losses in terms of probable maximum and average annualized losses and discusses the results from the perspective of the compulsory <span class="hlt">earthquake</span> insurance scheme operational in the country. The TCIP system is essentially designed to operate in Turkey with sufficient penetration to enable the accumulation of funds in the pool. Today, with only 20% national penetration, and about approximately one-half of all policies in highly <span class="hlt">earthquake</span> prone areas (one-third in Istanbul) the system exhibits signs of adverse selection, inadequate premium structure and insufficient funding. Our findings indicate that the national compulsory <span class="hlt">earthquake</span> insurance pool in Turkey will face difficulties in covering incurring building losses in Istanbul in the occurrence of a large <span class="hlt">earthquake</span>. The annualized <span class="hlt">earthquake</span> losses in Istanbul are between 140-300 million. Even if we assume that the deductible is raised to 15%, the <span class="hlt">earthquake</span> losses that need to be paid after a large <span class="hlt">earthquake</span> in Istanbul will be at about 2.5 Billion, somewhat above the current capacity of the TCIP. Thus, a modification to the system for the insured in Istanbul (or Marmara region) is necessary. This may mean an increase in the premia and deductible rates, purchase of larger re-insurance covers and development of a claim processing system. Also, to avoid adverse selection, the penetration rates elsewhere in Turkey need to be increased substantially. A better model would be introduction of parametric insurance for Istanbul. By such a model the losses will not be indemnified, however will be directly calculated on the basis of indexed ground motion levels and damages. The immediate improvement of a parametric insurance model over the existing one will be the elimination of the claim processing</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016NatGe...9..834I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016NatGe...9..834I"><span><span class="hlt">Earthquake</span> potential revealed by tidal influence on <span class="hlt">earthquake</span> size-frequency statistics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ide, Satoshi; Yabe, Suguru; Tanaka, Yoshiyuki</p> <p>2016-11-01</p> <p>The possibility that tidal stress can trigger <span class="hlt">earthquakes</span> is long debated. In particular, a clear causal relationship between small <span class="hlt">earthquakes</span> and the phase of tidal stress is elusive. However, tectonic tremors deep within subduction zones are highly sensitive to tidal stress levels, with tremor rate increasing at an exponential rate with rising tidal stress. Thus, slow deformation and the possibility of <span class="hlt">earthquakes</span> at subduction plate boundaries may be enhanced during periods of large tidal stress. Here we calculate the tidal stress history, and specifically the amplitude of tidal stress, on a fault plane in the two weeks before large <span class="hlt">earthquakes</span> globally, based on data from the global, Japanese, and Californian <span class="hlt">earthquake</span> catalogues. We find that very large <span class="hlt">earthquakes</span>, including the 2004 Sumatran, 2010 Maule <span class="hlt">earthquake</span> in Chile and the 2011 Tohoku-Oki <span class="hlt">earthquake</span> in Japan, tend to occur near the time of maximum tidal stress amplitude. This tendency is not obvious for small <span class="hlt">earthquakes</span>. However, we also find that the fraction of large <span class="hlt">earthquakes</span> increases (the b-value of the Gutenberg-Richter relation decreases) as the amplitude of tidal shear stress increases. The relationship is also reasonable, considering the well-known relationship between stress and the b-value. This suggests that the probability of a tiny rock failure expanding to a gigantic rupture increases with increasing tidal stress levels. We conclude that large <span class="hlt">earthquakes</span> are more probable during periods of high tidal stress.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018IJMPB..3250081L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018IJMPB..3250081L"><span>Understanding <span class="hlt">earthquake</span> from the granular physics point of view — Causes of <span class="hlt">earthquake</span>, <span class="hlt">earthquake</span> precursors and predictions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lu, Kunquan; Hou, Meiying; Jiang, Zehui; Wang, Qiang; Sun, Gang; Liu, Jixing</p> <p>2018-03-01</p> <p>We treat the earth crust and mantle as large scale discrete matters based on the principles of granular physics and existing experimental observations. Main outcomes are: A granular model of the structure and movement of the earth crust and mantle is established. The formation mechanism of the tectonic forces, which causes the <span class="hlt">earthquake</span>, and a model of propagation for precursory information are proposed. Properties of the seismic precursory information and its relevance with the <span class="hlt">earthquake</span> occurrence are illustrated, and principle of ways to detect the effective seismic precursor is elaborated. The mechanism of deep-focus <span class="hlt">earthquake</span> is also explained by the jamming-unjamming transition of the granular flow. Some <span class="hlt">earthquake</span> phenomena which were previously difficult to understand are explained, and the predictability of the <span class="hlt">earthquake</span> is discussed. Due to the discrete nature of the earth crust and mantle, the continuum theory no longer applies during the quasi-static seismological process. In this paper, based on the principles of granular physics, we study the causes of <span class="hlt">earthquakes</span>, <span class="hlt">earthquake</span> precursors and predictions, and a new understanding, different from the traditional seismological viewpoint, is obtained.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=earthquakes&pg=5&id=EJ782558','ERIC'); return false;" href="https://eric.ed.gov/?q=earthquakes&pg=5&id=EJ782558"><span>Redefining <span class="hlt">Earthquakes</span> and the <span class="hlt">Earthquake</span> Machine</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Hubenthal, Michael; Braile, Larry; Taber, John</p> <p>2008-01-01</p> <p>The <span class="hlt">Earthquake</span> Machine (EML), a mechanical model of stick-slip fault systems, can increase student engagement and facilitate opportunities to participate in the scientific process. This article introduces the EML model and an activity that challenges ninth-grade students' misconceptions about <span class="hlt">earthquakes</span>. The activity emphasizes the role of models…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012NHESS..12..431R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012NHESS..12..431R"><span>Transient postseismic mantle relaxation following 2004 Sumatra <span class="hlt">earthquake</span>: implications of seismic vulnerability in the Andaman-Nicobar region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Reddy, C. D.; Prajapati, S. K.; Sunil, P. S.; Arora, S. K.</p> <p>2012-02-01</p> <p>Throughout the world, the tsunami generation potential of some large under-sea <span class="hlt">earthquakes</span> significantly contributes to regional seismic hazard, which gives rise to significant risk in the near-shore provinces where human settlements are in sizeable population, often referred to as coastal seismic risk. In this context, we show from the pertinent GPS data that the transient stresses generated by the viscoelastic relaxation process taking place in the mantle is capable of rupturing major faults by stress transfer from the mantle through the lower crust including triggering additional rupture on the other major faults. We also infer that postseismic relaxation at relatively large depths can push some of the fault segments to reactivation causing failure sequences. As an illustration to these effects, we consider in detail the <span class="hlt">earthquake</span> sequence comprising six events, starting from the main event of Mw = 7.5, on 10 August 2009 and tapering off to a small <span class="hlt">earthquake</span> of Mw = 4.5 on 2 February 2011 over a period of eighteen months in the intensely seismic Andaman Islands between <span class="hlt">India</span> and Myanmar. The persisting transient stresses, spatio-temporal seismic pattern, modeled Coulomb stress changes, and the southward migration of <span class="hlt">earthquake</span> activity has increased the probability of moderate <span class="hlt">earthquakes</span> recurring in the northern Andaman region, particularly closer to or somewhat south of Diglipur.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.S11B1697E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.S11B1697E"><span>OMG <span class="hlt">Earthquake</span>! Can Twitter improve <span class="hlt">earthquake</span> response?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Earle, P. S.; Guy, M.; Ostrum, C.; Horvath, S.; Buckmaster, R. A.</p> <p>2009-12-01</p> <p>The U.S. Geological Survey (USGS) is investigating how the social networking site Twitter, a popular service for sending and receiving short, public, text messages, can augment its <span class="hlt">earthquake</span> response products and the delivery of hazard information. The goal is to gather near real-time, <span class="hlt">earthquake</span>-related messages (tweets) and provide geo-located <span class="hlt">earthquake</span> detections and rough maps of the corresponding felt areas. Twitter and other social Internet technologies are providing the general public with anecdotal <span class="hlt">earthquake</span> hazard information before scientific information has been published from authoritative sources. People local to an event often publish information within seconds via these technologies. In contrast, depending on the location of the <span class="hlt">earthquake</span>, scientific alerts take between 2 to 20 minutes. Examining the tweets following the March 30, 2009, M4.3 Morgan Hill <span class="hlt">earthquake</span> shows it is possible (in some cases) to rapidly detect and map the felt area of an <span class="hlt">earthquake</span> using Twitter responses. Within a minute of the <span class="hlt">earthquake</span>, the frequency of “earthquake” tweets rose above the background level of less than 1 per hour to about 150 per minute. Using the tweets submitted in the first minute, a rough map of the felt area can be obtained by plotting the tweet locations. Mapping the tweets from the first six minutes shows observations extending from Monterey to Sacramento, similar to the perceived shaking region mapped by the USGS “Did You Feel It” system. The tweets submitted after the <span class="hlt">earthquake</span> also provided (very) short first-impression narratives from people who experienced the shaking. Accurately assessing the potential and robustness of a Twitter-based system is difficult because only tweets spanning the previous seven days can be searched, making a historical study impossible. We have, however, been archiving tweets for several months, and it is clear that significant limitations do exist. The main drawback is the lack of quantitative information</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20642340','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20642340"><span>Prevelence and causes of visual impairment and blindness in older adults in an area of <span class="hlt">India</span> with a high cataract surgical rate.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Murthy, Gudlavalleti V S; Vashist, Praveen; John, Neena; Pokharel, Gopal; Ellwein, Leon B</p> <p>2010-08-01</p> <p>The cataract surgical rate (CSR) in <span class="hlt">Gujarat</span>, <span class="hlt">India</span> is reported to be above 10,000 per million population. This study was conducted to investigate the prevalence and causes of vision impairment/blindness among older adults in a high CSR area. Geographically defined cluster sampling was used in randomly selecting persons >or= 50 years of age in Navsari district. Subjects in 35 study clusters were enumerated and invited for measurement of presenting and best-corrected visual acuity and an ocular examination. The principal cause was identified for eyes with presenting visual acuity < 20/32. A total of 5158 eligible persons were enumerated and 4738 (91.9%) examined. Prevalence of presenting visual impairment < 20/63 to 20/200 in the better eye was 29.3% (95% confidence interval [CI]: 27.5-31.2) and 13.5% (95% CI: 12.0-14.9) with best correction. The prevalence of presenting bilateral blindness (< 20/200) was 6.9% (95% CI: 5.7-8.1), and 3.1% (95% CI: 2.5-3.7) with best correction. Presenting and best-corrected blindness were both associated with older age and illiteracy; gender and rural/urban residence were not significant. Cataract in one or both eyes was the main cause of bilateral blindness (82.6%), followed by retinal disorders (8.9%). Cataract (50.3%) and refractive error (35.4%) were the main causes in eyes with vision acuity < 20/63 to 20/200, and refractive error (86.6%) in eyes with acuity < 20/32 to 20/63. Visual impairment and blindness is a significant problem among the elderly in <span class="hlt">Gujarat</span>. Despite a reportedly high CSR, cataract remains the predominant cause of blindness.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_17 --> <div id="page_18" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="341"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://dx.doi.org/10.4401/ag-5364','USGSPUBS'); return false;" href="http://dx.doi.org/10.4401/ag-5364"><span>Twitter <span class="hlt">earthquake</span> detection: <span class="hlt">Earthquake</span> monitoring in a social world</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Earle, Paul S.; Bowden, Daniel C.; Guy, Michelle R.</p> <p>2011-01-01</p> <p>The U.S. Geological Survey (USGS) is investigating how the social networking site Twitter, a popular service for sending and receiving short, public text messages, can augment USGS <span class="hlt">earthquake</span> response products and the delivery of hazard information. Rapid detection and qualitative assessment of shaking events are possible because people begin sending public Twitter messages (tweets) with in tens of seconds after feeling shaking. Here we present and evaluate an <span class="hlt">earthquake</span> detection procedure that relies solely on Twitter data. A tweet-frequency time series constructed from tweets containing the word "<span class="hlt">earthquake</span>" clearly shows large peaks correlated with the origin times of widely felt events. To identify possible <span class="hlt">earthquakes</span>, we use a short-term-average, long-term-average algorithm. When tuned to a moderate sensitivity, the detector finds 48 globally-distributed <span class="hlt">earthquakes</span> with only two false triggers in five months of data. The number of detections is small compared to the 5,175 <span class="hlt">earthquakes</span> in the USGS global <span class="hlt">earthquake</span> catalog for the same five-month time period, and no accurate location or magnitude can be assigned based on tweet data alone. However, Twitter <span class="hlt">earthquake</span> detections are not without merit. The detections are generally caused by widely felt events that are of more immediate interest than those with no human impact. The detections are also fast; about 75% occur within two minutes of the origin time. This is considerably faster than seismographic detections in poorly instrumented regions of the world. The tweets triggering the detections also provided very short first-impression narratives from people who experienced the shaking.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMNH21A3829M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMNH21A3829M"><span>Village Level Tsunami Threat Maps for Tamil Nadu, SE Coast of <span class="hlt">India</span>: Numerical Modeling Technique</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>MP, J.; Kulangara Madham Subrahmanian, D.; V, R. M.</p> <p>2014-12-01</p> <p>The Indian Ocean tsunami (IOT) devastated several countries of North Indian Ocean. <span class="hlt">India</span> is one of the worst affected countries after Indonesia and Sri Lanka. In <span class="hlt">India</span>, Tamil Nadu suffered maximum with fatalities exceeding 8,000 people. Historical records show that tsunami has invaded the shores of Tamil Nadu in the past and has made people realize that the tsunami threat looms over Tamil Nadu and it is necessary to evolve strategies for tsunami threat management. The IOT has brought to light that tsunami inundation and runup varied within short distances and for the disaster management for tsunami, large scale maps showing areas that are likely to be affected by future tsunami are identified. Therefore threat assessment for six villages including Mamallapuram (also called Mahabalipuram) which is famous for its rock-cut temples, from the northern part of Tamil Nadu state of <span class="hlt">India</span> has been carried out and threat maps categorizing the coast into areas of different degree of threat are prepared. The threat was assessed by numerical modeling using TUNAMI N2 code considering different tsunamigenic sources along the Andaman - Sumatra trench. While GEBCO and C-Map data was used for bathymetry and for land elevation data was generated by RTK - GPS survey for a distance of 1 km from shore and SRTM for the inland areas. The model results show that in addition to the Sumatra source which generated the IOT in 2004, <span class="hlt">earthquakes</span> originating in Car Nicobar and North Andaman can inflict more damage. The North Andaman source can generate a massive tsunami and an <span class="hlt">earthquake</span> of magnitude more than Mw 9 can not only affect Tamil Nadu but also entire south east coast of <span class="hlt">India</span>. The runup water level is used to demarcate the tsunami threat zones in the villages using GIS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70048463','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70048463"><span>Crustal <span class="hlt">earthquake</span> triggering by pre-historic great <span class="hlt">earthquakes</span> on subduction zone thrusts</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Sherrod, Brian; Gomberg, Joan</p> <p>2014-01-01</p> <p>Triggering of <span class="hlt">earthquakes</span> on upper plate faults during and shortly after recent great (M>8.0) subduction thrust <span class="hlt">earthquakes</span> raises concerns about <span class="hlt">earthquake</span> triggering following Cascadia subduction zone <span class="hlt">earthquakes</span>. Of particular regard to Cascadia was the previously noted, but only qualitatively identified, clustering of M>~6.5 crustal <span class="hlt">earthquakes</span> in the Puget Sound region between about 1200–900 cal yr B.P. and the possibility that this was triggered by a great Cascadia thrust subduction thrust <span class="hlt">earthquake</span>, and therefore portends future such clusters. We confirm quantitatively the extraordinary nature of the Puget Sound region crustal <span class="hlt">earthquake</span> clustering between 1200–900 cal yr B.P., at least over the last 16,000. We conclude that this cluster was not triggered by the penultimate, and possibly full-margin, great Cascadia subduction thrust <span class="hlt">earthquake</span>. However, we also show that the paleoseismic record for Cascadia is consistent with conclusions of our companion study of the global modern record outside Cascadia, that M>8.6 subduction thrust events have a high probability of triggering at least one or more M>~6.5 crustal <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5644303','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5644303"><span>Retrospective analysis of clinical information in Crimean-Congo haemorrhagic fever patients: 2014-2015, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Mourya, Devendra T.; Viswanathan, Rajlakshmi; Jadhav, Santosh Kumar; Yadav, Pragya D.; Basu, Atanu; Chadha, Mandeep S.</p> <p>2017-01-01</p> <p>Background & objectives: Differential diagnosis of Crimean-Congo haemorrhagic fever (CCHF) from other acute febrile illnesses with haemorrhagic manifestation is challenging in <span class="hlt">India</span>. Nosocomial infection is a significant mode of transmission due to exposure of healthcare workers to blood and body fluids of infected patients. Being a risk group 4 virus, laboratory confirmation of infection is not widely available. In such a situation, early identification of potential CCHF patients would be useful in limiting the spread of the disease. The objective of this study was to retrospectively analyse clinical and laboratory findings of CCHF patients that might be useful in early detection of a CCHF case in limited resource settings. Methods: Retrospective analysis of clinical and laboratory data of patients suspected to have CCHF referred for diagnosis from <span class="hlt">Gujarat</span> and Rajasthan States of <span class="hlt">India</span> (2014-2015) was done. Samples were tested using CCHF-specific real time reverse transcription (RT)-PCR and IgM ELISA. Results: Among the 69 patients referred, 21 were laboratory confirmed CCHF cases of whom nine had a history of occupational exposure. No clustering of cases was noted. Platelet count cut-off for detection of positive cases by receiver operating characteristic curve was 21.5×10[9]/l with sensitivity 82.4 per cent and specificity 82.1 per cent. Melaena was a significant clinical presentation in confirmed positive CCHF patients. Interpretation & conclusions: The study findings suggest that in endemic areas thrombocytopenia and melaena may be early indicators of CCHF. Further studies are needed to confirm these findings. PMID:28948959</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JAESc.159....1P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JAESc.159....1P"><span>Microseismicity, tectonics and seismic potential in the Western Himalayan segment, NW Himalaya, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Parija, Mahesh Prasad; Kumar, Sushil; Tiwari, V. M.; Rao, N. Purnachandra; Kumar, Narendra; Biswal, Shubhasmita; Singh, Ishwar</p> <p>2018-06-01</p> <p>The tectonics and seismic potential of the western Himalayan segment (30-33°N; 76-80°E) of the NW Himalayan (<span class="hlt">India</span>) region have been determined in this study. 423 <span class="hlt">earthquakes</span> were located in the NW Himalaya between 2004 and 2013 using more than 4495 P and 4453 S differential travel times to determine the moment tensors for 8 (Mw ≥ 4.0) of these <span class="hlt">earthquakes</span> using their broadband regional waveforms. The geometry of the Main Himalayan Thrust (MHT) plane which varies along the strike of the Himalaya in flat and ramp segments with a dip ranging between ∼2.5 to ∼4° to ∼19° below the Himalayan Frontal Thrust (HFT) in the south to the South Tibetan Detachment (STD) in the north has also been deduced in this study. Two crustal ramps were reported in this study with a depth variance below the Main Central Thrust (MCT) and to the South Tibetan Detachment (STD) between 12 to 22 km and 28 to 40 km depth respectively. The estimated <span class="hlt">earthquake</span> potential prevailing in the western Himalayan seismic gap lying between the epicentral zone of the 1905 Kangra <span class="hlt">earthquake</span> and the 1975 Kinnaur <span class="hlt">earthquake</span> reveals that the total amount of energy released since the last great event is only a fraction (3-5%) of the accommodated energy i.e.1.1E+28 dyne-cm/yr. This suggests that if an <span class="hlt">earthquake</span> hits this NW Himalayan segment in the future, its magnitude might be around Mw ≥ 8.0.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23703433','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23703433"><span>Review of the bioenvironmental methods for malaria control with special reference to the use of larvivorous fishes and composite fish culture in central <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kant, Rajni; Haq, S; Srivastava, H C; Sharma, V P</p> <p>2013-03-01</p> <p>Mosquito control with the use of insecticides is faced with the challenges of insecticide resistance in disease vectors, community refusal, their high cost, operational difficulties, and environmental concern. In view of this, integrated vector control strategies with the use of larvivorous fishes such as Guppy (Poecilia reticulata) and Gambusia (G. affinis) as biological control agents were used in controlling mosquito breeding in different types of breeding places such as intradomestic containers, various types of wells, rice-fields, pools, ponds and elsewhere in malaria prone rural areas of central <span class="hlt">Gujarat</span>. Attempts were also made to demonstrate composite fish culture in unused abandoned village ponds by culturing Guppy along with the food fishes such as Rohu (Labeo rohita), Catla (Catla catla) and Mrigal (Cirrhinus mrigala). Income generated from these ponds through sale of fishes was utilized for mosquito control and village development. The technology was later adopted by the villagers themselves and food fish culture was practised in 23 ponds which generated an income of Rs 1,02,50,992 between 1985 and 2008. The number of villages increased from 13 to 23 in 2008 and there was also gradual increase of income from Rs 3,66,245 in 1985-90 to Rs 55,06,127 in 2002-08 block. It is concluded that larvivorous fishes can be useful tool in controlling mosquito breeding in certain situations and their use along with composite fish culture may also generate income to make the programme self-sustainable.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1063732','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1063732"><span>Using Third-Party Inspectors in Building Energy Codes Enforcement in <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Yu, Sha; Evans, Meredydd; Kumar, Pradeep</p> <p></p> <p><span class="hlt">India</span> is experiencing fast income growth and urbanization, and this leads to unprecedented increases in demand for building energy services and resulting energy consumption. In response to rapid growth in building energy use, the Government of <span class="hlt">India</span> issued the Energy Conservation Building Code (ECBC) in 2007, which is consistent with and based on the 2001 Energy Conservation Act. ECBC implementation has been voluntary since its enactment and a few states have started to make progress towards mandatory implementation. Rajasthan is the first state in <span class="hlt">India</span> to adopt ECBC as a mandatory code. The State adopted ECBC with minor additions onmore » March 28, 2011 through a stakeholder process; it became mandatory in Rajasthan on September 28, 2011. Tamil Nadu, <span class="hlt">Gujarat</span>, and Andhra Pradesh have started to draft an implementation roadmap and build capacity for its implementation. The Bureau of Energy Efficiency (BEE) plans to encourage more states to adopt ECBC in the near future, including Haryana, Uttar Pradesh, Karnataka, Maharashtra, West Bengal, and Delhi. Since its inception, <span class="hlt">India</span> has applied the code on a voluntary basis, but the Government of <span class="hlt">India</span> is developing a strategy to mandate compliance. Implementing ECBC requires coordination between the Ministry of Power and the Ministry of Urban Development at the national level as well as interdepartmental coordination at the state level. One challenge is that the Urban Local Bodies (ULBs), the enforcement entities of building by-laws, lack capacity to implement ECBC effectively. For example, ULBs in some states might find the building permitting procedures to be too complex; in other cases, lack of awareness and technical knowledge on ECBC slows down the amendment of local building by-laws as well as ECBC implementation. The intent of this white paper is to share with Indian decision-makers code enforcement approaches: through code officials, third-party inspectors, or a hybrid approach. Given the limited capacity and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3881738','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3881738"><span>Impact of <span class="hlt">earthquakes</span> on sex ratio at birth: Eastern Marmara <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Doğer, Emek; Çakıroğlu, Yiğit; Köpük, Şule Yıldırım; Ceylan, Yasin; Şimşek, Hayal Uzelli; Çalışkan, Eray</p> <p>2013-01-01</p> <p>Objective: Previous reports suggest that maternal exposure to acute stress related to <span class="hlt">earthquakes</span> affects the sex ratio at birth. Our aim was to examine the change in sex ratio at birth after Eastern Marmara <span class="hlt">earthquake</span> disasters. Material and Methods: This study was performed using the official birth statistics from January 1997 to December 2002 – before and after 17 August 1999, the date of the Golcuk <span class="hlt">Earthquake</span> – supplied from the Turkey Statistics Institute. The secondary sex ratio was expressed as the male proportion at birth, and the ratio of both affected and unaffected areas were calculated and compared on a monthly basis using data from gender with using the Chi-square test. Results: We observed significant decreases in the secondary sex ratio in the 4th and 8th months following an <span class="hlt">earthquake</span> in the affected region compared to the unaffected region (p= 0.001 and p= 0.024). In the <span class="hlt">earthquake</span> region, the decrease observed in the secondary sex ratio during the 8th month after an <span class="hlt">earthquake</span> was specific to the period after the <span class="hlt">earthquake</span>. Conclusion: Our study indicated a significant reduction in the secondary sex ratio after an <span class="hlt">earthquake</span>. With these findings, events that cause sudden intense stress such as <span class="hlt">earthquakes</span> can have an effect on the sex ratio at birth. PMID:24592082</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/6783055-large-scale-earthquake-countermeasures-act-earthquake-prediction-council-japan','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/6783055-large-scale-earthquake-countermeasures-act-earthquake-prediction-council-japan"><span>Large-Scale <span class="hlt">Earthquake</span> Countermeasures Act and the <span class="hlt">Earthquake</span> Prediction Council in Japan</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Rikitake, T.</p> <p>1979-08-07</p> <p>The Large-Scale <span class="hlt">Earthquake</span> Countermeasures Act was enacted in Japan in December 1978. This act aims at mitigating <span class="hlt">earthquake</span> hazards by designating an area to be an area under intensified measures against <span class="hlt">earthquake</span> disaster, such designation being based on long-term <span class="hlt">earthquake</span> prediction information, and by issuing an <span class="hlt">earthquake</span> warnings statement based on imminent prediction information, when possible. In an emergency case as defined by the law, the prime minister will be empowered to take various actions which cannot be taken at ordinary times. For instance, he may ask the Self-Defense Force to come into the <span class="hlt">earthquake</span>-threatened area before the <span class="hlt">earthquake</span> occurrence.more » A Prediction Council has been formed in order to evaluate premonitory effects that might be observed over the Tokai area, which was designated an area under intensified measures against <span class="hlt">earthquake</span> disaster some time in June 1979. An extremely dense observation network has been constructed over the area.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.bssaonline.org/content/84/3/892.abstract','USGSPUBS'); return false;" href="http://www.bssaonline.org/content/84/3/892.abstract"><span>Foreshocks, aftershocks, and <span class="hlt">earthquake</span> probabilities: Accounting for the landers <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Jones, Lucile M.</p> <p>1994-01-01</p> <p>The equation to determine the probability that an <span class="hlt">earthquake</span> occurring near a major fault will be a foreshock to a mainshock on that fault is modified to include the case of aftershocks to a previous <span class="hlt">earthquake</span> occurring near the fault. The addition of aftershocks to the background seismicity makes its less probable that an <span class="hlt">earthquake</span> will be a foreshock, because nonforeshocks have become more common. As the aftershocks decay with time, the probability that an <span class="hlt">earthquake</span> will be a foreshock increases. However, fault interactions between the first mainshock and the major fault can increase the long-term probability of a characteristic <span class="hlt">earthquake</span> on that fault, which will, in turn, increase the probability that an event is a foreshock, compensating for the decrease caused by the aftershocks.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22387647','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22387647"><span>Emergence of viral hemorrhagic fevers: is recent outbreak of Crimean Congo Hemorrhagic Fever in <span class="hlt">India</span> an indication?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lahariya, C; Goel, M K; Kumar, A; Puri, M; Sodhi, A</p> <p>2012-01-01</p> <p>The emerging and re-emerging diseases are posing a great health risk for the last few years. One such category of diseases is viral haemorrhagic fevers (VHFs), which have emerged in the new territories, worldwide. Crimean Congo Hemorrhagic Fever (CCHF) cases, for the first time in <span class="hlt">India</span>, were reported from <span class="hlt">Gujarat</span>, in January 2011. The emergence of diseases not reported earlier, pose great economic and social challenge, burden health system, and create panic reaction. Nonetheless, with recent experience in control of epidemic diseases, and advances in basic scientific knowledge; the public health community is better prepared for these unexpected events. This review provides information to physicians on CCHF for managing outbreak, and identifies public health measures to prevent emergence and re-emergence of VHFs (including CCHF) in future. The authors suggest that though, there are a few challenging and unanswered questions, the public health preparedness still remains the key to control emerging and re-emerging diseases. The countries where virus activities have been reported need to be prepared accordingly.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/2014/1025/b/pdf/ofr2014-1025b.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/2014/1025/b/pdf/ofr2014-1025b.pdf"><span><span class="hlt">Earthquake</span> catalog for estimation of maximum <span class="hlt">earthquake</span> magnitude, Central and Eastern United States: Part B, historical <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Wheeler, Russell L.</p> <p>2014-01-01</p> <p>Computation of probabilistic <span class="hlt">earthquake</span> hazard requires an estimate of Mmax: the moment magnitude of the largest <span class="hlt">earthquake</span> that is thought to be possible within a specified geographic region. The region specified in this report is the Central and Eastern United States and adjacent Canada. Parts A and B of this report describe the construction of a global catalog of moderate to large <span class="hlt">earthquakes</span> that occurred worldwide in tectonic analogs of the Central and Eastern United States. Examination of histograms of the magnitudes of these <span class="hlt">earthquakes</span> allows estimation of Central and Eastern United States Mmax. The catalog and Mmax estimates derived from it are used in the 2014 edition of the U.S. Geological Survey national seismic-hazard maps. Part A deals with prehistoric <span class="hlt">earthquakes</span>, and this part deals with historical events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4260540','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4260540"><span><span class="hlt">Earthquake</span> and tsunami forecasts: Relation of slow slip events to subsequent <span class="hlt">earthquake</span> rupture</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Dixon, Timothy H.; Jiang, Yan; Malservisi, Rocco; McCaffrey, Robert; Voss, Nicholas; Protti, Marino; Gonzalez, Victor</p> <p>2014-01-01</p> <p>The 5 September 2012 Mw 7.6 <span class="hlt">earthquake</span> on the Costa Rica subduction plate boundary followed a 62-y interseismic period. High-precision GPS recorded numerous slow slip events (SSEs) in the decade leading up to the <span class="hlt">earthquake</span>, both up-dip and down-dip of seismic rupture. Deeper SSEs were larger than shallower ones and, if characteristic of the interseismic period, release most locking down-dip of the <span class="hlt">earthquake</span>, limiting down-dip rupture and <span class="hlt">earthquake</span> magnitude. Shallower SSEs were smaller, accounting for some but not all interseismic locking. One SSE occurred several months before the <span class="hlt">earthquake</span>, but changes in Mohr–Coulomb failure stress were probably too small to trigger the <span class="hlt">earthquake</span>. Because many SSEs have occurred without subsequent rupture, their individual predictive value is limited, but taken together they released a significant amount of accumulated interseismic strain before the <span class="hlt">earthquake</span>, effectively defining the area of subsequent seismic rupture (rupture did not occur where slow slip was common). Because <span class="hlt">earthquake</span> magnitude depends on rupture area, this has important implications for <span class="hlt">earthquake</span> hazard assessment. Specifically, if this behavior is representative of future <span class="hlt">earthquake</span> cycles and other subduction zones, it implies that monitoring SSEs, including shallow up-dip events that lie offshore, could lead to accurate forecasts of <span class="hlt">earthquake</span> magnitude and tsunami potential. PMID:25404327</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25404327','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25404327"><span><span class="hlt">Earthquake</span> and tsunami forecasts: relation of slow slip events to subsequent <span class="hlt">earthquake</span> rupture.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dixon, Timothy H; Jiang, Yan; Malservisi, Rocco; McCaffrey, Robert; Voss, Nicholas; Protti, Marino; Gonzalez, Victor</p> <p>2014-12-02</p> <p>The 5 September 2012 M(w) 7.6 <span class="hlt">earthquake</span> on the Costa Rica subduction plate boundary followed a 62-y interseismic period. High-precision GPS recorded numerous slow slip events (SSEs) in the decade leading up to the <span class="hlt">earthquake</span>, both up-dip and down-dip of seismic rupture. Deeper SSEs were larger than shallower ones and, if characteristic of the interseismic period, release most locking down-dip of the <span class="hlt">earthquake</span>, limiting down-dip rupture and <span class="hlt">earthquake</span> magnitude. Shallower SSEs were smaller, accounting for some but not all interseismic locking. One SSE occurred several months before the <span class="hlt">earthquake</span>, but changes in Mohr-Coulomb failure stress were probably too small to trigger the <span class="hlt">earthquake</span>. Because many SSEs have occurred without subsequent rupture, their individual predictive value is limited, but taken together they released a significant amount of accumulated interseismic strain before the <span class="hlt">earthquake</span>, effectively defining the area of subsequent seismic rupture (rupture did not occur where slow slip was common). Because <span class="hlt">earthquake</span> magnitude depends on rupture area, this has important implications for <span class="hlt">earthquake</span> hazard assessment. Specifically, if this behavior is representative of future <span class="hlt">earthquake</span> cycles and other subduction zones, it implies that monitoring SSEs, including shallow up-dip events that lie offshore, could lead to accurate forecasts of <span class="hlt">earthquake</span> magnitude and tsunami potential.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/fs/2012/3014/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/fs/2012/3014/"><span>Understanding <span class="hlt">earthquake</span> hazards in urban areas - Evansville Area <span class="hlt">Earthquake</span> Hazards Mapping Project</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Boyd, Oliver S.</p> <p>2012-01-01</p> <p>The region surrounding Evansville, Indiana, has experienced minor damage from <span class="hlt">earthquakes</span> several times in the past 200 years. Because of this history and the proximity of Evansville to the Wabash Valley and New Madrid seismic zones, there is concern among nearby communities about hazards from <span class="hlt">earthquakes</span>. <span class="hlt">Earthquakes</span> currently cannot be predicted, but scientists can estimate how strongly the ground is likely to shake as a result of an <span class="hlt">earthquake</span> and are able to design structures to withstand this estimated ground shaking. <span class="hlt">Earthquake</span>-hazard maps provide one way of conveying such information and can help the region of Evansville prepare for future <span class="hlt">earthquakes</span> and reduce <span class="hlt">earthquake</span>-caused loss of life and financial and structural loss. The Evansville Area <span class="hlt">Earthquake</span> Hazards Mapping Project (EAEHMP) has produced three types of hazard maps for the Evansville area: (1) probabilistic seismic-hazard maps show the ground motion that is expected to be exceeded with a given probability within a given period of time; (2) scenario ground-shaking maps show the expected shaking from two specific scenario <span class="hlt">earthquakes</span>; (3) liquefaction-potential maps show how likely the strong ground shaking from the scenario <span class="hlt">earthquakes</span> is to produce liquefaction. These maps complement the U.S. Geological Survey's National Seismic Hazard Maps but are more detailed regionally and take into account surficial geology, soil thickness, and soil stiffness; these elements greatly affect ground shaking.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017Tecto..36.2407M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Tecto..36.2407M"><span>The 2015 Mw7.2 Sarez Strike-Slip <span class="hlt">Earthquake</span> in the Pamir Interior: Response to the Underthrusting of <span class="hlt">India</span>'s Western Promontory</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Metzger, Sabrina; Schurr, Bernd; Ratschbacher, Lothar; Sudhaus, Henriette; Kufner, Sofia-Katerina; Schöne, Tilo; Zhang, Yong; Perry, Mason; Bendick, Rebecca</p> <p>2017-11-01</p> <p>The Pamir orogen, Central Asia, is the result of the ongoing northward advance of the Indian continent causing shortening inside Asia. Geodetic and seismic data place the most intense deformation along the northern rim of the Pamir, but the recent 7 December 2015, Mw7.2 Sarez <span class="hlt">earthquake</span> occurred in the Pamir's interior. We present a distributed slip model of this <span class="hlt">earthquake</span> using coseismic geodetic data and postseismic field observations. The <span class="hlt">earthquake</span> ruptured an ˜80 km long, subvertical, sinistral fault consisting of three right-stepping segments from the surface to ˜30 km depth with a maximum slip of three meters in the upper 10 km of the crust. The coseismic slip model agrees well with en échelon secondary surface breaks that are partly influenced by liquefaction-induced mass movements. These structures reveal up to 2 m of sinistral offset along the northern, low-offset segment of modeled rupture. The 2015 event initiated close to the presumed epicenter of the 1911 Mw˜7.3 Lake Sarez <span class="hlt">earthquake</span>, which had a similar strike-slip mechanism. These <span class="hlt">earthquakes</span> highlight the importance of NE trending sinistral faults in the active tectonics of the Pamir. Strike-slip deformation accommodates shear between the rapidly northward moving eastern Pamir and the Tajik basin in the west and is part of the westward (lateral) extrusion of thickened Pamir plateau crust into the Tajik basin. The Sarez-Karakul fault system and the two large Sarez <span class="hlt">earthquakes</span> likely are crustal expressions of the underthrusting of the northwestern leading edge of the Indian mantle lithosphere beneath the Pamir.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70116796','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70116796"><span>Continuing megathrust <span class="hlt">earthquake</span> potential in Chile after the 2014 Iquique <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hayes, Gavin P.; Herman, Matthew W.; Barnhart, William D.; Furlong, Kevin P.; Riquelme, Sebástian; Benz, Harley M.; Bergman, Eric; Barrientos, Sergio; Earle, Paul S.; Samsonov, Sergey</p> <p>2014-01-01</p> <p>The seismic gap theory identifies regions of elevated hazard based on a lack of recent seismicity in comparison with other portions of a fault. It has successfully explained past <span class="hlt">earthquakes</span> (see, for example, ref. 2) and is useful for qualitatively describing where large <span class="hlt">earthquakes</span> might occur. A large <span class="hlt">earthquake</span> had been expected in the subduction zone adjacent to northern Chile which had not ruptured in a megathrust <span class="hlt">earthquake</span> since a M ~8.8 event in 1877. On 1 April 2014 a M 8.2 <span class="hlt">earthquake</span> occurred within this seismic gap. Here we present an assessment of the seismotectonics of the March–April 2014 Iquique sequence, including analyses of <span class="hlt">earthquake</span> relocations, moment tensors, finite fault models, moment deficit calculations and cumulative Coulomb stress transfer. This ensemble of information allows us to place the sequence within the context of regional seismicity and to identify areas of remaining and/or elevated hazard. Our results constrain the size and spatial extent of rupture, and indicate that this was not the <span class="hlt">earthquake</span> that had been anticipated. Significant sections of the northern Chile subduction zone have not ruptured in almost 150 years, so it is likely that future megathrust <span class="hlt">earthquakes</span> will occur to the south and potentially to the north of the 2014 Iquique sequence.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25119028','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25119028"><span>Continuing megathrust <span class="hlt">earthquake</span> potential in Chile after the 2014 Iquique <span class="hlt">earthquake</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hayes, Gavin P; Herman, Matthew W; Barnhart, William D; Furlong, Kevin P; Riquelme, Sebástian; Benz, Harley M; Bergman, Eric; Barrientos, Sergio; Earle, Paul S; Samsonov, Sergey</p> <p>2014-08-21</p> <p>The seismic gap theory identifies regions of elevated hazard based on a lack of recent seismicity in comparison with other portions of a fault. It has successfully explained past <span class="hlt">earthquakes</span> (see, for example, ref. 2) and is useful for qualitatively describing where large <span class="hlt">earthquakes</span> might occur. A large <span class="hlt">earthquake</span> had been expected in the subduction zone adjacent to northern Chile, which had not ruptured in a megathrust <span class="hlt">earthquake</span> since a M ∼8.8 event in 1877. On 1 April 2014 a M 8.2 <span class="hlt">earthquake</span> occurred within this seismic gap. Here we present an assessment of the seismotectonics of the March-April 2014 Iquique sequence, including analyses of <span class="hlt">earthquake</span> relocations, moment tensors, finite fault models, moment deficit calculations and cumulative Coulomb stress transfer. This ensemble of information allows us to place the sequence within the context of regional seismicity and to identify areas of remaining and/or elevated hazard. Our results constrain the size and spatial extent of rupture, and indicate that this was not the <span class="hlt">earthquake</span> that had been anticipated. Significant sections of the northern Chile subduction zone have not ruptured in almost 150 years, so it is likely that future megathrust <span class="hlt">earthquakes</span> will occur to the south and potentially to the north of the 2014 Iquique sequence.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.geotimes.org/mar05/feature_eqprediction.html','USGSPUBS'); return false;" href="http://www.geotimes.org/mar05/feature_eqprediction.html"><span><span class="hlt">Earthquakes</span>: Predicting the unpredictable?</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hough, Susan E.</p> <p>2005-01-01</p> <p>The <span class="hlt">earthquake</span> prediction pendulum has swung from optimism in the 1970s to rather extreme pessimism in the 1990s. Earlier work revealed evidence of possible <span class="hlt">earthquake</span> precursors: physical changes in the planet that signal that a large <span class="hlt">earthquake</span> is on the way. Some respected <span class="hlt">earthquake</span> scientists argued that <span class="hlt">earthquakes</span> are likewise fundamentally unpredictable. The fate of the Parkfield prediction experiment appeared to support their arguments: A moderate <span class="hlt">earthquake</span> had been predicted along a specified segment of the central San Andreas fault within five years of 1988, but had failed to materialize on schedule. At some point, however, the pendulum began to swing back. Reputable scientists began using the "P-word" in not only polite company, but also at meetings and even in print. If the optimism regarding <span class="hlt">earthquake</span> prediction can be attributed to any single cause, it might be scientists' burgeoning understanding of the <span class="hlt">earthquake</span> cycle.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22410538','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22410538"><span>Comparison of two large <span class="hlt">earthquakes</span>: the 2008 Sichuan <span class="hlt">Earthquake</span> and the 2011 East Japan <span class="hlt">Earthquake</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Otani, Yuki; Ando, Takayuki; Atobe, Kaori; Haiden, Akina; Kao, Sheng-Yuan; Saito, Kohei; Shimanuki, Marie; Yoshimoto, Norifumi; Fukunaga, Koichi</p> <p>2012-01-01</p> <p>Between August 15th and 19th, 2011, eight 5th-year medical students from the Keio University School of Medicine had the opportunity to visit the Peking University School of Medicine and hold a discussion session titled "What is the most effective way to educate people for survival in an acute disaster situation (before the mental health care stage)?" During the session, we discussed the following six points: basic information regarding the Sichuan <span class="hlt">Earthquake</span> and the East Japan <span class="hlt">Earthquake</span>, differences in preparedness for <span class="hlt">earthquakes</span>, government actions, acceptance of medical rescue teams, <span class="hlt">earthquake</span>-induced secondary effects, and media restrictions. Although comparison of the two <span class="hlt">earthquakes</span> was not simple, we concluded that three major points should be emphasized to facilitate the most effective course of disaster planning and action. First, all relevant agencies should formulate emergency plans and should supply information regarding the emergency to the general public and health professionals on a normal basis. Second, each citizen should be educated and trained in how to minimize the risks from <span class="hlt">earthquake</span>-induced secondary effects. Finally, the central government should establish a single headquarters responsible for command, control, and coordination during a natural disaster emergency and should centralize all powers in this single authority. We hope this discussion may be of some use in future natural disasters in China, Japan, and worldwide.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_18 --> <div id="page_19" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="361"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JIEIA..97..359K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JIEIA..97..359K"><span>Design of Visco-Elastic Dampers for RC Frame for Site-Specific <span class="hlt">Earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kamatchi, P.; Rama Raju, K.; Ravisankar, K.; Iyer, Nagesh R.</p> <p>2016-12-01</p> <p>Number of Reinforced Concrete (RC) framed buildings have got damaged at Ahmedabad city, <span class="hlt">India</span> located at about 240 km away from epicenter during January 2001, 7.6 moment magnitude (Mw) Bhuj <span class="hlt">earthquake</span>. In the present study, two dimensional nonlinear time history dynamic analyses of a typical 13 storey frame assumed to be located at Ahmedabad is carried out with the rock level and surface level site-specific ground motion for scenario <span class="hlt">earthquake</span> of Mw 7.6 from Bhuj. Artificial ground motions are generated using extended finite source stochastic model with seismological parameters reported in literature for 2001 Bhuj <span class="hlt">earthquake</span>. Surface level ground motions are obtained for a typical soil profile of 100 m depth reported in literature through one dimensional equivalent linear wave propagation analyses. From the analyses, failure of frame is observed for surface level ground motions which indicates that, in addition to the in-adequacy of the cross sections and reinforcement of the RC members of the frame chosen, the rich energy content of the surface level ground motion near the fundamental time period of the frame has also contributed for the failure of frame. As a part of retrofitting measure, five Visco-elastic Dampers (VED) in chevron bracing are added to frame. For the frame considered in the present study, provision of VED is found to be effective to mitigate damage for the soil site considered.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018Tectp.726...43M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018Tectp.726...43M"><span>Magnetotelluric study to characterize Kachchh Mainland Fault (KMF) and Katrol Hill Fault (KHF) in the western part of Kachchh region of <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mohan, Kapil; Chaudhary, Peush; Patel, Pruthul; Chaudhary, B. S.; Chopra, Sumer</p> <p>2018-02-01</p> <p>The Kachchh Mainland Fault (KMF) is a major E-W trending fault in the Kachchh region of <span class="hlt">Gujarat</span> extending >150 km from Lakhpat village in the west to the Bhachau town in the east. The Katrol Hill Fault (KHF) is an E-W trending intrabasinal fault located in the central region of Kachchh Basin and the south of KMF. The western parts of both of the faults are characterized, and the sediment thickness has been estimated in the region using a Magnetotelluric (MT) survey at 17 sites along a 55 km long north-south profile with a site spacing of 2-3 km. The analysis reveals that the maximum sediment thickness is 2.3 km (Quaternary, Tertiary, and Mesozoic) in the region, out of which, the Mesozoic sediments feature a maximum thickness of 2 km. The estimated sediment thickness is found consistent with the thickness suggested by a deep borehole (depth approx. 2.5 km) drilled by Oil and Natural Gas Corporation (ONGC) at Nirona (Northern part of the study area). From 2-D inversion of the MT data, three conductive zones are identified from north to south. The first conductive zone is dipping nearly vertical down to 7-8 km depth. It becomes north-dipping below 8 km depth and is inferred as KMF. The second conductive zone is found steeply dipping into the southern limbs near Manjal village (28 km south of Nirona), which is inferred as the KHF. A vertical-dipping (down to 20 km depth) conductive zone has also been observed near Ulat village, located 16 km north of Manjal village and 12 km south of Nirona village. This conductive zone becomes listric north-dipping beyond 20 km depth. It is reported first time by a Geophysical survey in the region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70048668','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70048668"><span>Injection-induced <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Ellsworth, William L.</p> <p>2013-01-01</p> <p><span class="hlt">Earthquakes</span> in unusual locations have become an important topic of discussion in both North America and Europe, owing to the concern that industrial activity could cause damaging <span class="hlt">earthquakes</span>. It has long been understood that <span class="hlt">earthquakes</span> can be induced by impoundment of reservoirs, surface and underground mining, withdrawal of fluids and gas from the subsurface, and injection of fluids into underground formations. Injection-induced <span class="hlt">earthquakes</span> have, in particular, become a focus of discussion as the application of hydraulic fracturing to tight shale formations is enabling the production of oil and gas from previously unproductive formations. <span class="hlt">Earthquakes</span> can be induced as part of the process to stimulate the production from tight shale formations, or by disposal of wastewater associated with stimulation and production. Here, I review recent seismic activity that may be associated with industrial activity, with a focus on the disposal of wastewater by injection in deep wells; assess the scientific understanding of induced <span class="hlt">earthquakes</span>; and discuss the key scientific challenges to be met for assessing this hazard.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70169164','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70169164"><span><span class="hlt">Earthquakes</span>; January-February 1982</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1982-01-01</p> <p>In the United States, a number of <span class="hlt">earthquakes</span> occurred, but only minor damage was reported. Arkansas experienced a swarm of <span class="hlt">earthquakes</span> beginning on January 12. Canada experienced one of its strongest <span class="hlt">earthquakes</span> in a number of years on January 9; this <span class="hlt">earthquake</span> caused slight damage in Maine. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21949355','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21949355"><span>Results of the Regional <span class="hlt">Earthquake</span> Likelihood Models (RELM) test of <span class="hlt">earthquake</span> forecasts in California.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lee, Ya-Ting; Turcotte, Donald L; Holliday, James R; Sachs, Michael K; Rundle, John B; Chen, Chien-Chih; Tiampo, Kristy F</p> <p>2011-10-04</p> <p>The Regional <span class="hlt">Earthquake</span> Likelihood Models (RELM) test of <span class="hlt">earthquake</span> forecasts in California was the first competitive evaluation of forecasts of future <span class="hlt">earthquake</span> occurrence. Participants submitted expected probabilities of occurrence of M ≥ 4.95 <span class="hlt">earthquakes</span> in 0.1° × 0.1° cells for the period 1 January 1, 2006, to December 31, 2010. Probabilities were submitted for 7,682 cells in California and adjacent regions. During this period, 31 M ≥ 4.95 <span class="hlt">earthquakes</span> occurred in the test region. These <span class="hlt">earthquakes</span> occurred in 22 test cells. This seismic activity was dominated by <span class="hlt">earthquakes</span> associated with the M = 7.2, April 4, 2010, El Mayor-Cucapah <span class="hlt">earthquake</span> in northern Mexico. This <span class="hlt">earthquake</span> occurred in the test region, and 16 of the other 30 <span class="hlt">earthquakes</span> in the test region could be associated with it. Nine complete forecasts were submitted by six participants. In this paper, we present the forecasts in a way that allows the reader to evaluate which forecast is the most "successful" in terms of the locations of future <span class="hlt">earthquakes</span>. We conclude that the RELM test was a success and suggest ways in which the results can be used to improve future forecasts.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3189015','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3189015"><span>Results of the Regional <span class="hlt">Earthquake</span> Likelihood Models (RELM) test of <span class="hlt">earthquake</span> forecasts in California</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Lee, Ya-Ting; Turcotte, Donald L.; Holliday, James R.; Sachs, Michael K.; Rundle, John B.; Chen, Chien-Chih; Tiampo, Kristy F.</p> <p>2011-01-01</p> <p>The Regional <span class="hlt">Earthquake</span> Likelihood Models (RELM) test of <span class="hlt">earthquake</span> forecasts in California was the first competitive evaluation of forecasts of future <span class="hlt">earthquake</span> occurrence. Participants submitted expected probabilities of occurrence of M≥4.95 <span class="hlt">earthquakes</span> in 0.1° × 0.1° cells for the period 1 January 1, 2006, to December 31, 2010. Probabilities were submitted for 7,682 cells in California and adjacent regions. During this period, 31 M≥4.95 <span class="hlt">earthquakes</span> occurred in the test region. These <span class="hlt">earthquakes</span> occurred in 22 test cells. This seismic activity was dominated by <span class="hlt">earthquakes</span> associated with the M = 7.2, April 4, 2010, El Mayor–Cucapah <span class="hlt">earthquake</span> in northern Mexico. This <span class="hlt">earthquake</span> occurred in the test region, and 16 of the other 30 <span class="hlt">earthquakes</span> in the test region could be associated with it. Nine complete forecasts were submitted by six participants. In this paper, we present the forecasts in a way that allows the reader to evaluate which forecast is the most “successful” in terms of the locations of future <span class="hlt">earthquakes</span>. We conclude that the RELM test was a success and suggest ways in which the results can be used to improve future forecasts. PMID:21949355</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.S23A2741H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.S23A2741H"><span>Induced <span class="hlt">earthquake</span> during the 2016 Kumamoto <span class="hlt">earthquake</span> (Mw7.0): Importance of real-time shake monitoring for <span class="hlt">Earthquake</span> Early Warning</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hoshiba, M.; Ogiso, M.</p> <p>2016-12-01</p> <p>Sequence of the 2016 Kumamoto <span class="hlt">earthquakes</span> (Mw6.2 on April 14, Mw7.0 on April 16, and many aftershocks) caused a devastating damage at Kumamoto and Oita prefectures, Japan. During the Mw7.0 event, just after the direct S waves passing the central Oita, another M6 class event occurred there more than 80 km apart from the Mw7.0 event. The M6 event is interpreted as an induced <span class="hlt">earthquake</span>; but it brought stronger shaking at the central Oita than that from the Mw7.0 event. We will discuss the induced <span class="hlt">earthquake</span> from viewpoint of <span class="hlt">Earthquake</span> Early Warning. In terms of ground shaking such as PGA and PGV, the Mw7.0 event is much smaller than those of the M6 induced <span class="hlt">earthquake</span> at the central Oita (for example, 1/8 smaller at OIT009 station for PGA), and then it is easy to discriminate two events. However, PGD of the Mw7.0 is larger than that of the induced <span class="hlt">earthquake</span>, and its appearance is just before the occurrence of the induced <span class="hlt">earthquake</span>. It is quite difficult to recognize the induced <span class="hlt">earthquake</span> from displacement waveforms only, because the displacement is strongly contaminated by that of the preceding Mw7.0 event. In many methods of EEW (including current JMA EEW system), magnitude is used for prediction of ground shaking through Ground Motion Prediction Equation (GMPE) and the magnitude is often estimated from displacement. However, displacement magnitude does not necessarily mean the best one for prediction of ground shaking, such as PGA and PGV. In case of the induced <span class="hlt">earthquake</span> during the Kumamoto <span class="hlt">earthquake</span>, displacement magnitude could not be estimated because of the strong contamination. Actually JMA EEW system could not recognize the induced <span class="hlt">earthquake</span>. One of the important lessons we learned from eight years' operation of EEW is an issue of the multiple simultaneous <span class="hlt">earthquakes</span>, such as aftershocks of the 2011 Mw9.0 Tohoku <span class="hlt">earthquake</span>. Based on this lesson, we have proposed enhancement of real-time monitor of ground shaking itself instead of rapid estimation of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70168709','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70168709"><span><span class="hlt">Earthquakes</span>, September-October 1986</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1987-01-01</p> <p>There was one great <span class="hlt">earthquake</span> (8.0 and above) during this reporting period in the South Pacific in the Kermadec Islands. There were no major <span class="hlt">earthquakes</span> (7.0-7.9) but <span class="hlt">earthquake</span>-related deaths were reported in Greece and in El Salvador. There were no destrcutive <span class="hlt">earthquakes</span> in the United States.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/5323533-post-earthquake-recovery-natural-gas-systems-san-fernando-earthquake','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/5323533-post-earthquake-recovery-natural-gas-systems-san-fernando-earthquake"><span>Post <span class="hlt">earthquake</span> recovery in natural gas systems--1971 San Fernando <span class="hlt">Earthquake</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Johnson, W.T. Jr.</p> <p>1983-01-01</p> <p>In this paper a concise summary of the post <span class="hlt">earthquake</span> investigations for the 1971 San Fernando <span class="hlt">Earthquake</span> is presented. The effects of the <span class="hlt">earthquake</span> upon building and other above ground structures are briefly discussed. Then the damages and subsequent repairs in the natural gas systems are reported.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70169183','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70169183"><span><span class="hlt">Earthquakes</span>; July-August, 1978</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1979-01-01</p> <p><span class="hlt">Earthquake</span> activity during this period was about normal. Deaths from <span class="hlt">earthquakes</span> were reported from Greece and Guatemala. Three major <span class="hlt">earthquakes</span> (magnitude 7.0-7.9) occurred in Taiwan, Chile, and Costa Rica. In the United States, the most significant <span class="hlt">earthquake</span> was a magnitude 5.6 on August 13 in southern California. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.2710C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.2710C"><span>Improvements of the offshore <span class="hlt">earthquake</span> locations in the <span class="hlt">Earthquake</span> Early Warning System</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Ta-Yi; Hsu, Hsin-Chih</p> <p>2017-04-01</p> <p>Since 2014 the Earthworm Based <span class="hlt">Earthquake</span> Alarm Reporting (eBEAR) system has been operated and been used to issue warnings to schools. In 2015 the system started to provide warnings to the public in Taiwan via television and the cell phone. Online performance of the eBEAR system indicated that the average reporting times afforded by the system are approximately 15 and 28 s for inland and offshore <span class="hlt">earthquakes</span>, respectively. The eBEAR system in average can provide more warning time than the current EEW system (3.2 s and 5.5 s for inland and offshore <span class="hlt">earthquakes</span>, respectively). However, offshore <span class="hlt">earthquakes</span> were usually located poorly because only P-wave arrivals were used in the eBEAR system. Additionally, in the early stage of the <span class="hlt">earthquake</span> early warning system, only fewer stations are available. The poor station coverage may be a reason to answer why offshore <span class="hlt">earthquakes</span> are difficult to locate accurately. In the Geiger's inversion procedure of <span class="hlt">earthquake</span> location, we need to put an initial hypocenter and origin time into the location program. For the initial hypocenter, we defined some test locations on the offshore area instead of using the average of locations from triggered stations. We performed 20 programs concurrently running the Geiger's method with different pre-defined initial position to locate <span class="hlt">earthquakes</span>. We assume that if the program with the pre-defined initial position is close to the true <span class="hlt">earthquake</span> location, during the iteration procedure of the Geiger's method the processing time of this program should be less than others. The results show that using pre-defined locations for trial-hypocenter in the inversion procedure is able to improve the accurate of offshore <span class="hlt">earthquakes</span>. Especially for EEW system, in the initial stage of the EEW system, only use 3 or 5 stations to locate <span class="hlt">earthquakes</span> may lead to bad results because of poor station coverage. In this study, the pre-defined trial-locations provide a feasible way to improve the estimations of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUSMNH34A..02M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUSMNH34A..02M"><span>Megathrust <span class="hlt">earthquakes</span> in Central Chile: What is next after the Maule 2010 <span class="hlt">earthquake</span>?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Madariaga, R.</p> <p>2013-05-01</p> <p>The 27 February 2010 Maule <span class="hlt">earthquake</span> occurred in a well identified gap in the Chilean subduction zone. The event has now been studied in detail using both far-field, near field seismic and geodetic data, we will review this information gathered so far. The event broke a region that was much longer along strike than the gap left over from the 1835 Concepcion <span class="hlt">earthquake</span>, sometimes called the Darwin <span class="hlt">earthquake</span> because he was in the area when the <span class="hlt">earthquake</span> occurred and made many observations. Recent studies of contemporary documents by Udias et al indicate that the area broken by the Maule <span class="hlt">earthquake</span> in 2010 had previously broken by a similar <span class="hlt">earthquake</span> in 1751, but several events in the magnitude 8 range occurred in the area principally in 1835 already mentioned and, more recently on 1 December 1928 to the North and on 21 May 1960 (1 1/2 days before the big Chilean <span class="hlt">earthquake</span> of 1960). Currently the area of the 2010 <span class="hlt">earthquake</span> and the region immediately to the North is undergoing a very large increase in seismicity with numerous clusters of seismicity that move along the plate interface. Examination of the seismicity of Chile of the 18th and 19th century show that the region immediately to the North of the 2010 <span class="hlt">earthquake</span> broke in a very large megathrust event in July 1730. this is the largest known <span class="hlt">earthquake</span> in central Chile. The region where this event occurred has broken in many occasions with M 8 range <span class="hlt">earthquakes</span> in 1822, 1880, 1906, 1971 and 1985. Is it preparing for a new very large megathrust event? The 1906 <span class="hlt">earthquake</span> of Mw 8.3 filled the central part of the gap but it has broken again on several occasions in 1971, 1973 and 1985. The main question is whether the 1906 <span class="hlt">earthquake</span> relieved enough stresses from the 1730 rupture zone. Geodetic data shows that most of the region that broke in 1730 is currently almost fully locked from the northern end of the Maule <span class="hlt">earthquake</span> at 34.5°S to 30°S, near the southern end of the of the Mw 8.5 Atacama <span class="hlt">earthquake</span> of 11</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26139790','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26139790"><span>Socio-economic & demographic determinants of hypertension & knowledge, practices & risk behaviour of tribals in <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Laxmaiah, A; Meshram, I I; Arlappa, N; Balakrishna, N; Rao, K Mallikharjuna; Reddy, Ch Gal; Ravindranath, M; Kumar, Sharad; Kumar, Hari; Brahmam, G N V</p> <p>2015-05-01</p> <p>An increase in prevalence of hypertension has been observed in all ethnic groups in <span class="hlt">India</span>. The objective of the present study was to estimate prevalence and determinants of hypertension among tribals and their awareness, treatment practices and risk behaviours in nine States of <span class="hlt">India</span>. A community based cross-sectional study adopting multistage random sampling procedure was carried out. About 120 Integrated Tribal Development Authority villages were selected randomly from each State. From each village, 40 households were covered randomly. All men and women ≥ 20 yr of age in the selected households were included for various investigations. A total of 21141 men and 26260 women participated in the study. The prevalence of hypertension after age adjustment was 27.1 and 26.4 per cent among men and women, respectively. It was higher in the s0 tates of Odisha (50-54.4%) and Kerala (36.7-45%) and lowest in <span class="hlt">Gujarat</span> (7-11.5%). The risk of hypertension was 6-8 times higher in elderly people and 2-3 times in 35-59 yr compared with 20-34 yr. Only <10 per cent of men and women were known hypertensives and more than half on treatment (55-68%). Men with general and abdominal obesity were at 1.69 (CI: 1.43-2.01) and 2.42 (CI: 2.01-2.91) times higher risk of hypertension, respectively, while it was 2.03 (CI=1.77-2.33) and 2.35 (CI 2.12-2.60) times higher in women. Those using tobacco and consuming alcohol were at a higher risk of hypertension compared with the non users. The study revealed high prevalence of hypertension among tribals in <span class="hlt">India</span>. Age, literacy, physical activity, consumption of tobacco, alcohol and obesity were significantly associated with hypertension. Awareness and knowledge about hypertension and health seeking behaviour were low. Appropriate intervention strategies need to be adopted to increase awareness and treatment practices of hypertension among tribals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70169205','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70169205"><span><span class="hlt">Earthquakes</span>; March-April 1975</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1975-01-01</p> <p>There were no major <span class="hlt">earthquakes</span> (magnitude 7.0-7.9) in March or April; however, there were <span class="hlt">earthquake</span> fatalities in Chile, Iran, and Venezuela and approximately 35 <span class="hlt">earthquake</span>-related injuries were reported around the world. In the United States a magnitude 6.0 <span class="hlt">earthquake</span> struck the Idaho-Utah border region. Damage was estimated at about a million dollars. The shock was felt over a wide area and was the largest to hit the continental Untied States since the San Fernando <span class="hlt">earthquake</span> of February 1971. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://pubs.usgs.gov/gip/2007/42/','USGSPUBS'); return false;" href="http://pubs.usgs.gov/gip/2007/42/"><span>Protecting your family from <span class="hlt">earthquakes</span>: The seven steps to <span class="hlt">earthquake</span> safety</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Developed by American Red Cross, Asian Pacific Fund</p> <p>2007-01-01</p> <p>This book is provided here because of the importance of preparing for <span class="hlt">earthquakes</span> before they happen. Experts say it is very likely there will be a damaging San Francisco Bay Area <span class="hlt">earthquake</span> in the next 30 years and that it will strike without warning. It may be hard to find the supplies and services we need after this <span class="hlt">earthquake</span>. For example, hospitals may have more patients than they can treat, and grocery stores may be closed for weeks. You will need to provide for your family until help arrives. To keep our loved ones and our community safe, we must prepare now. Some of us come from places where <span class="hlt">earthquakes</span> are also common. However, the dangers of <span class="hlt">earthquakes</span> in our homelands may be very different than in the Bay Area. For example, many people in Asian countries die in major <span class="hlt">earthquakes</span> when buildings collapse or from big sea waves called tsunami. In the Bay Area, the main danger is from objects inside buildings falling on people. Take action now to make sure your family will be safe in an <span class="hlt">earthquake</span>. The first step is to read this book carefully and follow its advice. By making your home safer, you help make our community safer. Preparing for <span class="hlt">earthquakes</span> is important, and together we can make sure our families and community are ready. English version p. 3-13 Chinese version p. 14-24 Vietnamese version p. 25-36 Korean version p. 37-48</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PhDT.........4M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PhDT.........4M"><span>Evidence of the 1762 Arakan and Prior <span class="hlt">Earthquakes</span> in the Northern Sunda Subduction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mondal, Dhiman Ranjan</p> <p></p> <p> (Global Positioning System) survey documented 2 to 3 terraces. Among these three, the youngest terrace is possibly linked to the 1762 Arakan <span class="hlt">Earthquake</span> but the ages have not been verified. Modeling using the data obtained from Saint Martin's Island, Teknaf and other published articles (for the west coast of Teknaf) suggest a fault dipping at 10-15° to the northeast. The result of coseismic slip inversion shows 15-25 m of reverse slip along the Arakan rupture segment, which was accommodated by the upper plate failure. Based on our results from coral microatolls, terraces and the modeling study, this dissertation suggests that this segment of the Arakan collision zone has the potential to cause a future <span class="hlt">earthquake</span> of Mw > 8 which can produce a devastating effect to the inhabitants of Bangladesh, Myanmar and Eastern <span class="hlt">India</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T43B0691K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T43B0691K"><span>Structure and tectonics of the Main Himalayan Thrust and associated faults from recent <span class="hlt">earthquake</span> and seismic imaging studies using the NAMASTE array</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Karplus, M. S.; Pant, M.; Velasco, A. A.; Nabelek, J.; Kuna, V. M.; Sapkota, S. N.; Ghosh, A.; Mendoza, M.; Adhikari, L. B.; Klemperer, S. L.</p> <p>2017-12-01</p> <p>The <span class="hlt">India</span>-Eurasia collision zone presents a significant <span class="hlt">earthquake</span> hazard, as demonstrated by the recent, devastating April 25, 2015 M=7.8 Gorkha <span class="hlt">earthquake</span> and the following May 12, 2015 M=7.3 <span class="hlt">earthquake</span>. Important questions remain, including distinguishing possible geometries of the Main Himalayan Thrust (MHT), the role of other regional faults, the crustal composition and role of fluids in faulting, and the details of the rupture process, including structural causes and locations of rupture segmentation both along-strike and down-dip. These recent <span class="hlt">earthquakes</span> and their aftershocks provide a unique opportunity to learn more about this collision zone. In June 2015, funded by NSF, we deployed the Nepal Array Measuring Aftershock Seismicity Trailing <span class="hlt">Earthquake</span> (NAMASTE) array of 46 seismic stations distributed across eastern and central Nepal, spanning the region with most of the aftershocks. This array remained in place for 11 months from June 2015 to May 2016. We combine new results from this aftershock network in Nepal with previous geophysical and geological studies across the Himalaya to derive a new understanding of the tectonics of the Himalaya and southern Tibet in Nepal and surrounding countries. We focus on structure and composition of the Main Himalayan Thrust and compare this continent-continent subduction megathrust with megathrusts in other subduction zones.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S33G2947F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S33G2947F"><span><span class="hlt">Earthquake</span> Triggering in the September 2017 Mexican <span class="hlt">Earthquake</span> Sequence</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fielding, E. J.; Gombert, B.; Duputel, Z.; Huang, M. H.; Liang, C.; Bekaert, D. P.; Moore, A. W.; Liu, Z.; Ampuero, J. P.</p> <p>2017-12-01</p> <p>Southern Mexico was struck by four <span class="hlt">earthquakes</span> with Mw > 6 and numerous smaller <span class="hlt">earthquakes</span> in September 2017, starting with the 8 September Mw 8.2 Tehuantepec <span class="hlt">earthquake</span> beneath the Gulf of Tehuantepec offshore Chiapas and Oaxaca. We study whether this M8.2 <span class="hlt">earthquake</span> triggered the three subsequent large M>6 quakes in southern Mexico to improve understanding of <span class="hlt">earthquake</span> interactions and time-dependent risk. All four large <span class="hlt">earthquakes</span> were extensional despite the the subduction of the Cocos plate. The traditional definition of aftershocks: likely an aftershock if it occurs within two rupture lengths of the main shock soon afterwards. Two Mw 6.1 <span class="hlt">earthquakes</span>, one half an hour after the M8.2 beneath the Tehuantepec gulf and one on 23 September near Ixtepec in Oaxaca, both fit as traditional aftershocks, within 200 km of the main rupture. The 19 September Mw 7.1 Puebla <span class="hlt">earthquake</span> was 600 km away from the M8.2 shock, outside the standard aftershock zone. Geodetic measurements from interferometric analysis of synthetic aperture radar (InSAR) and time-series analysis of GPS station data constrain finite fault total slip models for the M8.2, M7.1, and M6.1 Ixtepec <span class="hlt">earthquakes</span>. The early M6.1 aftershock was too close in time and space to the M8.2 to measure with InSAR or GPS. We analyzed InSAR data from Copernicus Sentinel-1A and -1B satellites and JAXA ALOS-2 satellite. Our preliminary geodetic slip model for the M8.2 quake shows significant slip extended > 150 km NW from the hypocenter, longer than slip in the v1 finite-fault model (FFM) from teleseismic waveforms posted by G. Hayes at USGS NEIC. Our slip model for the M7.1 <span class="hlt">earthquake</span> is similar to the v2 NEIC FFM. Interferograms for the M6.1 Ixtepec quake confirm the shallow depth in the upper-plate crust and show centroid is about 30 km SW of the NEIC epicenter, a significant NEIC location bias, but consistent with cluster relocations (E. Bergman, pers. comm.) and with Mexican SSN location. Coulomb static stress</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/2014/1025/a/pdf/ofr2014-1025.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/2014/1025/a/pdf/ofr2014-1025.pdf"><span><span class="hlt">Earthquake</span> catalog for estimation of maximum <span class="hlt">earthquake</span> magnitude, Central and Eastern United States: Part A, Prehistoric <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Wheeler, Russell L.</p> <p>2014-01-01</p> <p>Computation of probabilistic <span class="hlt">earthquake</span> hazard requires an estimate of Mmax, the maximum <span class="hlt">earthquake</span> magnitude thought to be possible within a specified geographic region. This report is Part A of an Open-File Report that describes the construction of a global catalog of moderate to large <span class="hlt">earthquakes</span>, from which one can estimate Mmax for most of the Central and Eastern United States and adjacent Canada. The catalog and Mmax estimates derived from it were used in the 2014 edition of the U.S. Geological Survey national seismic-hazard maps. This Part A discusses prehistoric <span class="hlt">earthquakes</span> that occurred in eastern North America, northwestern Europe, and Australia, whereas a separate Part B deals with historical events.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5827770','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5827770"><span>‘M-TRACK’ (mobile phone reminders and electronic tracking tool) cuts the risk of pre-treatment loss to follow-up by 80% among people living with HIV under programme settings: a mixed-methods study from <span class="hlt">Gujarat</span>, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Mehta, Kedar; Kumar, Ajay M. V.; Chawla, Sudhir; Chavda, Paragkumar; Selvaraj, Kalaiselvi; Shringarpure, Kalpita S.; Solanki, Dipak M.; Verma, Pramod B.; Rewari, B. B.</p> <p>2018-01-01</p> <p>ABSTRACT Background: In 2016, the National AIDS Control Programme (NACP) in <span class="hlt">Gujarat</span>, <span class="hlt">India</span> implemented an innovative intervention called ‘M-TRACK’ (mobile phone reminders once every week for four weeks after diagnosis and electronic patient tracking tool) to reduce pre-treatment loss to follow-up (LFU) among people living with HIV (PLHIV) in Vadodara district while other districts received standard of care. Objectives: To assess the effectiveness of M-TRACK in reducing pre-treatment LFU (proportion of diagnosed PLHIV not registering for HIV care by four weeks after diagnosis) and to explore the implementation enablers and challenges from health care providers’ and PLHIV perspective. Methods: An explanatory mixed-methods study design was used wherein the quantitative phase (cohort study with two groups: Vadodara district exposed to M-TRACK and Rajkot district as unexposed) was followed by a qualitative phase (descriptive study involving group interview with 16 health care providers, personal interviews with two programme managers and telephonic interviews with 16 PLHIV). Data were collected during October 2016 to February 2017. Results: During the pre-M-TRACK period (July–September 2016), the LFU proportion was similar [13% (25/191) in Vadodara; 15% (21/141) in Rajkot (p = 0.8)]. During the M-TRACK period (October–December 2016), LFU decreased to 4% (9/209) in Vadodara (exposed), whereas it remained similar at 16% (18/113) in Rajkot (unexposed) district (p = 0.02). PLHIV exposed to M-TRACK had an 80% lower risk of LFU (aRR 0.2; 95% CI: 0.1–0.5) compared with standard care, after adjusting for socio-demographics, time and clustering at district level. During interviews, M-TRACK was welcomed by both PLHIV and the counsellors. The latter felt it saved time by obviating the need for home visits and helped in documentation. Inconvenience of using landline phone available at the health facility, lack of budgets for reimbursement of mobile call expenses and</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_19 --> <div id="page_20" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="381"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70020887','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70020887"><span>The initial subevent of the 1994 Northridge, California, <span class="hlt">earthquake</span>: Is <span class="hlt">earthquake</span> size predictable?</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Kilb, Debi; Gomberg, J.</p> <p>1999-01-01</p> <p>We examine the initial subevent (ISE) of the M?? 6.7, 1994 Northridge, California, <span class="hlt">earthquake</span> in order to discriminate between two end-member rupture initiation models: the 'preslip' and 'cascade' models. Final <span class="hlt">earthquake</span> size may be predictable from an ISE's seismic signature in the preslip model but not in the cascade model. In the cascade model ISEs are simply small <span class="hlt">earthquakes</span> that can be described as purely dynamic ruptures. In this model a large <span class="hlt">earthquake</span> is triggered by smaller <span class="hlt">earthquakes</span>; there is no size scaling between triggering and triggered events and a variety of stress transfer mechanisms are possible. Alternatively, in the preslip model, a large <span class="hlt">earthquake</span> nucleates as an aseismically slipping patch in which the patch dimension grows and scales with the <span class="hlt">earthquake</span>'s ultimate size; the byproduct of this loading process is the ISE. In this model, the duration of the ISE signal scales with the ultimate size of the <span class="hlt">earthquake</span>, suggesting that nucleation and <span class="hlt">earthquake</span> size are determined by a more predictable, measurable, and organized process. To distinguish between these two end-member models we use short period seismograms recorded by the Southern California Seismic Network. We address questions regarding the similarity in hypocenter locations and focal mechanisms of the ISE and the mainshock. We also compare the ISE's waveform characteristics to those of small <span class="hlt">earthquakes</span> and to the beginnings of <span class="hlt">earthquakes</span> with a range of magnitudes. We find that the focal mechanisms of the ISE and mainshock are indistinguishable, and both events may have nucleated on and ruptured the same fault plane. These results satisfy the requirements for both models and thus do not discriminate between them. However, further tests show the ISE's waveform characteristics are similar to those of typical small <span class="hlt">earthquakes</span> in the vicinity and more importantly, do not scale with the mainshock magnitude. These results are more consistent with the cascade model.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17..624D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17..624D"><span>Numerical Simulation of Stress evolution and <span class="hlt">earthquake</span> sequence of the Tibetan Plateau</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dong, Peiyu; Hu, Caibo; Shi, Yaolin</p> <p>2015-04-01</p> <p>The <span class="hlt">India</span>-Eurasia's collision produces N-S compression and results in large thrust fault in the southern edge of the Tibetan Plateau. Differential eastern flow of the lower crust of the plateau leads to large strike-slip faults and normal faults within the plateau. From 1904 to 2014, more than 30 <span class="hlt">earthquakes</span> of Mw > 6.5 occurred sequentially in this distinctive tectonic environment. How did the stresses evolve during the last 110 years, how did the <span class="hlt">earthquakes</span> interact with each other? Can this knowledge help us to forecast the future seismic hazards? In this essay, we tried to simulate the evolution of the stress field and the <span class="hlt">earthquake</span> sequence in the Tibetan plateau within the last 110 years with a 2-D finite element model. Given an initial state of stress, the boundary condition was constrained by the present-day GPS observation, which was assumed as a constant rate during the 110 years. We calculated stress evolution year by year, and <span class="hlt">earthquake</span> would occur if stress exceed the crustal strength. Stress changes due to each large <span class="hlt">earthquake</span> in the sequence was calculated and contributed to the stress evolution. A key issue is the choice of initial stress state of the modeling, which is actually unknown. Usually, in the study of <span class="hlt">earthquake</span> triggering, people assume the initial stress is zero, and only calculate the stress changes by large <span class="hlt">earthquakes</span> - the Coulomb failure stress changes (Δ CFS). To some extent, this simplified method is a powerful tool because it can reveal which fault or which part of a fault becomes more risky or safer relatively. Nonetheless, it has not utilized all information available to us. The <span class="hlt">earthquake</span> sequence reveals, though far from complete, some information about the stress state in the region. If the entire region is close to a self-organized critical or subcritical state, <span class="hlt">earthquake</span> stress drop provides an estimate of lower limit of initial state. For locations no <span class="hlt">earthquakes</span> occurred during the period, initial stress has to be</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA519669','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA519669"><span>Empirical Observations of <span class="hlt">Earthquake</span>-Explosion Discrimination Using P/S Ratios and Implications for the Sources of Explosion S-Waves</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2007-09-01</p> <p>stations at test sites around the world (e.g., Nevada, Lop Nor, Novaya Zemlya, Semipalatinsk , <span class="hlt">India</span>, Pakistan, and North Korea). We show this pattern...regional P/S amplitudes tended to be dominated by frequencies around 1 Hz. As shown in Figure 2 at a number of major nuclear test sites , these...Figure 2. Bandpass filtered 1-2 Hz seismograms of <span class="hlt">earthquake</span> (red) and explosion (blue) pairs at nuclear test sites show little consistent</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA569495','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA569495"><span>Identification of Deep <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2010-09-01</p> <p>discriminants that will reliably separate small, crustal <span class="hlt">earthquakes</span> (magnitudes less than about 4 and depths less than about 40 to 50 km) from small...characteristics on discrimination plots designed to separate nuclear explosions from crustal <span class="hlt">earthquakes</span>. Thus, reliably flagging these small, deep events is...Further, reliably identifying subcrustal <span class="hlt">earthquakes</span> will allow us to eliminate deep events (previously misidentified as crustal <span class="hlt">earthquakes</span>) from</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17794569','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17794569"><span>The 1985 central chile <span class="hlt">earthquake</span>: a repeat of previous great <span class="hlt">earthquakes</span> in the region?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Comte, D; Eisenberg, A; Lorca, E; Pardo, M; Ponce, L; Saragoni, R; Singh, S K; Suárez, G</p> <p>1986-07-25</p> <p>A great <span class="hlt">earthquake</span> (surface-wave magnitude, 7.8) occurred along the coast of central Chile on 3 March 1985, causing heavy damage to coastal towns. Intense foreshock activity near the epicenter of the main shock occurred for 11 days before the <span class="hlt">earthquake</span>. The aftershocks of the 1985 <span class="hlt">earthquake</span> define a rupture area of 170 by 110 square kilometers. The <span class="hlt">earthquake</span> was forecast on the basis of the nearly constant repeat time (83 +/- 9 years) of great <span class="hlt">earthquakes</span> in this region. An analysis of previous <span class="hlt">earthquakes</span> suggests that the rupture lengths of great shocks in the region vary by a factor of about 3. The nearly constant repeat time and variable rupture lengths cannot be reconciled with time- or slip-predictable models of <span class="hlt">earthquake</span> recurrence. The great <span class="hlt">earthquakes</span> in the region seem to involve a variable rupture mode and yet, for unknown reasons, remain periodic. Historical data suggest that the region south of the 1985 rupture zone should now be considered a gap of high seismic potential that may rupture in a great <span class="hlt">earthquake</span> in the next few tens of years.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17162696','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17162696"><span>Administrative issues involved in disaster management in <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kaur, Jagdish</p> <p>2006-12-01</p> <p><span class="hlt">India</span> as a country is vulnerable to a number of disasters, from <span class="hlt">earthquakes</span> to floods. Poor and weaker members of the society have always been more vulnerable to various types of disasters. Disasters result in unacceptably high morbidity and mortality amongst the affected population. Damage to infrastructure and reduction in revenues from the affected region due to low yield add to the economic losses. Poor co-ordination at the local level, lack of early-warning systems, often very slow responses, paucity of trained dedicated clinicians, lack of search and rescue facilities and poor community empowerment are some of the factors, which have been contributing to poor response following disasters in the past. The first formal step towards development of policies relating to disaster care in <span class="hlt">India</span> was the formulation of the National Disaster Response Plan (NDRP) which was formulated initially by the Government of <span class="hlt">India</span> for managing natural disasters only. However, this was subsequently amended to include man-made disasters as well. It sets the scene for formulating state and district level plans in all states to bring cohesiveness and a degree of uniform management in dealing with disasters. A National Disaster Management Authority has been constituted which aims to provide national guidelines and is headed by the Prime Minister of <span class="hlt">India</span>. It is the highest decision-making body for the management of disasters in the country. The authority has the responsibility for co-ordinating response and post-disaster relief and rehabilitation. Each state is required to set up Disaster Management Authorities and District Disaster Management Committees for co-ordination and close supervision of activities and efforts related to the management of disasters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018E%26ES..108d2014W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018E%26ES..108d2014W"><span>The relationship between <span class="hlt">earthquake</span> exposure and posttraumatic stress disorder in 2013 Lushan <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wang, Yan; Lu, Yi</p> <p>2018-01-01</p> <p>The objective of this study is to explore the relationship between <span class="hlt">earthquake</span> exposure and the incidence of PTSD. A stratification random sample survey was conducted to collect data in the Longmenshan thrust fault after Lushan <span class="hlt">earthquake</span> three years. We used the Children's Revised Impact of Event Scale (CRIES-13) and the <span class="hlt">Earthquake</span> Experience Scale. Subjects in this study included 3944 school student survivors in local eleven schools. The prevalence of probable PTSD is relatively higher, when the people was trapped in the <span class="hlt">earthquake</span>, was injured in the <span class="hlt">earthquake</span> or have relatives who died in the <span class="hlt">earthquake</span>. It concluded that researchers need to pay more attention to the children and adolescents. The government should pay more attention to these people and provide more economic support.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1998SedG..119..239B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1998SedG..119..239B"><span>Seismites in a Proterozoic tidal succession, Singhbhum, Bihar, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bhattacharya, H. N.; Bandyopadhyay, Sandip</p> <p>1998-08-01</p> <p>Early Proterozoic metasediments of the Chaibasa Formation (Galudih-Ghatsila-Dhalbhumgarh region, Singhbhum, Bihar, <span class="hlt">India</span>) comprise a number of cyclic fining-upward prograding successions of tidalites. The tidalites show indications for <span class="hlt">earthquakes</span> in the form of synsedimentary deformation features, apart from the structures due to high-energy wave action. Deformed cross-bedding, convolute laminations, synsedimentary faults, graben-like structures, sandstone dykes, pseudonodules and slump folds record the seismic activity. A gradual decline in the frequency of seismites and tsunami-related depositional features, in combination with an upward increase in thickness of the tidal cycles, are attributed to gradual diminishing of tectonic activity within the basin.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26601167','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26601167"><span>Crowdsourced <span class="hlt">earthquake</span> early warning.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Minson, Sarah E; Brooks, Benjamin A; Glennie, Craig L; Murray, Jessica R; Langbein, John O; Owen, Susan E; Heaton, Thomas H; Iannucci, Robert A; Hauser, Darren L</p> <p>2015-04-01</p> <p><span class="hlt">Earthquake</span> early warning (EEW) can reduce harm to people and infrastructure from <span class="hlt">earthquakes</span> and tsunamis, but it has not been implemented in most high <span class="hlt">earthquake</span>-risk regions because of prohibitive cost. Common consumer devices such as smartphones contain low-cost versions of the sensors used in EEW. Although less accurate than scientific-grade instruments, these sensors are globally ubiquitous. Through controlled tests of consumer devices, simulation of an M w (moment magnitude) 7 <span class="hlt">earthquake</span> on California's Hayward fault, and real data from the M w 9 Tohoku-oki <span class="hlt">earthquake</span>, we demonstrate that EEW could be achieved via crowdsourcing.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4640622','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4640622"><span>Crowdsourced <span class="hlt">earthquake</span> early warning</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Minson, Sarah E.; Brooks, Benjamin A.; Glennie, Craig L.; Murray, Jessica R.; Langbein, John O.; Owen, Susan E.; Heaton, Thomas H.; Iannucci, Robert A.; Hauser, Darren L.</p> <p>2015-01-01</p> <p><span class="hlt">Earthquake</span> early warning (EEW) can reduce harm to people and infrastructure from <span class="hlt">earthquakes</span> and tsunamis, but it has not been implemented in most high <span class="hlt">earthquake</span>-risk regions because of prohibitive cost. Common consumer devices such as smartphones contain low-cost versions of the sensors used in EEW. Although less accurate than scientific-grade instruments, these sensors are globally ubiquitous. Through controlled tests of consumer devices, simulation of an Mw (moment magnitude) 7 <span class="hlt">earthquake</span> on California’s Hayward fault, and real data from the Mw 9 Tohoku-oki <span class="hlt">earthquake</span>, we demonstrate that EEW could be achieved via crowdsourcing. PMID:26601167</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70168767','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70168767"><span><span class="hlt">Earthquakes</span>, November-December 1992</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1993-01-01</p> <p>There were two major <span class="hlt">earthquakes</span> (7.0≤M<8.0) during the last two months of the year, a magntidue 7.5 <span class="hlt">earthquake</span> on December 12 in the Flores region, Indonesia, and a magnitude 7.0 <span class="hlt">earthquake</span> on December 20 in the Banda Sea. <span class="hlt">Earthquakes</span> caused fatalities in China and Indonesia. The greatest number of deaths (2,500) for the year occurred in Indonesia. In Switzerland, six people were killed by an accidental explosion recoreded by seismographs. In teh United States, a magnitude 5.3 <span class="hlt">earthquake</span> caused slight damage at Big Bear in southern California. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70195363','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70195363"><span>Crowdsourced <span class="hlt">earthquake</span> early warning</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Minson, Sarah E.; Brooks, Benjamin A.; Glennie, Craig L.; Murray, Jessica R.; Langbein, John O.; Owen, Susan E.; Heaton, Thomas H.; Iannucci, Robert A.; Hauser, Darren L.</p> <p>2015-01-01</p> <p><span class="hlt">Earthquake</span> early warning (EEW) can reduce harm to people and infrastructure from <span class="hlt">earthquakes</span> and tsunamis, but it has not been implemented in most high <span class="hlt">earthquake</span>-risk regions because of prohibitive cost. Common consumer devices such as smartphones contain low-cost versions of the sensors used in EEW. Although less accurate than scientific-grade instruments, these sensors are globally ubiquitous. Through controlled tests of consumer devices, simulation of an Mw (moment magnitude) 7 <span class="hlt">earthquake</span> on California’s Hayward fault, and real data from the Mw 9 Tohoku-oki <span class="hlt">earthquake</span>, we demonstrate that EEW could be achieved via crowdsourcing.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUSM.G11C..08D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUSM.G11C..08D"><span>Sumatra Megathrust <span class="hlt">Earthquakes</span> Trigger Intraplate Seismicity in the Indo-Australian Oceanic Lithosphere</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Delescluse, M.; Chamot-Rooke, N.; Cattin, R.</p> <p>2009-05-01</p> <p>The present-day intraplate deformation between <span class="hlt">India</span> and Australia started 9 Myrs ago. In the Central Indian Basin (CIB), this deformation is recorded in the thick sediments of the Bengal fan. The equatorial, dense E-W thrust fault network in this region is the result of a massive reverse reactivation of normal faults at the onset of deformation. The Wharton Basin (WB), separated from the CIB by the NinetyEast Ridge (NyR), shows a contrasting style of deformation with mainly left-lateral strike-slip seismicity. The WB finite deformation and seismicity also involve pre-existing faults, in this case the N-S paleo-transforms of the fossile Wharton spreading-ridge system. The oceanic plate seismicity after the December 2004 Aceh subduction <span class="hlt">earthquake</span> shows strike-slip events with a clear intraplate P-axis. No thrust faults are detected. This indicates short-term reactivation of the transform faults near the trench. Spatial and temporal distribution of intraplate erthquakes, as well as their anomalous moment release suggests triggering by the Aceh megathrust <span class="hlt">earthquake</span>, which appears to have acted as an "accelerator" for the oceanic intraplate deformation. In this study, we use Coulomb stress static variations to confirm our seismicity observations. We first assume that the reactivated transform and the neoformed thrust fault plane families are present in the oceanic lithosphere. We then compute the coseismic stresses in the vicinity of the trench from the Aceh and Nias <span class="hlt">earthquakes</span> slip distributions. Finally, we derive the normal and shear stresses on the fault planes. The results show that the strike-slip events are all favored by the subduction <span class="hlt">earthquakes</span> coseismic stresses. They also show that the normal fault <span class="hlt">earthquakes</span> at oceanic bulges are supported by the modeled coseismic stresses, except offshore Myanmar. The particularly interesting result is that all the possible neoformed thrust faults perpendicular to the intraplate P-axis are inhibited by the same</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4495514','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4495514"><span>Bio-Mimetics of Disaster Anticipation—Learning Experience and Key-Challenges</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Tributsch, Helmut</p> <p>2013-01-01</p> <p> event. The final product, however, of any energy turnover is heat. Satellite based infrared measurements have indeed identified significant thermal anomalies before major <span class="hlt">earthquakes</span>. One of these cases, occurring during the 2001 Bhuj <span class="hlt">earthquake</span> in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>, is analyzed together with parallel animal anomalies observed in the Gir national park. It is suggested that the time window is identical and that both phenomena have the same geophysical origin. It therefore remains to be demonstrated that energy can be released locally before major <span class="hlt">earthquake</span> events. It is shown that by considering appropriate geophysical feedback processes, this is possible for large scale energy conversion phenomena within highly non-linear geophysical mechanisms. With satellite monitored infrared anomalies indicating possible epicenters and local animal and environmental observations immediately initiated, the learning experience towards an understanding of the phenomena involved could be accelerated. PMID:26487318</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T31A0603S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T31A0603S"><span><span class="hlt">Earthquake</span> Clusters and Spatio-temporal Migration of <span class="hlt">earthquakes</span> in Northeastern Tibetan Plateau: a Finite Element Modeling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sun, Y.; Luo, G.</p> <p>2017-12-01</p> <p>Seismicity in a region is usually characterized by <span class="hlt">earthquake</span> clusters and <span class="hlt">earthquake</span> migration along its major fault zones. However, we do not fully understand why and how <span class="hlt">earthquake</span> clusters and spatio-temporal migration of <span class="hlt">earthquakes</span> occur. The northeastern Tibetan Plateau is a good example for us to investigate these problems. In this study, we construct and use a three-dimensional viscoelastoplastic finite-element model to simulate <span class="hlt">earthquake</span> cycles and spatio-temporal migration of <span class="hlt">earthquakes</span> along major fault zones in northeastern Tibetan Plateau. We calculate stress evolution and fault interactions, and explore effects of topographic loading and viscosity of middle-lower crust and upper mantle on model results. Model results show that <span class="hlt">earthquakes</span> and fault interactions increase Coulomb stress on the neighboring faults or segments, accelerating the future <span class="hlt">earthquakes</span> in this region. Thus, <span class="hlt">earthquakes</span> occur sequentially in a short time, leading to regional <span class="hlt">earthquake</span> clusters. Through long-term evolution, stresses on some seismogenic faults, which are far apart, may almost simultaneously reach the critical state of fault failure, probably also leading to regional <span class="hlt">earthquake</span> clusters and <span class="hlt">earthquake</span> migration. Based on our model synthetic seismic catalog and paleoseismic data, we analyze probability of <span class="hlt">earthquake</span> migration between major faults in northeastern Tibetan Plateau. We find that following the 1920 M 8.5 Haiyuan <span class="hlt">earthquake</span> and the 1927 M 8.0 Gulang <span class="hlt">earthquake</span>, the next big event (M≥7) in northeastern Tibetan Plateau would be most likely to occur on the Haiyuan fault.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AdSpR..60.1787C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AdSpR..60.1787C"><span>Numerical modeling of possible lower ionospheric anomalies associated with Nepal <span class="hlt">earthquake</span> in May, 2015</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chakraborty, Suman; Sasmal, Sudipta; Basak, Tamal; Ghosh, Soujan; Palit, Sourav; Chakrabarti, Sandip K.; Ray, Suman</p> <p>2017-10-01</p> <p>We present perturbations due to seismo-ionospheric coupling processes in propagation characteristics of sub-ionospheric Very Low Frequency (VLF) signals received at Ionospheric & <span class="hlt">Earthquake</span> Research Centre (IERC) (Lat. 22.50°N, Long. 87.48°E), <span class="hlt">India</span>. The study is done during and prior to an <span class="hlt">earthquake</span> of Richter scale magnitude M = 7.3 occurring at a depth of 18 km at southeast of Kodari, Nepal on 12 May 2015 at 12:35:19 IST (07:05:19 UT). The recorded VLF signal of Japanese transmitter JJI at frequency 22.2 kHz (Lat. 32.08°N, Long. 130.83°E) suffers from strong shifts in sunrise and sunset terminator times towards nighttime starting from three to four days prior to the <span class="hlt">earthquake</span>. The signal shows a similar variation in terminator times during a major aftershock of magnitude M = 6.7 on 16 May, 2015 at 17:04:10 IST (11:34:10 UT). These shifts in terminator times is numerically modeled using Long Wavelength Propagation Capability (LWPC) Programme. The unperturbed VLF signal is simulated by using the day and night variation of reflection height (h‧) and steepness parameter (β) fed in LWPC for the entire path. The perturbed signal is obtained by additional variation of these parameters inside the <span class="hlt">earthquake</span> preparation zone. It is found that the shift of the terminator time towards nighttime happens only when the reflection height is increased. We also calculate electron density profile by using the Wait's exponential formula for specified location over the propagation path.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70176398','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70176398"><span>Prototype operational <span class="hlt">earthquake</span> prediction system</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Spall, Henry</p> <p>1986-01-01</p> <p>An objective if the U.S. <span class="hlt">Earthquake</span> Hazards Reduction Act of 1977 is to introduce into all regions of the country that are subject to large and moderate <span class="hlt">earthquakes</span>, systems for predicting <span class="hlt">earthquakes</span> and assessing <span class="hlt">earthquake</span> risk. In 1985, the USGS developed for the Secretary of the Interior a program for implementation of a prototype operational <span class="hlt">earthquake</span> prediction system in southern California.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/14870793','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/14870793"><span>Detection of MEF-1 laboratory reference strain of poliovirus type 2 in children with poliomyelitis in <span class="hlt">India</span> in 2002 & 2003.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Deshpande, J M; Nadkarni, S S; Siddiqui, Z A</p> <p>2003-12-01</p> <p>Significant progress has been made towards eradication of poliomyelitis in <span class="hlt">India</span>. Surveillance for acute flaccid paralysis (AFP) has reached high standards. Among the 3 types of polioviruses, type 2 had been eliminated in <span class="hlt">India</span> and eradicated globally as of October 1999. However, we isolated wild poliovirus type 2 from a small number of polio cases in northern <span class="hlt">India</span> in 2000 and again during December 2002 to February 2003. Using molecular tools the origin, of the wild type 2 poliovirus was investigated. Polioviruses isolated from stool samples collected from patients with AFP were differentiated as wild virus or Sabin vaccine-like by ELISA and probe hybridization assays. Complete VP1 gene nucleotide sequences of the wild type 2 poliovirus isolates were determined by reverse transcriptase polymerase chain reaction (RT-PCR), followed by cycle sequencing. VP1 nucleotide sequences were compared with those of wild type 2 polioviruses that were indigenous in <span class="hlt">India</span> in the past as well as prototype/laboratory strains and the GenBank database. Wild poliovirus type 2 was detected in stool samples from 6 patients with AFP in western Uttar Pradesh and 1 in <span class="hlt">Gujarat</span>. In addition, the virus was isolated from one healthy contact child and from environmental sewage sample in Moradabad where three of these patients were reported. These isolates were identified as genetically closely related to laboratory reference strain MEF-1. Molecular characterization of the isolates confirmed that there was no evidence of extensive person-to-person transmission of the virus in the community. Laboratory reference strain (MEF-1) of poliovirus type 2 caused paralytic poliomyelitis in 10 patients in September 2000 and November 2002 to February 2003. The origin of the virus was some laboratory as yet not identified. This episode highlights the urgent need for stringent containment of wild poliovirus containing materials in the laboratories across the country in order to prevent recurrence of such</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/22300232','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/22300232"><span>Perception of <span class="hlt">earthquake</span> risk in Taiwan: effects of gender and past <span class="hlt">earthquake</span> experience.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Kung, Yi-Wen; Chen, Sue-Huei</p> <p>2012-09-01</p> <p>This study explored how individuals in Taiwan perceive the risk of <span class="hlt">earthquake</span> and the relationship of past <span class="hlt">earthquake</span> experience and gender to risk perception. Participants (n= 1,405), including <span class="hlt">earthquake</span> survivors and those in the general population without prior direct <span class="hlt">earthquake</span> exposure, were selected and interviewed through a computer-assisted telephone interviewing procedure using a random sampling and stratification method covering all 24 regions of Taiwan. A factor analysis of the interview data yielded a two-factor structure of risk perception in regard to <span class="hlt">earthquake</span>. The first factor, "personal impact," encompassed perception of threat and fear related to <span class="hlt">earthquakes</span>. The second factor, "controllability," encompassed a sense of efficacy of self-protection in regard to <span class="hlt">earthquakes</span>. The findings indicated prior <span class="hlt">earthquake</span> survivors and females reported higher scores on the personal impact factor than males and those with no prior direct <span class="hlt">earthquake</span> experience, although there were no group differences on the controllability factor. The findings support that risk perception has multiple components, and suggest that past experience (survivor status) and gender (female) affect the perception of risk. Exploration of potential contributions of other demographic factors such as age, education, and marital status to personal impact, especially for females and survivors, is discussed. Future research on and intervention program with regard to risk perception are suggested accordingly. © 2012 Society for Risk Analysis.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/1995/0624/pdf/of95-624.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/1995/0624/pdf/of95-624.pdf"><span><span class="hlt">Earthquakes</span> in Alaska</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Haeussler, Peter J.; Plafker, George</p> <p>1995-01-01</p> <p><span class="hlt">Earthquake</span> risk is high in much of the southern half of Alaska, but it is not the same everywhere. This map shows the overall geologic setting in Alaska that produces <span class="hlt">earthquakes</span>. The Pacific plate (darker blue) is sliding northwestward past southeastern Alaska and then dives beneath the North American plate (light blue, green, and brown) in southern Alaska, the Alaska Peninsula, and the Aleutian Islands. Most <span class="hlt">earthquakes</span> are produced where these two plates come into contact and slide past each other. Major <span class="hlt">earthquakes</span> also occur throughout much of interior Alaska as a result of collision of a piece of crust with the southern margin.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_20 --> <div id="page_21" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="401"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T54C..03M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T54C..03M"><span>Seismicity Pattern and Fault Structure in the Central Himalaya Seismic Gap Using Precise <span class="hlt">Earthquake</span> Hypocenters and their Source Parameters</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mendoza, M.; Ghosh, A.; Rai, S. S.</p> <p>2017-12-01</p> <p>The devastation brought on by the Mw 7.8 Gorkha <span class="hlt">earthquake</span> in Nepal on 25 April 2015, reconditioned people to the high <span class="hlt">earthquake</span> risk along the Himalayan arc. It is therefore imperative to learn from the Gorkha <span class="hlt">earthquake</span>, and gain a better understanding of the state of stress in this fault regime, in order to identify areas that could produce the next devastating <span class="hlt">earthquake</span>. Here, we focus on what is known as the "central Himalaya seismic gap". It is located in Uttarakhand, <span class="hlt">India</span>, west of Nepal, where a large (> Mw 7.0) <span class="hlt">earthquake</span> has not occurred for over the past 200 years [Rajendran, C.P., & Rajendran, K., 2005]. This 500 - 800 km long along-strike seismic gap has been poorly studied, mainly due to the lack of modern and dense instrumentation. It is especially concerning since it surrounds densely populated cities, such as New Delhi. In this study, we analyze a rich seismic dataset from a dense network consisting of 50 broadband stations, that operated between 2005 and 2012. We use the STA/LTA filter technique to detect <span class="hlt">earthquake</span> phases, and the latest tools contributed to the Antelope software environment, to develop a large and robust <span class="hlt">earthquake</span> catalog containing thousands of precise hypocentral locations, magnitudes, and focal mechanisms. By refining those locations in HypoDD [Waldhauser & Ellsworth, 2000] to form a tighter cluster of events using relative relocation, we can potentially illustrate fault structures in this region with high resolution. Additionally, using ZMAP [Weimer, S., 2001], we perform a variety of statistical analyses to understand the variability and nature of seismicity occurring in the region. Generating a large and consistent <span class="hlt">earthquake</span> catalog not only brings to light the physical processes controlling the <span class="hlt">earthquake</span> cycle in an Himalayan seismogenic zone, it also illustrates how stresses are building up along the décollment and the faults that stem from it. With this new catalog, we aim to reveal fault structure, study</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMMR33A2635H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMMR33A2635H"><span>Rupture Propagation of the 2013 Mw7.7 Balochistan, Pakistan, <span class="hlt">Earthquake</span> Affected by Poroelastic Stress Changes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>He, J.; Wang, W.; Xiao, J.</p> <p>2015-12-01</p> <p>The 2013 Mw7.7 Balochistan, Pakistan, <span class="hlt">earthquake</span> occurred on the curved Hoshab fault. This fault connects with the north-south trending Chaman strike-slip fault to northeast, and with the west-east trending Makran thrust fault system to southwest. Teleseismic waveform inversion, incorporated with coseismic ground surface deformation data, show that the rupture of this <span class="hlt">earthquake</span> nucleated around northeast segment of the fault, and then propagated southwestward along the northwest dipping Hoshab fault about 200 km, with the maximum coseismic displacement, featured mainly by purely left-lateral strike-slip motion, about 10 meters. In context of the <span class="hlt">India</span>-Asia collision frame, associating with the fault geometry around this region, the rupture propagation of this <span class="hlt">earthquake</span> seems to not follow an optimal path along the fault segment, because after nucleation of this event the Hoshab fault on the southwest of hypocenter of this <span class="hlt">earthquake</span> is clamped by elastic stress change. Here, we build a three-dimensional finite-element model to explore the evolution of both stress and pore-pressure during the rupturing process of this <span class="hlt">earthquake</span>. In the model, the crustal deformation is treated as undrained poroelastic media as described by Biot's theory, and the instantaneous rupture process is specified with split-node technique. By testing a reasonable range of parameters, including the coefficient of friction, the undrained Poisson's ratio, the permeability of the fault zone and the bulk crust, numerical results have shown that after the nucleation of rupture of this <span class="hlt">earthquake</span> around the northeast of the Hoshab fault, the positive change of normal stress (clamping the fault) on the fault plane is greatly reduced by the instantaneous increase of pore pressure (unclamping the fault). This process could result in the change of Coulomb failure stress resolved on the Hoshab fault to be hastened, explaining the possible mechanism for southwestward propagation of rupture of the Mw7</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..12.3555D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..12.3555D"><span>Three dimensional surface displacement of the Sichuan <span class="hlt">earthquake</span> (Mw 7.9, China) from Synthetic Aperture Radar.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>de Michele, Marcello; Raucoules, Daniel; de Sigoyer, Julia; Pubellier, Manuel; Lasserre, Cecile; Pathier, Erwan; Klinger, Yann; van der Woerd, Jerome; Chamot-Rooke, Nicolas</p> <p>2010-05-01</p> <p>The Sichuan <span class="hlt">earthquake</span>, Mw 7.9, struck the Longmen Shan range front, in the western Sichuan province, China, on 12 May 2008. It severely affected an area where little historical seismicity and little or no significant active shortening were reported before the <span class="hlt">earthquake</span> (e.g. Gu et al., 1989; Chen et al., 1994; Gan et al., 2007). The Longmen Shan thrust system bounds the eastern margin of the Tibetan plateau and is considered as a transpressive zone since Triassic time that was reactivated during the <span class="hlt">India</span>-Asia collision (e.g., Tapponnier and Molnar, 1977, Chen and Wilson 1996; Arne et al., 1997, Godard et al., 2009). However, contrasting geological evidences of sparse thrusting and marked dextral strike-slip faulting during the Quaternary along with high topography (Burchfiel et al., 1995; Densmore et al., 2007) have led to models of dynamically driven and sustained topography (Royden et al., 1997) limiting the role of <span class="hlt">earthquakes</span> in relief building and leaving the mechanism of long term strain distribution in this area as an open question. Here we combine C and L band Synthetic Aperture Radar (SAR) offsets data from ascending and descending paths to retrieve the three dimensional surface displacement distribution all along the <span class="hlt">earthquake</span> ruptures of the Sichuan <span class="hlt">earthquake</span>. For the first time on this <span class="hlt">earthquake</span> we present near field 3D co-seismic surface displacement, which is an important datum for constraining modelled fault geometry at depth. Our results complement other Interferometric Synthetic Aperture Radar (InSAR) and field analyses in indicating that crustal shortening is one of the main drivers for topography building in the Longmen Shan (Liu-Zeng, 2009; Shen et al., 2009; Hubbard and Shaw, 2009). Moreover, our results put into evidence a small but significant amount of displacement in the range front that we interpret as due to slip at depth on a blind structure. We verify this hypothesis by inverting the data against a simple elastic dislocation model</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70169207','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70169207"><span><span class="hlt">Earthquakes</span>, November-December 1973</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1974-01-01</p> <p>Other parts of the world suffered fatalities and significant damage from <span class="hlt">earthquakes</span>. In Iran, an <span class="hlt">earthquake</span> killed one person, injured many, and destroyed a number of homes. <span class="hlt">Earthquake</span> fatalities also occurred in the Azores and in Algeria. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.T52A..03C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.T52A..03C"><span>Recent Surface Deformation in the Himalaya and Adjoining Piedmont Zone of the Ganga Plain, Uttarakhand, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chang, C. P.</p> <p>2015-12-01</p> <p>The Himalaya Frontal Thrust (HFT) is the longest active contractional structure on Earth. Understanding the activity of HFT and its surrounding area is a key for both unraveling the mechanism of Himalayan growth and preparing the major <span class="hlt">earthquake</span> disasters. The latter issue became much more important after the April 25th 2015 Nepal <span class="hlt">earthquake</span> (also known as the Gorkha <span class="hlt">earthquake</span>), which killed more than 8,800 people and injured more than 23,000. This <span class="hlt">earthquake</span> is a dramatic manifestation of the ongoing convergence between the Indo-Australian and Asian tectonic plates that has progressively built the Himalayas over the last 50 million years. Despite its importance, only a few preliminary studies have focused on the frontal part of the western Himalaya. The Himalaya and adjoining Ganga (also called Gangetic) plain in Uttarakhand state of <span class="hlt">India</span> are traversed by a number of neotectonically active longitudinal and transverse faults. However, the pattern and extent of present day surface deformations caused by these faults is not yet well known. We herein present the preliminary results of our investigation directed in this direction. Surface deformations induced by active faults during a period of seven years from 2003 to 2010 in the south western Himalaya and adjoining proximal part of the Ganga Plain in Uttarakhand state of <span class="hlt">India</span> have been firstly monitored. Multidate ENVISAT radar images of the area have been analyzed by applying the latest radar remote sensing technique of Persistent Scatterers Interferometric Synthetic Aperture Radar (PSI). Since PSI can extracts surface information even on vegetated or mountainous regions as well. The study reveals some conspicuous surface deformation patterns, which may be related directly to the active movements along some of the major fault /thrust in the area. For example the HFT and the transverse Garampani-Kathgodam Fault (G-KF). A campaign GPS network of 20 stations has also been installed in 2013 in our study area. This</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.nrel.gov/csp/solarpaces/by_country_detail.cfm/country=IN','SCIGOVWS'); return false;" href="https://www.nrel.gov/csp/solarpaces/by_country_detail.cfm/country=IN"><span>Concentrating Solar Power Projects in <span class="hlt">India</span> | Concentrating Solar Power |</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>;alphabetical by <em>project</em> name. You can browse a <em>project</em> profile by clicking on the <em>project</em> name. Abhijeet Solar <em>Project</em> ACME Solar Tower Dadri ISCC Plant Dhursar Diwakar Godawari Solar <em>Project</em> <span class="hlt">Gujarat</span> Solar One KVK Energy Solar <em>Project</em> Megha Solar Plant National Solar Thermal Power Facility</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3180155','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3180155"><span>Comparative study of <span class="hlt">earthquake</span>-related and non-<span class="hlt">earthquake</span>-related head traumas using multidetector computed tomography</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Chu, Zhi-gang; Yang, Zhi-gang; Dong, Zhi-hui; Chen, Tian-wu; Zhu, Zhi-yu; Shao, Heng</p> <p>2011-01-01</p> <p>OBJECTIVE: The features of <span class="hlt">earthquake</span>-related head injuries may be different from those of injuries obtained in daily life because of differences in circumstances. We aim to compare the features of head traumas caused by the Sichuan <span class="hlt">earthquake</span> with those of other common head traumas using multidetector computed tomography. METHODS: In total, 221 patients with <span class="hlt">earthquake</span>-related head traumas (the <span class="hlt">earthquake</span> group) and 221 patients with other common head traumas (the non-<span class="hlt">earthquake</span> group) were enrolled in our study, and their computed tomographic findings were compared. We focused the differences between fractures and intracranial injuries and the relationships between extracranial and intracranial injuries. RESULTS: More <span class="hlt">earthquake</span>-related cases had only extracranial soft tissue injuries (50.7% vs. 26.2%, RR = 1.9), and fewer cases had intracranial injuries (17.2% vs. 50.7%, RR = 0.3) compared with the non-<span class="hlt">earthquake</span> group. For patients with fractures and intracranial injuries, there were fewer cases with craniocerebral injuries in the <span class="hlt">earthquake</span> group (60.6% vs. 77.9%, RR = 0.8), and the <span class="hlt">earthquake</span>-injured patients had fewer fractures and intracranial injuries overall (1.5±0.9 vs. 2.5±1.8; 1.3±0.5 vs. 2.1±1.1). Compared with the non-<span class="hlt">earthquake</span> group, the incidences of soft tissue injuries and cranial fractures combined with intracranial injuries in the <span class="hlt">earthquake</span> group were significantly lower (9.8% vs. 43.7%, RR = 0.2; 35.1% vs. 82.2%, RR = 0.4). CONCLUSION: As depicted with computed tomography, the severity of <span class="hlt">earthquake</span>-related head traumas in survivors was milder, and isolated extracranial injuries were more common in <span class="hlt">earthquake</span>-related head traumas than in non-<span class="hlt">earthquake</span>-related injuries, which may have been the result of different injury causes, mechanisms and settings. PMID:22012045</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011AGUFMNH32A..04C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011AGUFMNH32A..04C"><span>2011 Tohoku <span class="hlt">Earthquake</span> and Japan's Nuclear Disaster - Implications for Indian Ocean Rim countries</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chadha, R. K.</p> <p>2011-12-01</p> <p> along the coasts. There are a few countries where nuclear installations are planned and hence, a critical analysis is required to know the realistic hazard due to <span class="hlt">earthquakes</span> and tsunami in these countries. The December 2004 Indian Ocean tsunami generated due to Sumatra <span class="hlt">earthquake</span> of M9.3 claimed more than 250,000 lives but did not caused a situation like in Japan. We studied the tsunami run-up heights and inundation along the east coast of <span class="hlt">India</span>. The maximum run-up height of 5.2 meters was observed at Nagapattinam with lateral inundation up to 800 meters and the minimum was at Devanaampatnam with a lateral inundation up to 340 meters. At Kalpakkam Nuclear Power Plant, the tsunami run-up height was 4.1 meters and water entered up to 360 meters inside the campus. Using the observed data we modeled several scenarios for Indian coast line for different <span class="hlt">earthquakes</span> along the subduction zone of Andaman-Sumatra in the east and Makran in south Pakistan in the western side using N2 Tsunami Model. The results obtained for few critical structures will be presented with an overview of scenarios for other countries.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70168760','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70168760"><span><span class="hlt">Earthquakes</span>, May-June 1991</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1992-01-01</p> <p>In the United States, a magnitude 5.8 <span class="hlt">earthquake</span> in southern California on June 28 killed two people and caused considerable damage. Strong <span class="hlt">earthquakes</span> hit Alaska on May 1 and May 30; the May 1 <span class="hlt">earthquake</span> caused some minor damage. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PApGe.175...49L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PApGe.175...49L"><span>Nowcasting <span class="hlt">Earthquakes</span>: A Comparison of Induced <span class="hlt">Earthquakes</span> in Oklahoma and at the Geysers, California</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Luginbuhl, Molly; Rundle, John B.; Hawkins, Angela; Turcotte, Donald L.</p> <p>2018-01-01</p> <p>Nowcasting is a new method of statistically classifying seismicity and seismic risk (Rundle et al. 2016). In this paper, the method is applied to the induced seismicity at the Geysers geothermal region in California and the induced seismicity due to fluid injection in Oklahoma. Nowcasting utilizes the catalogs of seismicity in these regions. Two <span class="hlt">earthquake</span> magnitudes are selected, one large say M_{λ } ≥ 4, and one small say M_{σ } ≥ 2. The method utilizes the number of small <span class="hlt">earthquakes</span> that occurs between pairs of large <span class="hlt">earthquakes</span>. The cumulative probability distribution of these values is obtained. The <span class="hlt">earthquake</span> potential score (EPS) is defined by the number of small <span class="hlt">earthquakes</span> that has occurred since the last large <span class="hlt">earthquake</span>, the point where this number falls on the cumulative probability distribution of interevent counts defines the EPS. A major advantage of nowcasting is that it utilizes "natural time", <span class="hlt">earthquake</span> counts, between events rather than clock time. Thus, it is not necessary to decluster aftershocks and the results are applicable if the level of induced seismicity varies in time. The application of natural time to the accumulation of the seismic hazard depends on the applicability of Gutenberg-Richter (GR) scaling. The increasing number of small <span class="hlt">earthquakes</span> that occur after a large <span class="hlt">earthquake</span> can be scaled to give the risk of a large <span class="hlt">earthquake</span> occurring. To illustrate our approach, we utilize the number of M_{σ } ≥ 2.75 <span class="hlt">earthquakes</span> in Oklahoma to nowcast the number of M_{λ } ≥ 4.0 <span class="hlt">earthquakes</span> in Oklahoma. The applicability of the scaling is illustrated during the rapid build-up of injection-induced seismicity between 2012 and 2016, and the subsequent reduction in seismicity associated with a reduction in fluid injections. The same method is applied to the geothermal-induced seismicity at the Geysers, California, for comparison.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70030585','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70030585"><span>The 1906 <span class="hlt">earthquake</span> and a century of progress in understanding <span class="hlt">earthquakes</span> and their hazards</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Zoback, M.L.</p> <p>2006-01-01</p> <p>The 18 April 1906 San Francisco <span class="hlt">earthquake</span> killed nearly 3000 people and left 225,000 residents homeless. Three days after the <span class="hlt">earthquake</span>, an eight-person <span class="hlt">Earthquake</span> Investigation Commission composed of 25 geologists, seismologists, geodesists, biologists and engineers, as well as some 300 others started work under the supervision of Andrew Lawson to collect and document physical phenomena related to the quake . On 31 May 1906, the commission published a preliminary 17-page report titled "The Report of the State <span class="hlt">Earthquake</span> Investigation Commission". The report included the bulk of the geological and morphological descriptions of the faulting, detailed reports on shaking intensity, as well as an impressive atlas of 40 oversized maps and folios. Nearly 100 years after its publication, the Commission Report remains a model for post-<span class="hlt">earthquake</span> investigations. Because the diverse data sets were so complete and carefully documented, researchers continue to apply modern analysis techniques to learn from the 1906 <span class="hlt">earthquake</span>. While the <span class="hlt">earthquake</span> marked a seminal event in the history of California, it served as impetus for the birth of modern <span class="hlt">earthquake</span> science in the United States.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70169184','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70169184"><span><span class="hlt">Earthquakes</span>; January-February, 1979</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1979-01-01</p> <p>The first major <span class="hlt">earthquake</span> (magnitude 7.0 to 7.9) of the year struck in southeastern Alaska in a sparsely populated area on February 28. On January 16, Iran experienced the first destructive <span class="hlt">earthquake</span> of the year causing a number of casualties and considerable damage. Peru was hit by a destructive <span class="hlt">earthquake</span> on February 16 that left casualties and damage. A number of <span class="hlt">earthquakes</span> were experienced in parts of the Untied States, but only minor damage was reported. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..1211153V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..1211153V"><span>Preliminary results on <span class="hlt">earthquake</span> triggered landslides for the Haiti <span class="hlt">earthquake</span> (January 2010)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>van Westen, Cees; Gorum, Tolga</p> <p>2010-05-01</p> <p>This study presents the first results on an analysis of the landslides triggered by the Ms 7.0 Haiti <span class="hlt">earthquake</span> that occurred on January 12, 2010 in the boundary region of the Pacific Plate and the North American plate. The fault is a left lateral strike slip fault with a clear surface expression. According to the USGS <span class="hlt">earthquake</span> information the Enriquillo-Plantain Garden fault system has not produced any major <span class="hlt">earthquake</span> in the last 100 years, and historical <span class="hlt">earthquakes</span> are known from 1860, 1770, 1761, 1751, 1684, 1673, and 1618, though none of these has been confirmed in the field as associated with this fault. We used high resolution satellite imagery available for the pre and post <span class="hlt">earthquake</span> situations, which were made freely available for the response and rescue operations. We made an interpretation of all co-seismic landslides in the epicentral area. We conclude that the <span class="hlt">earthquake</span> mainly triggered landslide in the northern slope of the fault-related valley and in a number of isolated area. The <span class="hlt">earthquake</span> apparently didn't trigger many visible landslides within the slum areas on the slopes in the southern part of Port-au-Prince and Carrefour. We also used ASTER DEM information to relate the landslide occurrences with DEM derivatives.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..11.6648E','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..11.6648E"><span>Turkish Compulsory <span class="hlt">Earthquake</span> Insurance (TCIP)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Erdik, M.; Durukal, E.; Sesetyan, K.</p> <p>2009-04-01</p> <p>Through a World Bank project a government-sponsored Turkish Catastrophic Insurance Pool (TCIP) is created in 2000 with the essential aim of transferring the government's financial burden of replacing <span class="hlt">earthquake</span>-damaged housing to international reinsurance and capital markets. Providing coverage to about 2.9 Million homeowners TCIP is the largest insurance program in the country with about 0.5 Billion USD in its own reserves and about 2.3 Billion USD in total claims paying capacity. The total payment for <span class="hlt">earthquake</span> damage since 2000 (mostly small, 226 <span class="hlt">earthquakes</span>) amounts to about 13 Million USD. The country-wide penetration rate is about 22%, highest in the Marmara region (30%) and lowest in the south-east Turkey (9%). TCIP is the sole-source provider of <span class="hlt">earthquake</span> loss coverage up to 90,000 USD per house. The annual premium, categorized on the basis of <span class="hlt">earthquake</span> zones type of structure, is about US90 for a 100 square meter reinforced concrete building in the most hazardous zone with 2% deductible. The <span class="hlt">earthquake</span> engineering related shortcomings of the TCIP is exemplified by fact that the average rate of 0.13% (for reinforced concrete buildings) with only 2% deductible is rather low compared to countries with similar <span class="hlt">earthquake</span> exposure. From an <span class="hlt">earthquake</span> engineering point of view the risk underwriting (Typification of housing units to be insured, <span class="hlt">earthquake</span> intensity zonation and the sum insured) of the TCIP needs to be overhauled. Especially for large cities, models can be developed where its expected <span class="hlt">earthquake</span> performance (and consequently the insurance premium) can be can be assessed on the basis of the location of the unit (microzoned <span class="hlt">earthquake</span> hazard) and basic structural attributes (<span class="hlt">earthquake</span> vulnerability relationships). With such an approach, in the future the TCIP can contribute to the control of construction through differentiation of premia on the basis of <span class="hlt">earthquake</span> vulnerability.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JGRB..123.2318B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JGRB..123.2318B"><span>Remote Triggering in the Koyna-Warna Reservoir-Induced Seismic Zone, Western <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bansal, Abhey Ram; Rao, N. Purnachandra; Peng, Zhigang; Shashidhar, D.; Meng, Xiaofeng</p> <p>2018-03-01</p> <p>Dynamic triggering following large distant <span class="hlt">earthquakes</span> has been observed in many regions globally. In this study, we present evidence for remote dynamic triggering in the Koyna-Warna region of Western <span class="hlt">India</span>, which is known to be a premier site of reservoir-induced seismicity. Using data from a closely spaced broadband network of 11 stations operated in the region since 2005, we conduct a systematic search for dynamic triggering following 20 large distant <span class="hlt">earthquakes</span> with dynamic stresses of at least 1 kPa in the region. We find that the only positive cases of dynamic triggering occurred during 11 April 2012, Mw8.6 Indian Ocean <span class="hlt">earthquake</span> and its largest aftershock of Mw8.2. In the first case, microearthquakes started to occur in the first few cycles of the Love waves, and the largest event of magnitude 3.3 occurred during the first few cycles of the Rayleigh waves. The increase of microseismicity lasted for up to five days, including a magnitude 4.8 event occurred approximately three days later. Our results suggest that the Koyna-Warna region is stress sensitive and susceptible for remote dynamic triggering, although the apparent triggering threshold appears to be slightly higher than other regions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUFM.S13C1453Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUFM.S13C1453Y"><span>Limitation of the Predominant-Period Estimator for <span class="hlt">Earthquake</span> Early Warning and the Initial Rupture of <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yamada, T.; Ide, S.</p> <p>2007-12-01</p> <p><span class="hlt">Earthquake</span> early warning is an important and challenging issue for the reduction of the seismic damage, especially for the mitigation of human suffering. One of the most important problems in <span class="hlt">earthquake</span> early warning systems is how immediately we can estimate the final size of an <span class="hlt">earthquake</span> after we observe the ground motion. It is relevant to the problem whether the initial rupture of an <span class="hlt">earthquake</span> has some information associated with its final size. Nakamura (1988) developed the Urgent <span class="hlt">Earthquake</span> Detection and Alarm System (UrEDAS). It calculates the predominant period of the P wave (τp) and estimates the magnitude of an <span class="hlt">earthquake</span> immediately after the P wave arrival from the value of τpmax, or the maximum value of τp. The similar approach has been adapted by other <span class="hlt">earthquake</span> alarm systems (e.g., Allen and Kanamori (2003)). To investigate the characteristic of the parameter τp and the effect of the length of the time window (TW) in the τpmax calculation, we analyze the high-frequency recordings of <span class="hlt">earthquakes</span> at very close distances in the Mponeng mine in South Africa. We find that values of τpmax have upper and lower limits. For larger <span class="hlt">earthquakes</span> whose source durations are longer than TW, the values of τpmax have an upper limit which depends on TW. On the other hand, the values for smaller <span class="hlt">earthquakes</span> have a lower limit which is proportional to the sampling interval. For intermediate <span class="hlt">earthquakes</span>, the values of τpmax are close to their typical source durations. These two limits and the slope for intermediate <span class="hlt">earthquakes</span> yield an artificial final size dependence of τpmax in a wide size range. The parameter τpmax is useful for detecting large <span class="hlt">earthquakes</span> and broadcasting <span class="hlt">earthquake</span> early warnings. However, its dependence on the final size of <span class="hlt">earthquakes</span> does not suggest that the <span class="hlt">earthquake</span> rupture is deterministic. This is because τpmax does not always have a direct relation to the physical quantities of an <span class="hlt">earthquake</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008Geomo.101..631K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008Geomo.101..631K"><span>GIS-based landslide susceptibility mapping for the 2005 Kashmir <span class="hlt">earthquake</span> region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kamp, Ulrich; Growley, Benjamin J.; Khattak, Ghazanfar A.; Owen, Lewis A.</p> <p>2008-11-01</p> <p>The Mw 7.6 October 8, 2005 Kashmir <span class="hlt">earthquake</span> triggered several thousand landslides throughout the Himalaya of northern Pakistan and <span class="hlt">India</span>. These were concentrated in six different geomorphic-geologic-anthropogenic settings. A spatial database, which included 2252 landslides, was developed and analyzed using ASTER satellite imagery and geographical information system (GIS) technology. A multi-criterion evaluation was applied to determine the significance of event-controlling parameters in triggering the landslides. The parameters included lithology, faults, slope gradient, slope aspect, elevation, land cover, rivers and roads. The results showed four classes of landslide susceptibility. Furthermore, they indicated that lithology had the strongest influence on landsliding, particularly when the rock is highly fractured, such as in shale, slate, clastic sediments, and limestone and dolomite. Moreover, the proximity of the landslides to faults, rivers, and roads was also an important factor in helping to initiate failures. In addition, landslides occurred particularly in moderate elevations on south facing slopes. Shrub land, grassland, and also agricultural land were highly susceptible to failures, while forested slopes had few landslides. One-third of the study area was highly or very highly susceptible to future landsliding and requires immediate mitigation action. The rest of the region had a low or moderate susceptibility to landsliding and remains relatively stable. This study supports the view that (1) <span class="hlt">earthquake</span>-triggered landslides are concentrated in specific zones associated with event-controlling parameters; and (2) in the western Himalaya deforestation and road construction contributed significantly to landsliding during and shortly after <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFMNH51C1627K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFMNH51C1627K"><span>Sun, Moon and <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kolvankar, V. G.</p> <p>2013-12-01</p> <p>During a study conducted to find the effect of Earth tides on the occurrence of <span class="hlt">earthquakes</span>, for small areas [typically 1000km X1000km] of high-seismicity regions, it was noticed that the Sun's position in terms of universal time [GMT] shows links to the sum of EMD [longitude of <span class="hlt">earthquake</span> location - longitude of Moon's foot print on earth] and SEM [Sun-Earth-Moon angle]. This paper provides the details of this relationship after studying <span class="hlt">earthquake</span> data for over forty high-seismicity regions of the world. It was found that over 98% of the <span class="hlt">earthquakes</span> for these different regions, examined for the period 1973-2008, show a direct relationship between the Sun's position [GMT] and [EMD+SEM]. As the time changes from 00-24 hours, the factor [EMD+SEM] changes through 360 degree, and plotting these two variables for <span class="hlt">earthquakes</span> from different small regions reveals a simple 45 degree straight-line relationship between them. This relationship was tested for all <span class="hlt">earthquakes</span> and <span class="hlt">earthquake</span> sequences for magnitude 2.0 and above. This study conclusively proves how Sun and the Moon govern all <span class="hlt">earthquakes</span>. Fig. 12 [A+B]. The left-hand figure provides a 24-hour plot for forty consecutive days including the main event (00:58:23 on 26.12.2004, Lat.+3.30, Long+95.980, Mb 9.0, EQ count 376). The right-hand figure provides an <span class="hlt">earthquake</span> plot for (EMD+SEM) vs GMT timings for the same data. All the 376 events including the main event faithfully follow the straight-line curve.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMNG12A..06S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMNG12A..06S"><span>Are <span class="hlt">Earthquakes</span> Predictable? A Study on Magnitude Correlations in <span class="hlt">Earthquake</span> Catalog and Experimental Data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Stavrianaki, K.; Ross, G.; Sammonds, P. R.</p> <p>2015-12-01</p> <p>The clustering of <span class="hlt">earthquakes</span> in time and space is widely accepted, however the existence of correlations in <span class="hlt">earthquake</span> magnitudes is more questionable. In standard models of seismic activity, it is usually assumed that magnitudes are independent and therefore in principle unpredictable. Our work seeks to test this assumption by analysing magnitude correlation between <span class="hlt">earthquakes</span> and their aftershocks. To separate mainshocks from aftershocks, we perform stochastic declustering based on the widely used Epidemic Type Aftershock Sequence (ETAS) model, which allows us to then compare the average magnitudes of aftershock sequences to that of their mainshock. The results of <span class="hlt">earthquake</span> magnitude correlations were compared with acoustic emissions (AE) from laboratory analog experiments, as fracturing generates both AE at the laboratory scale and <span class="hlt">earthquakes</span> on a crustal scale. Constant stress and constant strain rate experiments were done on Darley Dale sandstone under confining pressure to simulate depth of burial. Microcracking activity inside the rock volume was analyzed by the AE technique as a proxy for <span class="hlt">earthquakes</span>. Applying the ETAS model to experimental data allowed us to validate our results and provide for the first time a holistic view on the correlation of <span class="hlt">earthquake</span> magnitudes. Additionally we search the relationship between the conditional intensity estimates of the ETAS model and the <span class="hlt">earthquake</span> magnitudes. A positive relation would suggest the existence of magnitude correlations. The aim of this study is to observe any trends of dependency between the magnitudes of aftershock <span class="hlt">earthquakes</span> and the <span class="hlt">earthquakes</span> that trigger them.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/gip/119/pdf/GIP119_ScreenVersion.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/gip/119/pdf/GIP119_ScreenVersion.pdf"><span>Putting down roots in <span class="hlt">earthquake</span> country-Your handbook for <span class="hlt">earthquakes</span> in the Central United States</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Contributors: Dart, Richard; McCarthy, Jill; McCallister, Natasha; Williams, Robert A.</p> <p>2011-01-01</p> <p>This handbook provides information to residents of the Central United States about the threat of <span class="hlt">earthquakes</span> in that area, particularly along the New Madrid seismic zone, and explains how to prepare for, survive, and recover from such events. It explains the need for concern about <span class="hlt">earthquakes</span> for those residents and describes what one can expect during and after an <span class="hlt">earthquake</span>. Much is known about the threat of <span class="hlt">earthquakes</span> in the Central United States, including where they are likely to occur and what can be done to reduce losses from future <span class="hlt">earthquakes</span>, but not enough has been done to prepare for future <span class="hlt">earthquakes</span>. The handbook describes such preparations that can be taken by individual residents before an <span class="hlt">earthquake</span> to be safe and protect property.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_21 --> <div id="page_22" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="421"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://peer.berkeley.edu/links.html','SCIGOVWS'); return false;" href="http://peer.berkeley.edu/links.html"><span>Important <span class="hlt">Earthquake</span> Engineering Resources</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>PEER logo Pacific <span class="hlt">Earthquake</span> <em>Engineering</em> Research Center home about peer news events research <em>Engineering</em> Resources Site Map Search Important <span class="hlt">Earthquake</span> <em>Engineering</em> Resources - American Concrete Institute Motion Observation Systems (COSMOS) - Consortium of Universities for Research in <span class="hlt">Earthquake</span> <em>Engineering</em></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.T43D3039C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.T43D3039C"><span>Repeating <span class="hlt">Earthquakes</span> Following an Mw 4.4 <span class="hlt">Earthquake</span> Near Luther, Oklahoma</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Clements, T.; Keranen, K. M.; Savage, H. M.</p> <p>2015-12-01</p> <p>An Mw 4.4 <span class="hlt">earthquake</span> on April 16, 2013 near Luther, OK was one of the earliest M4+ <span class="hlt">earthquakes</span> in central Oklahoma, following the Prague sequence in 2011. A network of four local broadband seismometers deployed within a day of the Mw 4.4 event, along with six Oklahoma netquake stations, recorded more than 500 aftershocks in the two weeks following the Luther <span class="hlt">earthquake</span>. Here we use HypoDD (Waldhauser & Ellsworth, 2000) and waveform cross-correlation to obtain precise aftershock locations. The location uncertainty, calculated using the SVD method in HypoDD, is ~15 m horizontally and ~ 35 m vertically. The <span class="hlt">earthquakes</span> define a near vertical, NE-SW striking fault plane. Events occur at depths from 2 km to 3.5 km within the granitic basement, with a small fraction of events shallower, near the sediment-basement interface. <span class="hlt">Earthquakes</span> occur within a zone of ~200 meters thickness on either side of the best-fitting fault surface. We use an equivalency class algorithm to identity clusters of repeating events, defined as event pairs with median three-component correlation > 0.97 across common stations (Aster & Scott, 1993). Repeating events occur as doublets of only two events in over 50% of cases; overall, 41% of <span class="hlt">earthquakes</span> recorded occur as repeating events. The recurrence intervals for the repeating events range from minutes to days, with common recurrence intervals of less than two minutes. While clusters occur in tight dimensions, commonly of 80 m x 200 m, aftershocks occur in 3 distinct ~2km x 2km-sized patches along the fault. Our analysis suggests that with rapidly deployed local arrays, the plethora of ~Mw 4 <span class="hlt">earthquakes</span> occurring in Oklahoma and Southern Kansas can be used to investigate the <span class="hlt">earthquake</span> rupture process and the role of damage zones.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=continental+AND+drift&pg=2&id=EJ211635','ERIC'); return false;" href="https://eric.ed.gov/?q=continental+AND+drift&pg=2&id=EJ211635"><span><span class="hlt">Earthquake</span> Hazards.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Donovan, Neville</p> <p>1979-01-01</p> <p>Provides a survey and a review of <span class="hlt">earthquake</span> activity and global tectonics from the advancement of the theory of continental drift to the present. Topics include: an identification of the major seismic regions of the earth, seismic measurement techniques, seismic design criteria for buildings, and the prediction of <span class="hlt">earthquakes</span>. (BT)</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70169168','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70169168"><span><span class="hlt">Earthquakes</span>, May-June 1981</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1981-01-01</p> <p>The months of May and June were somewhat quiet, seismically speaking. There was one major <span class="hlt">earthquake</span> (7.0-7.9) off the west coast of South Island, New Zealand. The most destructive <span class="hlt">earthquake</span> during this reporting period was in southern Iran on June 11 which caused fatalities and extensive damage. Peru also experienced a destructive <span class="hlt">earthquake</span> on June 22 which caused fatalities and damage. In the United States, a number of <span class="hlt">earthquakes</span> were experienced, but none caused significant damage. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70188363','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70188363"><span>ViscoSim <span class="hlt">Earthquake</span> Simulator</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Pollitz, Fred</p> <p>2012-01-01</p> <p>Synthetic seismicity simulations have been explored by the Southern California <span class="hlt">Earthquake</span> Center (SCEC) <span class="hlt">Earthquake</span> Simulators Group in order to guide long‐term forecasting efforts related to the Unified California <span class="hlt">Earthquake</span> Rupture Forecast (Tullis et al., 2012a). In this study I describe the viscoelastic <span class="hlt">earthquake</span> simulator (ViscoSim) of Pollitz, 2009. Recapitulating to a large extent material previously presented by Pollitz (2009, 2011) I describe its implementation of synthetic ruptures and how it differs from other simulators being used by the group.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20010125646&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dearthquakes','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20010125646&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D70%26Ntt%3Dearthquakes"><span>Earth-Atmospheric Coupling During Strong <span class="hlt">Earthquakes</span> by Analyzing MODIS Data</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Ouzounov, Dimitar; Williams, Robin G.; Freund, Friedemann</p> <p>2001-01-01</p> <p>Interactions between the Earth and the atmosphere during major <span class="hlt">earthquakes</span> (M greater than 5) are the subject of this investigation. Recently a mechanism has been proposed predicting the build-up of positive ground potentials prior to strong <span class="hlt">earthquake</span> activity. Connected phenomena include: transient conductivity of rocks, injection of currents, possibly also electromagnetic emission and light emission from high points at the surface of the Earth. To understand this process we analyze vertical atmospheric profiles, land surface and brightness (temperature) data, using the Moderate Resolution Imaging Spectroradiometer (MODIS) onboard NASA's Terra satellite launched in December 1999. MODIS covers the entire Earth every 1-2 days in 36 wavelength bands (20 visible and 16 infrared) at different spatial resolutions (250 m, 500 m, and 1 km). Using MODIS data we look for correlations between the atmospheric dynamics and solid Earth processes for the January 2001 strong <span class="hlt">earthquakes</span> in San Salvador and <span class="hlt">India</span>. As part of the build-up of positive grounds potential, an IR luminescence is predicted to occur in the 8-12 micrometer band. We use the MODIS data to differentiate between true "thermal" signals and IR luminescence. Indeed, on the basis of a temporal and spatial distribution analysis, a thermal anomaly pattern is found that appears to be related to the seismic activity. Aerosol content and atmospheric instability parameters also change when ground charges build up causing ion emission and leading to a thin aerosol layer over land. We analyze the aerosol content, atmospheric pressure, moisture profile and lifted index. Anomalous trends have been identified in few days prior to the main shocks. The significance of this observation should be explored further using other data sets.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017JAGeo..11..179P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017JAGeo..11..179P"><span>Options for developing modernized geodetic datum for Nepal following the April 25, 2015 Mw7.8 Gorkha <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pearson, Chris; Manandhar, Niraj; Denys, Paul</p> <p>2017-09-01</p> <p>Along with the damage to buildings and infrastructure, the April 25, 2015 Mw7.8 Gorkha <span class="hlt">earthquake</span> caused significant deformation over a large area of eastern Nepal with displacements of over 2 m recorded in the vicinity of Kathmandu. Nepal currently uses a classical datum developed in 1984 by the Royal (UK) Engineers in collaboration with the Nepal Survey Department. It has served Nepal well; however, the recent <span class="hlt">earthquakes</span> have provided an impetus for developing a semi-dynamic datum that will be based on ITRF2014 and have the capacity to correct for tectonic deformation. In the scenario we present here, the datum would be based on ITRF2014 with a reference epoch set some time after the end of the current sequence of <span class="hlt">earthquakes</span>. The deformation model contains a grid of the secular velocity field combined with models of the Gorkha <span class="hlt">Earthquake</span> and the May 12 Mw7.3 aftershock. We have developed a preliminary velocity field by collating GPS derived crustal velocities from four previous studies for Nepal and adjacent parts of China and <span class="hlt">India</span> and aligning them to the ITRF. Patches for the co-seismic part of the deformation for the Gorkha <span class="hlt">earthquake</span> and the May 12, 2015 Mw 7.2 aftershock are based on published dislocation models. High order control would be a CORS network based around the existing Nepal GPS Array. Coordinates for existing lower order control would be determined by readjusting existing survey measurements and these would be combined with a series of new control stations spread throughout Nepal.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018Tectp.724..137M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018Tectp.724..137M"><span><span class="hlt">Earthquake</span> damage orientation to infer seismic parameters in archaeological sites and historical <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Martín-González, Fidel</p> <p>2018-01-01</p> <p>Studies to provide information concerning seismic parameters and seismic sources of historical and archaeological seismic events are used to better evaluate the seismic hazard of a region. This is of especial interest when no surface rupture is recorded or the seismogenic fault cannot be identified. The orientation pattern of the <span class="hlt">earthquake</span> damage (ED) (e.g., fallen columns, dropped key stones) that affected architectonic elements of cities after <span class="hlt">earthquakes</span> has been traditionally used in historical and archaeoseismological studies to infer seismic parameters. However, in the literature depending on the authors, the parameters that can be obtained are contradictory (it has been proposed: the epicenter location, the orientation of the P-waves, the orientation of the compressional strain and the fault kinematics) and authors even question these relations with the <span class="hlt">earthquake</span> damage. The <span class="hlt">earthquakes</span> of Lorca in 2011, Christchurch in 2011 and Emilia Romagna in 2012 present an opportunity to measure systematically a large number and wide variety of <span class="hlt">earthquake</span> damage in historical buildings (the same structures that are used in historical and archaeological studies). The damage pattern orientation has been compared with modern instrumental data, which is not possible in historical and archaeoseismological studies. From measurements and quantification of the orientation patterns in the studied <span class="hlt">earthquakes</span>, it is observed that there is a systematic pattern of the <span class="hlt">earthquake</span> damage orientation (EDO) in the proximity of the seismic source (fault trace) (<10 km). The EDO in these <span class="hlt">earthquakes</span> is normal to the fault trend (±15°). This orientation can be generated by a pulse of motion that in the near fault region has a distinguishable acceleration normal to the fault due to the polarization of the S-waves. Therefore, the <span class="hlt">earthquake</span> damage orientation could be used to estimate the seismogenic fault trend of historical <span class="hlt">earthquakes</span> studies where no instrumental data are available.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70176503','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70176503"><span><span class="hlt">Earthquakes</span>, March-April, 1993</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, Waverly J.</p> <p>1993-01-01</p> <p>Worldwide, only one major <span class="hlt">earthquake</span> (7.0<M<8.0) occurred during this reporting period. This <span class="hlt">earthquake</span>, a magnitude 7.2 shock, struck the Santa Cruz Islands region in the South Pacific on March 6. <span class="hlt">Earthquake</span>-related deaths occurred in the Fiji Islands, China, and Peru.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.earthquakeconference.org','SCIGOVWS'); return false;" href="http://www.earthquakeconference.org"><span>2016 National <span class="hlt">Earthquake</span> Conference</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Thank you to our Presenting Sponsor, California <em><span class="hlt">Earthquake</span></em> Authority. What's New? What's Next ? What's Your Role in Building a National Strategy? The National <em><span class="hlt">Earthquake</span></em> Conference (NEC) is a , state government leaders, social science practitioners, U.S. State and Territorial <em><span class="hlt">Earthquake</span></em> Managers</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70100882','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70100882"><span>The music of <span class="hlt">earthquakes</span> and <span class="hlt">Earthquake</span> Quartet #1</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Michael, Andrew J.</p> <p>2013-01-01</p> <p><span class="hlt">Earthquake</span> Quartet #1, my composition for voice, trombone, cello, and seismograms, is the intersection of listening to <span class="hlt">earthquakes</span> as a seismologist and performing music as a trombonist. Along the way, I realized there is a close relationship between what I do as a scientist and what I do as a musician. A musician controls the source of the sound and the path it travels through their instrument in order to make sound waves that we hear as music. An <span class="hlt">earthquake</span> is the source of waves that travel along a path through the earth until reaching us as shaking. It is almost as if the earth is a musician and people, including seismologists, are metaphorically listening and trying to understand what the music means.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ISPAr42W7..461D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ISPAr42W7..461D"><span>Tsunami Risk Assessment Modelling in Chabahar Port, Iran</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Delavar, M. R.; Mohammadi, H.; Sharifi, M. A.; Pirooz, M. D.</p> <p>2017-09-01</p> <p>The well-known historical tsunami in the Makran Subduction Zone (MSZ) region was generated by the <span class="hlt">earthquake</span> of November 28, 1945 in Makran Coast in the North of Oman Sea. This destructive tsunami killed over 4,000 people in Southern Pakistan and <span class="hlt">India</span>, caused great loss of life and devastation along the coasts of Western <span class="hlt">India</span>, Iran and Oman. According to the report of "Remembering the 1945 Makran Tsunami", compiled by the Intergovernmental Oceanographic Commission (UNESCO/IOC), the maximum inundation of Chabahar port was 367 m toward the dry land, which had a height of 3.6 meters from the sea level. In addition, the maximum amount of inundation at Pasni (Pakistan) reached to 3 km from the coastline. For the two beaches of <span class="hlt">Gujarat</span> (<span class="hlt">India</span>) and Oman the maximum run-up height was 3 m from the sea level. In this paper, we first use Makran 1945 seismic parameters to simulate the tsunami in generation, propagation and inundation phases. The effect of tsunami on Chabahar port is simulated using the ComMIT model which is based on the Method of Splitting Tsunami (MOST). In this process the results are compared with the documented eyewitnesses and some reports from researchers for calibration and validation of the result. Next we have used the model to perform risk assessment for Chabahar port in the south of Iran with the worst case scenario of the tsunami. The simulated results showed that the tsunami waves will reach Chabahar coastline 11 minutes after generation and 9 minutes later, over 9.4 Km2 of the dry land will be flooded with maximum wave amplitude reaching up to 30 meters.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeoJI.212.1331N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeoJI.212.1331N"><span><span class="hlt">Earthquake</span> triggering in southeast Africa following the 2012 Indian Ocean <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Neves, Miguel; Custódio, Susana; Peng, Zhigang; Ayorinde, Adebayo</p> <p>2018-02-01</p> <p>In this paper we present evidence of <span class="hlt">earthquake</span> dynamic triggering in southeast Africa. We analysed seismic waveforms recorded at 53 broad-band and short-period stations in order to identify possible increases in the rate of microearthquakes and tremor due to the passage of teleseismic waves generated by the Mw8.6 2012 Indian Ocean <span class="hlt">earthquake</span>. We found evidence of triggered local <span class="hlt">earthquakes</span> and no evidence of triggered tremor in the region. We assessed the statistical significance of the increase in the number of local <span class="hlt">earthquakes</span> using β-statistics. Statistically significant dynamic triggering of local <span class="hlt">earthquakes</span> was observed at 7 out of the 53 analysed stations. Two of these stations are located in the northeast coast of Madagascar and the other five stations are located in the Kaapvaal Craton, southern Africa. We found no evidence of dynamically triggered seismic activity in stations located near the structures of the East African Rift System. Hydrothermal activity exists close to the stations that recorded dynamic triggering, however, it also exists near the East African Rift System structures where no triggering was observed. Our results suggest that factors other than solely tectonic regime and geothermalism are needed to explain the mechanisms that underlie <span class="hlt">earthquake</span> triggering.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.T23I..07L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.T23I..07L"><span>Toward real-time regional <span class="hlt">earthquake</span> simulation of Taiwan <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lee, S.; Liu, Q.; Tromp, J.; Komatitsch, D.; Liang, W.; Huang, B.</p> <p>2013-12-01</p> <p>We developed a Real-time Online <span class="hlt">earthquake</span> Simulation system (ROS) to simulate regional <span class="hlt">earthquakes</span> in Taiwan. The ROS uses a centroid moment tensor solution of seismic events from a Real-time Moment Tensor monitoring system (RMT), which provides all the point source parameters including the event origin time, hypocentral location, moment magnitude and focal mechanism within 2 minutes after the occurrence of an <span class="hlt">earthquake</span>. Then, all of the source parameters are automatically forwarded to the ROS to perform an <span class="hlt">earthquake</span> simulation, which is based on a spectral-element method (SEM). We have improved SEM mesh quality by introducing a thin high-resolution mesh layer near the surface to accommodate steep and rapidly varying topography. The mesh for the shallow sedimentary basin is adjusted to reflect its complex geometry and sharp lateral velocity contrasts. The grid resolution at the surface is about 545 m, which is sufficient to resolve topography and tomography data for simulations accurate up to 1.0 Hz. The ROS is also an infrastructural service, making online <span class="hlt">earthquake</span> simulation feasible. Users can conduct their own <span class="hlt">earthquake</span> simulation by providing a set of source parameters through the ROS webpage. For visualization, a ShakeMovie and ShakeMap are produced during the simulation. The time needed for one event is roughly 3 minutes for a 70 sec ground motion simulation. The ROS is operated online at the Institute of Earth Sciences, Academia Sinica (http://ros.earth.sinica.edu.tw/). Our long-term goal for the ROS system is to contribute to public earth science outreach and to realize seismic ground motion prediction in real-time.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008AGUFM.S52A..08J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008AGUFM.S52A..08J"><span>Geophysical Anomalies and <span class="hlt">Earthquake</span> Prediction</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jackson, D. D.</p> <p>2008-12-01</p> <p>Finding anomalies is easy. Predicting <span class="hlt">earthquakes</span> convincingly from such anomalies is far from easy. Why? Why have so many beautiful geophysical abnormalities not led to successful prediction strategies? What is <span class="hlt">earthquake</span> prediction? By my definition it is convincing information that an <span class="hlt">earthquake</span> of specified size is temporarily much more likely than usual in a specific region for a specified time interval. We know a lot about normal <span class="hlt">earthquake</span> behavior, including locations where <span class="hlt">earthquake</span> rates are higher than elsewhere, with estimable rates and size distributions. We know that <span class="hlt">earthquakes</span> have power law size distributions over large areas, that they cluster in time and space, and that aftershocks follow with power-law dependence on time. These relationships justify prudent protective measures and scientific investigation. <span class="hlt">Earthquake</span> prediction would justify exceptional temporary measures well beyond those normal prudent actions. Convincing <span class="hlt">earthquake</span> prediction would result from methods that have demonstrated many successes with few false alarms. Predicting <span class="hlt">earthquakes</span> convincingly is difficult for several profound reasons. First, <span class="hlt">earthquakes</span> start in tiny volumes at inaccessible depth. The power law size dependence means that tiny unobservable ones are frequent almost everywhere and occasionally grow to larger size. Thus prediction of important <span class="hlt">earthquakes</span> is not about nucleation, but about identifying the conditions for growth. Second, <span class="hlt">earthquakes</span> are complex. They derive their energy from stress, which is perniciously hard to estimate or model because it is nearly singular at the margins of cracks and faults. Physical properties vary from place to place, so the preparatory processes certainly vary as well. Thus establishing the needed track record for validation is very difficult, especially for large events with immense interval times in any one location. Third, the anomalies are generally complex as well. Electromagnetic anomalies in particular require</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017GSL.....4....7H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017GSL.....4....7H"><span>Historical <span class="hlt">earthquake</span> research in Austria</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hammerl, Christa</p> <p>2017-12-01</p> <p>Austria has a moderate seismicity, and on average the population feels 40 <span class="hlt">earthquakes</span> per year or approximately three <span class="hlt">earthquakes</span> per month. A severe <span class="hlt">earthquake</span> with light building damage is expected roughly every 2 to 3 years in Austria. Severe damage to buildings ( I 0 > 8° EMS) occurs significantly less frequently, the average period of recurrence is about 75 years. For this reason the historical <span class="hlt">earthquake</span> research has been of special importance in Austria. The interest in historical <span class="hlt">earthquakes</span> in the past in the Austro-Hungarian Empire is outlined, beginning with an initiative of the Austrian Academy of Sciences and the development of historical <span class="hlt">earthquake</span> research as an independent research field after the 1978 "Zwentendorf plebiscite" on whether the nuclear power plant will start up. The applied methods are introduced briefly along with the most important studies and last but not least as an example of a recently carried out case study, one of the strongest past <span class="hlt">earthquakes</span> in Austria, the <span class="hlt">earthquake</span> of 17 July 1670, is presented. The research into historical <span class="hlt">earthquakes</span> in Austria concentrates on seismic events of the pre-instrumental period. The investigations are not only of historical interest, but also contribute to the completeness and correctness of the Austrian <span class="hlt">earthquake</span> catalogue, which is the basis for seismic hazard analysis and as such benefits the public, communities, civil engineers, architects, civil protection, and many others.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S13D..02V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S13D..02V"><span>Unraveling <span class="hlt">earthquake</span> stresses: Insights from dynamically triggered and induced <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Velasco, A. A.; Alfaro-Diaz, R. A.</p> <p>2017-12-01</p> <p>Induced seismicity, <span class="hlt">earthquakes</span> caused by anthropogenic activity, has more than doubled in the last several years resulting from practices related to oil and gas production. Furthermore, large <span class="hlt">earthquakes</span> have been shown to promote the triggering of other events within two fault lengths (static triggering), due to static stresses caused by physical movement along the fault, and also remotely from the passage of seismic waves (dynamic triggering). Thus, in order to understand the mechanisms for <span class="hlt">earthquake</span> failure, we investigate regions where natural, induced, and dynamically triggered events occur, and specifically target Oklahoma. We first analyze data from EarthScope's USArray Transportable Array (TA) and local seismic networks implementing an optimized (STA/LTA) detector in order to develop local detection and <span class="hlt">earthquake</span> catalogs. After we identify triggered events through statistical analysis, and perform a stress analysis to gain insight on the stress-states leading to triggered <span class="hlt">earthquake</span> failure. We use our observations to determine the role of different transient stresses in contributing to natural and induced seismicity by comparing these stresses to regional stress orientation. We also delineate critically stressed regions of triggered seismicity that may indicate areas susceptible to <span class="hlt">earthquake</span> hazards associated with sustained fluid injection in provinces of induced seismicity. Anthropogenic injection and extraction activity can alter the stress state and fluid flow within production basins. By analyzing the stress release of these ancient faults caused by dynamic stresses, we may be able to determine if fluids are solely responsible for increased seismic activity in induced regions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70023299','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70023299"><span><span class="hlt">Earthquake</span> triggering by seismic waves following the landers and hector mine <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Gomberg, J.; Reasenberg, P.A.; Bodin, P.; Harris, R.A.</p> <p>2001-01-01</p> <p>The proximity and similarity of the 1992, magnitude 7.3 Landers and 1999, magnitude 7.1 Hector Mine <span class="hlt">earthquakes</span> in California permit testing of <span class="hlt">earthquake</span> triggering hypotheses not previously possible. The Hector Mine <span class="hlt">earthquake</span> confirmed inferences that transient, oscillatory 'dynamic' deformations radiated as seismic waves can trigger seismicity rate increases, as proposed for the Landers <span class="hlt">earthquake</span>1-6. Here we quantify the spatial and temporal patterns of the seismicity rate changes7. The seismicity rate increase was to the north for the Landers <span class="hlt">earthquake</span> and primarily to the south for the Hector Mine <span class="hlt">earthquake</span>. We suggest that rupture directivity results in elevated dynamic deformations north and south of the Landers and Hector Mine faults, respectively, as evident in the asymmetry of the recorded seismic velocity fields. Both dynamic and static stress changes seem important for triggering in the near field with dynamic stress changes dominating at greater distances. Peak seismic velocities recorded for each <span class="hlt">earthquake</span> suggest the existence of, and place bounds on, dynamic triggering thresholds. These thresholds vary from a few tenths to a few MPa in most places, depend on local conditions, and exceed inferred static thresholds by more than an order of magnitude. At some sites, the onset of triggering was delayed until after the dynamic deformations subsided. Physical mechanisms consistent with all these observations may be similar to those that give rise to liquefaction or cyclic fatigue.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.S43D2818L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.S43D2818L"><span>Real-Time Science on Social Media: The Example of Twitter in the Minutes, Hours, Days after the 2015 M7.8 Nepal <span class="hlt">Earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lomax, A.; Bossu, R.; Mazet-Roux, G.</p> <p>2015-12-01</p> <p>Scientific information on disasters such as <span class="hlt">earthquakes</span> typically comes firstly from official organizations, news reports and interviews with experts, and later from scientific presentations and peer-reviewed articles. With the advent of the Internet and social media, this information is available in real-time from automated systems and within a dynamic, collaborative interaction between scientific experts, responders and the public. After the 2015 M7.8 Nepal <span class="hlt">earthquake</span>, Twitter Tweets from earth scientists* included information, analysis, commentary and discussion on <span class="hlt">earthquake</span> parameters (location, size, mechanism, rupture extent, high-frequency radiation, …), <span class="hlt">earthquake</span> effects (distribution of felt shaking and damage, triggered seismicity, landslides, …), <span class="hlt">earthquake</span> rumors (e.g. the imminence of a larger event) and other <span class="hlt">earthquake</span> information and observations (aftershock forecasts, statistics and maps, source and regional tectonics, seismograms, GPS, InSAR, photos/videos, …).In the future (while taking into account security, false or erroneous information and identity verification), collaborative, real-time science on social media after a disaster will give earlier and better scientific understanding and dissemination of public information, and enable improved emergency response and disaster management.* A sample of scientific Tweets after the 2015 Nepal <span class="hlt">earthquake</span>: In the first minutes: "mb5.9 Mwp7.4 <span class="hlt">earthquake</span> Nepal 2015.04.25-06:11:25UTC", "Major <span class="hlt">earthquake</span> shakes Nepal 8 min ago", "Epicenter between Pokhara and Kathmandu", "Major <span class="hlt">earthquake</span> shakes Nepal 18 min ago. Effects derived from witnesses' reports". In the first hour: "shallow thrust faulting to North under Himalayas", "a very large and shallow event ... Mw7.6-7.7", "aftershocks extend east and south of Kathmandu, so likely ruptured beneath city", "Valley-blocking landslides must be a very real worry". In the first day: "M7.8 <span class="hlt">earthquake</span> in Nepal 2hr ago: destructive in Kathmandu Valley and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012NHESS..12..575Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012NHESS..12..575Y"><span>Analysis of pre-<span class="hlt">earthquake</span> ionospheric anomalies before the global M = 7.0+ <span class="hlt">earthquakes</span> in 2010</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yao, Y. B.; Chen, P.; Zhang, S.; Chen, J. J.; Yan, F.; Peng, W. F.</p> <p>2012-03-01</p> <p>The pre-<span class="hlt">earthquake</span> ionospheric anomalies that occurred before the global M = 7.0+ <span class="hlt">earthquakes</span> in 2010 are investigated using the total electron content (TEC) from the global ionosphere map (GIM). We analyze the possible causes of the ionospheric anomalies based on the space environment and magnetic field status. Results show that some anomalies are related to the <span class="hlt">earthquakes</span>. By analyzing the time of occurrence, duration, and spatial distribution of these ionospheric anomalies, a number of new conclusions are drawn, as follows: <span class="hlt">earthquake</span>-related ionospheric anomalies are not bound to appear; both positive and negative anomalies are likely to occur; and the <span class="hlt">earthquake</span>-related ionospheric anomalies discussed in the current study occurred 0-2 days before the associated <span class="hlt">earthquakes</span> and in the afternoon to sunset (i.e. between 12:00 and 20:00 local time). Pre-<span class="hlt">earthquake</span> ionospheric anomalies occur mainly in areas near the epicenter. However, the maximum affected area in the ionosphere does not coincide with the vertical projection of the epicenter of the subsequent <span class="hlt">earthquake</span>. The directions deviating from the epicenters do not follow a fixed rule. The corresponding ionospheric effects can also be observed in the magnetically conjugated region. However, the probability of the anomalies appearance and extent of the anomalies in the magnetically conjugated region are smaller than the anomalies near the epicenter. Deep-focus <span class="hlt">earthquakes</span> may also exhibit very significant pre-<span class="hlt">earthquake</span> ionospheric anomalies.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_22 --> <div id="page_23" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="441"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFMNH42A..01I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFMNH42A..01I"><span>Modeling, Forecasting and Mitigating Extreme <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ismail-Zadeh, A.; Le Mouel, J.; Soloviev, A.</p> <p>2012-12-01</p> <p>Recent <span class="hlt">earthquake</span> disasters highlighted the importance of multi- and trans-disciplinary studies of <span class="hlt">earthquake</span> risk. A major component of <span class="hlt">earthquake</span> disaster risk analysis is hazards research, which should cover not only a traditional assessment of ground shaking, but also studies of geodetic, paleoseismic, geomagnetic, hydrological, deep drilling and other geophysical and geological observations together with comprehensive modeling of <span class="hlt">earthquakes</span> and forecasting extreme events. Extreme <span class="hlt">earthquakes</span> (large magnitude and rare events) are manifestations of complex behavior of the lithosphere structured as a hierarchical system of blocks of different sizes. Understanding of physics and dynamics of the extreme events comes from observations, measurements and modeling. A quantitative approach to simulate <span class="hlt">earthquakes</span> in models of fault dynamics will be presented. The models reproduce basic features of the observed seismicity (e.g., the frequency-magnitude relationship, clustering of <span class="hlt">earthquakes</span>, occurrence of extreme seismic events). They provide a link between geodynamic processes and seismicity, allow studying extreme events, influence of fault network properties on seismic patterns and seismic cycles, and assist, in a broader sense, in <span class="hlt">earthquake</span> forecast modeling. Some aspects of predictability of large <span class="hlt">earthquakes</span> (how well can large <span class="hlt">earthquakes</span> be predicted today?) will be also discussed along with possibilities in mitigation of <span class="hlt">earthquake</span> disasters (e.g., on 'inverse' forensic investigations of <span class="hlt">earthquake</span> disasters).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/18292339','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/18292339"><span>Extending <span class="hlt">earthquakes</span>' reach through cascading.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Marsan, David; Lengliné, Olivier</p> <p>2008-02-22</p> <p><span class="hlt">Earthquakes</span>, whatever their size, can trigger other <span class="hlt">earthquakes</span>. Mainshocks cause aftershocks to occur, which in turn activate their own local aftershock sequences, resulting in a cascade of triggering that extends the reach of the initial mainshock. A long-lasting difficulty is to determine which <span class="hlt">earthquakes</span> are connected, either directly or indirectly. Here we show that this causal structure can be found probabilistically, with no a priori model nor parameterization. Large regional <span class="hlt">earthquakes</span> are found to have a short direct influence in comparison to the overall aftershock sequence duration. Relative to these large mainshocks, small <span class="hlt">earthquakes</span> collectively have a greater effect on triggering. Hence, cascade triggering is a key component in <span class="hlt">earthquake</span> interactions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.S53A2828G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.S53A2828G"><span><span class="hlt">Earthquake</span> Catalogue of the Caucasus</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Godoladze, T.; Gok, R.; Tvaradze, N.; Tumanova, N.; Gunia, I.; Onur, T.</p> <p>2016-12-01</p> <p>The Caucasus has a documented historical catalog stretching back to the beginning of the Christian era. Most of the largest historical <span class="hlt">earthquakes</span> prior to the 19th century are assumed to have occurred on active faults of the Greater Caucasus. Important <span class="hlt">earthquakes</span> include the Samtskhe <span class="hlt">earthquake</span> of 1283 (Ms˜7.0, Io=9); Lechkhumi-Svaneti <span class="hlt">earthquake</span> of 1350 (Ms˜7.0, Io=9); and the Alaverdi <span class="hlt">earthquake</span> of 1742 (Ms˜6.8, Io=9). Two significant historical <span class="hlt">earthquakes</span> that may have occurred within the Javakheti plateau in the Lesser Caucasus are the Tmogvi <span class="hlt">earthquake</span> of 1088 (Ms˜6.5, Io=9) and the Akhalkalaki <span class="hlt">earthquake</span> of 1899 (Ms˜6.3, Io =8-9). Large <span class="hlt">earthquakes</span> that occurred in the Caucasus within the period of instrumental observation are: Gori 1920; Tabatskuri 1940; Chkhalta 1963; Racha <span class="hlt">earthquake</span> of 1991 (Ms=7.0), is the largest event ever recorded in the region; Barisakho <span class="hlt">earthquake</span> of 1992 (M=6.5); Spitak <span class="hlt">earthquake</span> of 1988 (Ms=6.9, 100 km south of Tbilisi), which killed over 50,000 people in Armenia. Recently, permanent broadband stations have been deployed across the region as part of the various national networks (Georgia (˜25 stations), Azerbaijan (˜35 stations), Armenia (˜14 stations)). The data from the last 10 years of observation provides an opportunity to perform modern, fundamental scientific investigations. In order to improve seismic data quality a catalog of all instrumentally recorded <span class="hlt">earthquakes</span> has been compiled by the IES (Institute of Earth Sciences/NSMC, Ilia State University) in the framework of regional joint project (Armenia, Azerbaijan, Georgia, Turkey, USA) "Probabilistic Seismic Hazard Assessment (PSHA) in the Caucasus. The catalogue consists of more then 80,000 events. First arrivals of each <span class="hlt">earthquake</span> of Mw>=4.0 have been carefully examined. To reduce calculation errors, we corrected arrivals from the seismic records. We improved locations of the events and recalculate Moment magnitudes in order to obtain unified magnitude</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70168757','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70168757"><span><span class="hlt">Earthquakes</span>, July-August 1992</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1992-01-01</p> <p>There were two major <span class="hlt">earthquakes</span> (7.0≤M<8.0) during this reporting period. A magnitude 7.5 <span class="hlt">earthquake</span> occurred in Kyrgyzstan on August 19 and a magnitude 7.0 quake struck the Ascension Island region on August 28. In southern California, aftershocks of the magnitude 7.6 <span class="hlt">earthquake</span> on June 28, 1992, continued. One of these aftershocks caused damage and injuries, and at least one other aftershock caused additional damage. <span class="hlt">Earthquake</span>-related fatalities were reportred in Kyrgzstan and Pakistan. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008PApGe.165..777A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008PApGe.165..777A"><span><span class="hlt">Earthquakes</span>: Recurrence and Interoccurrence Times</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Abaimov, S. G.; Turcotte, D. L.; Shcherbakov, R.; Rundle, J. B.; Yakovlev, G.; Goltz, C.; Newman, W. I.</p> <p>2008-04-01</p> <p>The purpose of this paper is to discuss the statistical distributions of recurrence times of <span class="hlt">earthquakes</span>. Recurrence times are the time intervals between successive <span class="hlt">earthquakes</span> at a specified location on a specified fault. Although a number of statistical distributions have been proposed for recurrence times, we argue in favor of the Weibull distribution. The Weibull distribution is the only distribution that has a scale-invariant hazard function. We consider three sets of characteristic <span class="hlt">earthquakes</span> on the San Andreas fault: (1) The Parkfield <span class="hlt">earthquakes</span>, (2) the sequence of <span class="hlt">earthquakes</span> identified by paleoseismic studies at the Wrightwood site, and (3) an example of a sequence of micro-repeating <span class="hlt">earthquakes</span> at a site near San Juan Bautista. In each case we make a comparison with the applicable Weibull distribution. The number of <span class="hlt">earthquakes</span> in each of these sequences is too small to make definitive conclusions. To overcome this difficulty we consider a sequence of <span class="hlt">earthquakes</span> obtained from a one million year “Virtual California” simulation of San Andreas <span class="hlt">earthquakes</span>. Very good agreement with a Weibull distribution is found. We also obtain recurrence statistics for two other model studies. The first is a modified forest-fire model and the second is a slider-block model. In both cases good agreements with Weibull distributions are obtained. Our conclusion is that the Weibull distribution is the preferred distribution for estimating the risk of future <span class="hlt">earthquakes</span> on the San Andreas fault and elsewhere.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012E%26PSL.333...46M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012E%26PSL.333...46M"><span>Localized crustal deformation in the Godavari failed rift, <span class="hlt">India</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mahesh, P.; Gahalaut, V. K.; Catherine, J. K.; Ambikapathy, A.; Kundu, Bhaskar; Bansal, Amit; Chadha, R. K.; Narsaiah, M.</p> <p>2012-06-01</p> <p>Six years of GPS measurements of crustal deformation in the Godavari failed rift (GFR) of stable <span class="hlt">India</span> plate suggest very localized deformation. Elsewhere, all along the GFR the deformation is very low (<1.5 mm/yr). Localized deformation (up to 3.3±0.5 mm/yr) at least at two sites, implying compression on steep faults located on the southern margin of the GFR, is coincident with the region characterized by high level low-magnitude seismicity of past six years and implies strain accumulation for future moderate to strong magnitude <span class="hlt">earthquake</span> in the region. The localized deformation is consistent with the view about deformation in such regions where seismicity migrates and deformation rate changes with time.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018PApGe.175..661L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018PApGe.175..661L"><span>Natural Time and Nowcasting <span class="hlt">Earthquakes</span>: Are Large Global <span class="hlt">Earthquakes</span> Temporally Clustered?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Luginbuhl, Molly; Rundle, John B.; Turcotte, Donald L.</p> <p>2018-02-01</p> <p>The objective of this paper is to analyze the temporal clustering of large global <span class="hlt">earthquakes</span> with respect to natural time, or interevent count, as opposed to regular clock time. To do this, we use two techniques: (1) nowcasting, a new method of statistically classifying seismicity and seismic risk, and (2) time series analysis of interevent counts. We chose the sequences of M_{λ } ≥ 7.0 and M_{λ } ≥ 8.0 <span class="hlt">earthquakes</span> from the global centroid moment tensor (CMT) catalog from 2004 to 2016 for analysis. A significant number of these <span class="hlt">earthquakes</span> will be aftershocks of the largest events, but no satisfactory method of declustering the aftershocks in clock time is available. A major advantage of using natural time is that it eliminates the need for declustering aftershocks. The event count we utilize is the number of small <span class="hlt">earthquakes</span> that occur between large <span class="hlt">earthquakes</span>. The small <span class="hlt">earthquake</span> magnitude is chosen to be as small as possible, such that the catalog is still complete based on the Gutenberg-Richter statistics. For the CMT catalog, starting in 2004, we found the completeness magnitude to be M_{σ } ≥ 5.1. For the nowcasting method, the cumulative probability distribution of these interevent counts is obtained. We quantify the distribution using the exponent, β, of the best fitting Weibull distribution; β = 1 for a random (exponential) distribution. We considered 197 <span class="hlt">earthquakes</span> with M_{λ } ≥ 7.0 and found β = 0.83 ± 0.08. We considered 15 <span class="hlt">earthquakes</span> with M_{λ } ≥ 8.0, but this number was considered too small to generate a meaningful distribution. For comparison, we generated synthetic catalogs of <span class="hlt">earthquakes</span> that occur randomly with the Gutenberg-Richter frequency-magnitude statistics. We considered a synthetic catalog of 1.97 × 10^5 M_{λ } ≥ 7.0 <span class="hlt">earthquakes</span> and found β = 0.99 ± 0.01. The random catalog converted to natural time was also random. We then generated 1.5 × 10^4 synthetic catalogs with 197 M_{λ } ≥ 7.0 in each catalog and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/16319414','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/16319414"><span>Validity of the construct of post-traumatic stress disorder in a low-income country: interview study of women in <span class="hlt">Gujarat</span>, <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mehta, Khyati; Vankar, Ganpat; Patel, Vikram</p> <p>2005-12-01</p> <p>The validity of the clinical construct of post-traumatic stress disorder (PTSD) has been questioned in non-Western cultures. This report describes in-depth interviews exploring the experiences of women who were traumatised by the communal riots in Ahmedabad, <span class="hlt">India</span>, in March 2002. Three specific narratives are presented which describe experiences that closely resemble re-experiencing, avoidance and hyperarousal. Thus, symptoms described as characteristic features of PTSD in biomedical classifications are clearly expressed by the women in our study, and are attributed by them to trauma and grief. We conclude that PTSD may be a relevant clinical construct in the Indian context.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMED53C3498H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMED53C3498H"><span><span class="hlt">Earthquake</span> and Tsunami booklet based on two Indonesia <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hayashi, Y.; Aci, M.</p> <p>2014-12-01</p> <p>Many destructive <span class="hlt">earthquakes</span> occurred during the last decade in Indonesia. These experiences are very important precepts for the world people who live in <span class="hlt">earthquake</span> and tsunami countries. We are collecting the testimonies of tsunami survivors to clarify successful evacuation process and to make clear the characteristic physical behaviors of tsunami near coast. We research 2 tsunami events, 2004 Indian Ocean tsunami and 2010 Mentawai slow <span class="hlt">earthquake</span> tsunami. Many video and photographs were taken by people at some places in 2004 Indian ocean tsunami disaster; nevertheless these were few restricted points. We didn't know the tsunami behavior in another place. In this study, we tried to collect extensive information about tsunami behavior not only in many places but also wide time range after the strong shake. In Mentawai case, the <span class="hlt">earthquake</span> occurred in night, so there are no impressive photos. To collect detail information about evacuation process from tsunamis, we contrived the interview method. This method contains making pictures of tsunami experience from the scene of victims' stories. In 2004 Aceh case, all survivors didn't know tsunami phenomena. Because there were no big <span class="hlt">earthquakes</span> with tsunami for one hundred years in Sumatra region, public people had no knowledge about tsunami. This situation was highly improved in 2010 Mentawai case. TV programs and NGO or governmental public education programs about tsunami evacuation are widespread in Indonesia. Many people know about fundamental knowledge of <span class="hlt">earthquake</span> and tsunami disasters. We made drill book based on victim's stories and painted impressive scene of 2 events. We used the drill book in disaster education event in school committee of west Java. About 80 % students and teachers evaluated that the contents of the drill book are useful for correct understanding.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70128256','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70128256"><span><span class="hlt">Earthquakes</span>: hydrogeochemical precursors</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Ingebritsen, Steven E.; Manga, Michael</p> <p>2014-01-01</p> <p><span class="hlt">Earthquake</span> prediction is a long-sought goal. Changes in groundwater chemistry before <span class="hlt">earthquakes</span> in Iceland highlight a potential hydrogeochemical precursor, but such signals must be evaluated in the context of long-term, multiparametric data sets.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70168770','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70168770"><span><span class="hlt">Earthquakes</span>, September-October 1993</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1993-01-01</p> <p>The fatalities in the United States were caused by two <span class="hlt">earthquakes</span> in southern Oregon on September 21. These <span class="hlt">earthquakes</span>, both with magnitude 6.0 and separated in time by about 2 hrs, led to the deaths of two people. One of these deaths was apparently due to a heart attack induced by the <span class="hlt">earthquake</span>. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ901261.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ901261.pdf"><span>Children's Ideas about <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Simsek, Canan Lacin</p> <p>2007-01-01</p> <p><span class="hlt">Earthquake</span>, a natural disaster, is among the fundamental problems of many countries. If people know how to protect themselves from <span class="hlt">earthquake</span> and arrange their life styles in compliance with this, damage they will suffer will reduce to that extent. In particular, a good training regarding <span class="hlt">earthquake</span> to be received in primary schools is considered…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMED21B0277C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMED21B0277C"><span>Excel, <span class="hlt">Earthquakes</span>, and Moneyball: exploring Cascadia <span class="hlt">earthquake</span> probabilities using spreadsheets and baseball analogies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Campbell, M. R.; Salditch, L.; Brooks, E. M.; Stein, S.; Spencer, B. D.</p> <p>2017-12-01</p> <p>Much recent media attention focuses on Cascadia's <span class="hlt">earthquake</span> hazard. A widely cited magazine article starts "An <span class="hlt">earthquake</span> will destroy a sizable portion of the coastal Northwest. The question is when." Stories include statements like "a massive <span class="hlt">earthquake</span> is overdue", "in the next 50 years, there is a 1-in-10 chance a "really big one" will erupt," or "the odds of the big Cascadia <span class="hlt">earthquake</span> happening in the next fifty years are roughly one in three." These lead students to ask where the quoted probabilities come from and what they mean. These probability estimates involve two primary choices: what data are used to describe when past <span class="hlt">earthquakes</span> happened and what models are used to forecast when future <span class="hlt">earthquakes</span> will happen. The data come from a 10,000-year record of large paleoearthquakes compiled from subsidence data on land and turbidites, offshore deposits recording submarine slope failure. <span class="hlt">Earthquakes</span> seem to have happened in clusters of four or five events, separated by gaps. <span class="hlt">Earthquakes</span> within a cluster occur more frequently and regularly than in the full record. Hence the next <span class="hlt">earthquake</span> is more likely if we assume that we are in the recent cluster that started about 1700 years ago, than if we assume the cluster is over. Students can explore how changing assumptions drastically changes probability estimates using easy-to-write and display spreadsheets, like those shown below. Insight can also come from baseball analogies. The cluster issue is like deciding whether to assume that a hitter's performance in the next game is better described by his lifetime record, or by the past few games, since he may be hitting unusually well or in a slump. The other big choice is whether to assume that the probability of an <span class="hlt">earthquake</span> is constant with time, or is small immediately after one occurs and then grows with time. This is like whether to assume that a player's performance is the same from year to year, or changes over their career. Thus saying "the chance of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26197482','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26197482"><span>Do <span class="hlt">Earthquakes</span> Shake Stock Markets?</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ferreira, Susana; Karali, Berna</p> <p>2015-01-01</p> <p>This paper examines how major <span class="hlt">earthquakes</span> affected the returns and volatility of aggregate stock market indices in thirty-five financial markets over the last twenty years. Results show that global financial markets are resilient to shocks caused by <span class="hlt">earthquakes</span> even if these are domestic. Our analysis reveals that, in a few instances, some macroeconomic variables and <span class="hlt">earthquake</span> characteristics (gross domestic product per capita, trade openness, bilateral trade flows, <span class="hlt">earthquake</span> magnitude, a tsunami indicator, distance to the epicenter, and number of fatalities) mediate the impact of <span class="hlt">earthquakes</span> on stock market returns, resulting in a zero net effect. However, the influence of these variables is market-specific, indicating no systematic pattern across global capital markets. Results also demonstrate that stock market volatility is unaffected by <span class="hlt">earthquakes</span>, except for Japan.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JAESc..87...56L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JAESc..87...56L"><span>Toward real-time regional <span class="hlt">earthquake</span> simulation II: Real-time Online <span class="hlt">earthquake</span> Simulation (ROS) of Taiwan <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lee, Shiann-Jong; Liu, Qinya; Tromp, Jeroen; Komatitsch, Dimitri; Liang, Wen-Tzong; Huang, Bor-Shouh</p> <p>2014-06-01</p> <p>We developed a Real-time Online <span class="hlt">earthquake</span> Simulation system (ROS) to simulate regional <span class="hlt">earthquakes</span> in Taiwan. The ROS uses a centroid moment tensor solution of seismic events from a Real-time Moment Tensor monitoring system (RMT), which provides all the point source parameters including the event origin time, hypocentral location, moment magnitude and focal mechanism within 2 min after the occurrence of an <span class="hlt">earthquake</span>. Then, all of the source parameters are automatically forwarded to the ROS to perform an <span class="hlt">earthquake</span> simulation, which is based on a spectral-element method (SEM). A new island-wide, high resolution SEM mesh model is developed for the whole Taiwan in this study. We have improved SEM mesh quality by introducing a thin high-resolution mesh layer near the surface to accommodate steep and rapidly varying topography. The mesh for the shallow sedimentary basin is adjusted to reflect its complex geometry and sharp lateral velocity contrasts. The grid resolution at the surface is about 545 m, which is sufficient to resolve topography and tomography data for simulations accurate up to 1.0 Hz. The ROS is also an infrastructural service, making online <span class="hlt">earthquake</span> simulation feasible. Users can conduct their own <span class="hlt">earthquake</span> simulation by providing a set of source parameters through the ROS webpage. For visualization, a ShakeMovie and ShakeMap are produced during the simulation. The time needed for one event is roughly 3 min for a 70 s ground motion simulation. The ROS is operated online at the Institute of Earth Sciences, Academia Sinica (http://ros.earth.sinica.edu.tw/). Our long-term goal for the ROS system is to contribute to public earth science outreach and to realize seismic ground motion prediction in real-time.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMEP12C..04M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMEP12C..04M"><span>Sedimentary Signatures of Submarine <span class="hlt">Earthquakes</span>: Deciphering the Extent of Sediment Remobilization from the 2011 Tohoku <span class="hlt">Earthquake</span> and Tsunami and 2010 Haiti <span class="hlt">Earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McHugh, C. M.; Seeber, L.; Moernaut, J.; Strasser, M.; Kanamatsu, T.; Ikehara, K.; Bopp, R.; Mustaque, S.; Usami, K.; Schwestermann, T.; Kioka, A.; Moore, L. M.</p> <p>2017-12-01</p> <p>The 2004 Sumatra-Andaman Mw9.3 and the 2011 Tohoku (Japan) Mw9.0 <span class="hlt">earthquakes</span> and tsunamis were huge geological events with major societal consequences. Both were along subduction boundaries and ruptured portions of these boundaries that had been deemed incapable of such events. Submarine strike-slip <span class="hlt">earthquakes</span>, such as the 2010 Mw7.0 in Haiti, are smaller but may be closer to population centers and can be similarly catastrophic. Both classes of <span class="hlt">earthquakes</span> remobilize sediment and leave distinct signatures in the geologic record by a wide range of processes that depends on both environment and <span class="hlt">earthquake</span> characteristics. Understanding them has the potential of greatly expanding the record of past <span class="hlt">earthquakes</span>, which is critical for geohazard analysis. Recent events offer precious ground truth about the <span class="hlt">earthquakes</span> and short-lived radioisotopes offer invaluable tools to identify sediments they remobilized. In the 2011 Mw9 Japan <span class="hlt">earthquake</span> they document the spatial extent of remobilized sediment from water depths of 626m in the forearc slope to trench depths of 8000m. Subbottom profiles, multibeam bathymetry and 40 piston cores collected by the R/V Natsushima and R/V Sonne expeditions to the Japan Trench document multiple turbidites and high-density flows. Core tops enriched in xs210Pb,137Cs and 134Cs reveal sediment deposited by the 2011 Tohoku <span class="hlt">earthquake</span> and tsunami. The thickest deposits (2m) were documented on a mid-slope terrace and trench (4000-8000m). Sediment was deposited on some terraces (600-3000m), but shed from the steep forearc slope (3000-4000m). The 2010 Haiti mainshock ruptured along the southern flank of Canal du Sud and triggered multiple nearshore sediment failures, generated turbidity currents and stirred fine sediment into suspension throughout this basin. A tsunami was modeled to stem from both sediment failures and tectonics. Remobilized sediment was tracked with short-lived radioisotopes from the nearshore, slope, in fault basins including the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/2007/1437/h/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/2007/1437/h/"><span>WGCEP Historical California <span class="hlt">Earthquake</span> Catalog</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Felzer, Karen R.; Cao, Tianqing</p> <p>2008-01-01</p> <p>This appendix provides an <span class="hlt">earthquake</span> catalog for California and the surrounding area. Our goal is to provide a listing for all known M > 5.5 <span class="hlt">earthquakes</span> that occurred from 1850-1932 and all known M > 4.0 <span class="hlt">earthquakes</span> that occurred from 1932-2006 within the region of 31.0 to 43.0 degrees North and -126.0 to -114.0 degrees West. Some pre-1932 <span class="hlt">earthquakes</span> 4 5, before the Northern California network was online. Some <span class="hlt">earthquakes</span> from 1900-1932, and particularly from 1910-1932 are also based on instrumental readings, but the quality of the instrumental record and the resulting analysis are much less precise than for later listings. A partial exception is for some of the largest <span class="hlt">earthquakes</span>, such as the San Francisco <span class="hlt">earthquake</span> of April 18, 1906, for which global teleseismic records (Wald et al. 1993) and geodetic measurements (Thatcher et al. 1906) have been used to help determine magnitudes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70169179','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70169179"><span><span class="hlt">Earthquakes</span>, September-October 1978</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1979-01-01</p> <p>The months of September and October were somewhat quiet seismically speaking. One major <span class="hlt">earthquake</span>, magnitude (M) 7.7 occurred in Iran on September 16. In Germany, a magntidue 5.0 <span class="hlt">earthquake</span> caused damage and considerable alarm to many people in parts of that country. In the United States, the largest <span class="hlt">earthquake</span> occurred along the California-Nevada border region. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70168759','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70168759"><span><span class="hlt">Earthquakes</span>, March-April 1991</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Person, W.J.</p> <p>1992-01-01</p> <p>Two major <span class="hlt">earthquakes</span> (7.0-7.9) occurred during this reporting period: a magnitude 7.6 in Costa Rica on April 22 and a magntidue 7.0 in the USSR on April 29. Destructive <span class="hlt">earthquakes</span> hit northern Peru on April 4 and 5. There were no destructive <span class="hlt">earthquakes</span> in the United States during this period. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.osti.gov/sciencecinema/biblio/1320783','SCIGOVIMAGE-SCICINEMA'); return false;" href="http://www.osti.gov/sciencecinema/biblio/1320783"><span>Can We Predict <span class="hlt">Earthquakes</span>?</span></a></p> <p><a target="_blank" href="http://www.osti.gov/sciencecinema/">ScienceCinema</a></p> <p>Johnson, Paul</p> <p>2018-01-16</p> <p>The only thing we know for sure about <span class="hlt">earthquakes</span> is that one will happen again very soon. <span class="hlt">Earthquakes</span> pose a vital yet puzzling set of research questions that have confounded scientists for decades, but new ways of looking at seismic information and innovative laboratory experiments are offering tantalizing clues to what triggers <span class="hlt">earthquakes</span> — and when.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_23 --> <div id="page_24" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="461"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=children+AND+interior&pg=7&id=ED438702','ERIC'); return false;" href="https://eric.ed.gov/?q=children+AND+interior&pg=7&id=ED438702"><span><span class="hlt">Earthquake</span> and Schools. [Videotape].</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Federal Emergency Management Agency, Washington, DC.</p> <p></p> <p>Designing schools to make them more <span class="hlt">earthquake</span> resistant and protect children from the catastrophic collapse of the school building is discussed in this videotape. It reveals that 44 of the 50 U.S. states are vulnerable to <span class="hlt">earthquake</span>, but most schools are structurally unprepared to take on the stresses that <span class="hlt">earthquakes</span> exert. The cost to the…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/2011/1118/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/2011/1118/"><span><span class="hlt">Earthquakes</span> in Arkansas and vicinity 1699-2010</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Dart, Richard L.; Ausbrooks, Scott M.</p> <p>2011-01-01</p> <p>This map summarizes approximately 300 years of <span class="hlt">earthquake</span> activity in Arkansas. It is one in a series of similar State <span class="hlt">earthquake</span> history maps. Work on the Arkansas map was done in collaboration with the Arkansas Geological Survey. The <span class="hlt">earthquake</span> data plotted on the map are from several sources: the Arkansas Geological Survey, the Center for <span class="hlt">Earthquake</span> Research and Information, the National Center for <span class="hlt">Earthquake</span> Engineering Research, and the Mississippi Department of Environmental Quality. In addition to <span class="hlt">earthquake</span> locations, other materials presented include seismic hazard and isoseismal maps and related text. <span class="hlt">Earthquakes</span> are a legitimate concern in Arkansas and parts of adjacent states. Arkansas has undergone a number of significant felt <span class="hlt">earthquakes</span> since 1811. At least two of these events caused property damage: a magnitude 4.7 <span class="hlt">earthquake</span> in 1931, and a magnitude 4.3 <span class="hlt">earthquake</span> in 1967. The map shows all historical and instrumentally located <span class="hlt">earthquakes</span> in Arkansas and vicinity between 1811 and 2010. The largest historic <span class="hlt">earthquake</span> in the vicinity of the State was an intensity XI event, on December 16, 1811; the first <span class="hlt">earthquake</span> in the New Madrid sequence. This violent event and the <span class="hlt">earthquakes</span> that followed caused considerable damage to the then sparsely settled region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S53B0696F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S53B0696F"><span><span class="hlt">Earthquake</span> Forecasting System in Italy</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Falcone, G.; Marzocchi, W.; Murru, M.; Taroni, M.; Faenza, L.</p> <p>2017-12-01</p> <p>In Italy, after the 2009 L'Aquila <span class="hlt">earthquake</span>, a procedure was developed for gathering and disseminating authoritative information about the time dependence of seismic hazard to help communities prepare for a potentially destructive <span class="hlt">earthquake</span>. The most striking time dependency of the <span class="hlt">earthquake</span> occurrence process is the time clustering, which is particularly pronounced in time windows of days and weeks. The Operational <span class="hlt">Earthquake</span> Forecasting (OEF) system that is developed at the Seismic Hazard Center (Centro di Pericolosità Sismica, CPS) of the Istituto Nazionale di Geofisica e Vulcanologia (INGV) is the authoritative source of seismic hazard information for Italian Civil Protection. The philosophy of the system rests on a few basic concepts: transparency, reproducibility, and testability. In particular, the transparent, reproducible, and testable <span class="hlt">earthquake</span> forecasting system developed at CPS is based on ensemble modeling and on a rigorous testing phase. Such phase is carried out according to the guidance proposed by the Collaboratory for the Study of <span class="hlt">Earthquake</span> Predictability (CSEP, international infrastructure aimed at evaluating quantitatively <span class="hlt">earthquake</span> prediction and forecast models through purely prospective and reproducible experiments). In the OEF system, the two most popular short-term models were used: the Epidemic-Type Aftershock Sequences (ETAS) and the Short-Term <span class="hlt">Earthquake</span> Probabilities (STEP). Here, we report the results from OEF's 24hour <span class="hlt">earthquake</span> forecasting during the main phases of the 2016-2017 sequence occurred in Central Apennines (Italy).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFMNH53B..04C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFMNH53B..04C"><span>The 2008 Wenchuan <span class="hlt">Earthquake</span> and the Rise and Fall of <span class="hlt">Earthquake</span> Prediction in China</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, Q.; Wang, K.</p> <p>2009-12-01</p> <p>Regardless of the future potential of <span class="hlt">earthquake</span> prediction, it is presently impractical to rely on it to mitigate <span class="hlt">earthquake</span> disasters. The practical approach is to strengthen the resilience of our built environment to <span class="hlt">earthquakes</span> based on hazard assessment. But this was not common understanding in China when the M 7.9 Wenchuan <span class="hlt">earthquake</span> struck the Sichuan Province on 12 May 2008, claiming over 80,000 lives. In China, <span class="hlt">earthquake</span> prediction is a government-sanctioned and law-regulated measure of disaster prevention. A sudden boom of the <span class="hlt">earthquake</span> prediction program in 1966-1976 coincided with a succession of nine M > 7 damaging <span class="hlt">earthquakes</span> in the densely populated region of the country and the political chaos of the Cultural Revolution. It climaxed with the prediction of the 1975 Haicheng <span class="hlt">earthquake</span>, which was due mainly to an unusually pronounced foreshock sequence and the extraordinary readiness of some local officials to issue imminent warning and evacuation order. The Haicheng prediction was a success in practice and yielded useful lessons, but the experience cannot be applied to most other <span class="hlt">earthquakes</span> and cultural environments. Since the disastrous Tangshan <span class="hlt">earthquake</span> in 1976 that killed over 240,000 people, there have been two opposite trends in China: decreasing confidence in prediction and increasing emphasis on regulating construction design for <span class="hlt">earthquake</span> resilience. In 1976, most of the seismic intensity XI areas of Tangshan were literally razed to the ground, but in 2008, many buildings in the intensity XI areas of Wenchuan did not collapse. Prediction did not save life in either of these events; the difference was made by construction standards. For regular buildings, there was no seismic design in Tangshan to resist any <span class="hlt">earthquake</span> shaking in 1976, but limited seismic design was required for the Wenchuan area in 2008. Although the construction standards were later recognized to be too low, those buildings that met the standards suffered much less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70036936','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70036936"><span><span class="hlt">Earthquake</span> impact scale</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Wald, D.J.; Jaiswal, K.S.; Marano, K.D.; Bausch, D.</p> <p>2011-01-01</p> <p>With the advent of the USGS prompt assessment of global <span class="hlt">earthquakes</span> for response (PAGER) system, which rapidly assesses <span class="hlt">earthquake</span> impacts, U.S. and international <span class="hlt">earthquake</span> responders are reconsidering their automatic alert and activation levels and response procedures. To help facilitate rapid and appropriate <span class="hlt">earthquake</span> response, an <span class="hlt">Earthquake</span> Impact Scale (EIS) is proposed on the basis of two complementary criteria. On the basis of the estimated cost of damage, one is most suitable for domestic events; the other, on the basis of estimated ranges of fatalities, is generally more appropriate for global events, particularly in developing countries. Simple thresholds, derived from the systematic analysis of past <span class="hlt">earthquake</span> impact and associated response levels, are quite effective in communicating predicted impact and response needed after an event through alerts of green (little or no impact), yellow (regional impact and response), orange (national-scale impact and response), and red (international response). Corresponding fatality thresholds for yellow, orange, and red alert levels are 1, 100, and 1,000, respectively. For damage impact, yellow, orange, and red thresholds are triggered by estimated losses reaching $1M, $100M, and $1B, respectively. The rationale for a dual approach to <span class="hlt">earthquake</span> alerting stems from the recognition that relatively high fatalities, injuries, and homelessness predominate in countries in which local building practices typically lend themselves to high collapse and casualty rates, and these impacts lend to prioritization for international response. In contrast, financial and overall societal impacts often trigger the level of response in regions or countries in which prevalent <span class="hlt">earthquake</span> resistant construction practices greatly reduce building collapse and resulting fatalities. Any newly devised alert, whether economic- or casualty-based, should be intuitive and consistent with established lexicons and procedures. Useful alerts should</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014GSL.....1...10S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014GSL.....1...10S"><span>A post-Tohoku <span class="hlt">earthquake</span> review of <span class="hlt">earthquake</span> probabilities in the Southern Kanto District, Japan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Somerville, Paul G.</p> <p>2014-12-01</p> <p>The 2011 Mw 9.0 Tohoku <span class="hlt">earthquake</span> generated an aftershock sequence that affected a large part of northern Honshu, and has given rise to widely divergent forecasts of changes in <span class="hlt">earthquake</span> occurrence probabilities in northern Honshu. The objective of this review is to assess these forecasts as they relate to potential changes in the occurrence probabilities of damaging <span class="hlt">earthquakes</span> in the Kanto Region. It is generally agreed that the 2011 Mw 9.0 Tohoku <span class="hlt">earthquake</span> increased the stress on faults in the southern Kanto district. Toda and Stein (Geophys Res Lett 686, 40: doi:10.1002, 2013) further conclude that the probability of <span class="hlt">earthquakes</span> in the Kanto Corridor has increased by a factor of 2.5 for the time period 11 March 2013 to 10 March 2018 in the Kanto Corridor. Estimates of <span class="hlt">earthquake</span> probabilities in a wider region of the Southern Kanto District by Nanjo et al. (Geophys J Int, doi:10.1093, 2013) indicate that any increase in the probability of <span class="hlt">earthquakes</span> is insignificant in this larger region. Uchida et al. (Earth Planet Sci Lett 374: 81-91, 2013) conclude that the Philippine Sea plate the extends well north of the northern margin of Tokyo Bay, inconsistent with the Kanto Fragment hypothesis of Toda et al. (Nat Geosci, 1:1-6,2008), which attributes deep <span class="hlt">earthquakes</span> in this region, which they term the Kanto Corridor, to a broken fragment of the Pacific plate. The results of Uchida and Matsuzawa (J Geophys Res 115:B07309, 2013)support the conclusion that fault creep in southern Kanto may be slowly relaxing the stress increase caused by the Tohoku <span class="hlt">earthquake</span> without causing more large <span class="hlt">earthquakes</span>. Stress transfer calculations indicate a large stress transfer to the Off Boso Segment as a result of the 2011 Tohoku <span class="hlt">earthquake</span>. However, Ozawa et al. (J Geophys Res 117:B07404, 2012) used onshore GPS measurements to infer large post-Tohoku creep on the plate interface in the Off-Boso region, and Uchida and Matsuzawa (ibid.) measured similar large creep off the Boso</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70161897','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70161897"><span>Post-<span class="hlt">earthquake</span> building safety inspection: Lessons from the Canterbury, New Zealand, <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Marshall, J.; Jaiswal, Kishor; Gould, N.; Turner, F.; Lizundia, B.; Barnes, J.</p> <p>2013-01-01</p> <p>The authors discuss some of the unique aspects and lessons of the New Zealand post-<span class="hlt">earthquake</span> building safety inspection program that was implemented following the Canterbury <span class="hlt">earthquake</span> sequence of 2010–2011. The post-event safety assessment program was one of the largest and longest programs undertaken in recent times anywhere in the world. The effort engaged hundreds of engineering professionals throughout the country, and also sought expertise from outside, to perform post-<span class="hlt">earthquake</span> structural safety inspections of more than 100,000 buildings in the city of Christchurch and the surrounding suburbs. While the building safety inspection procedure implemented was analogous to the ATC 20 program in the United States, many modifications were proposed and implemented in order to assess the large number of buildings that were subjected to strong and variable shaking during a period of two years. This note discusses some of the key aspects of the post-<span class="hlt">earthquake</span> building safety inspection program and summarizes important lessons that can improve future <span class="hlt">earthquake</span> response.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4510879','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4510879"><span>Do <span class="hlt">Earthquakes</span> Shake Stock Markets?</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2015-01-01</p> <p>This paper examines how major <span class="hlt">earthquakes</span> affected the returns and volatility of aggregate stock market indices in thirty-five financial markets over the last twenty years. Results show that global financial markets are resilient to shocks caused by <span class="hlt">earthquakes</span> even if these are domestic. Our analysis reveals that, in a few instances, some macroeconomic variables and <span class="hlt">earthquake</span> characteristics (gross domestic product per capita, trade openness, bilateral trade flows, <span class="hlt">earthquake</span> magnitude, a tsunami indicator, distance to the epicenter, and number of fatalities) mediate the impact of <span class="hlt">earthquakes</span> on stock market returns, resulting in a zero net effect. However, the influence of these variables is market-specific, indicating no systematic pattern across global capital markets. Results also demonstrate that stock market volatility is unaffected by <span class="hlt">earthquakes</span>, except for Japan. PMID:26197482</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/12178110','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/12178110"><span><span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p></p> <p>1985-05-01</p> <p>In this discussion of <span class="hlt">India</span> attention is directed to the following: the people; geography; history; government; political conditions; the economy; foreign relations (Pakistan and Bangladesh, China, and the Soviet Union); defense; and the relations between the US and <span class="hlt">India</span>. In 1983 <span class="hlt">India</span>'s population was estimated at 746 million with an annual growth rate of 2.24%. The infant mortality rate was estimated at 116/1000 in 1984 with a life expectancy of 54.9 years. Although <span class="hlt">India</span> occupies only 2.4% of the world's land area, it supports nearly 15% of the world's population. 2 major ethnic strains predominate in <span class="hlt">India</span>: the Aryan in the north and the Dravidian in the south, although the lines between them are blurred. <span class="hlt">India</span> dominates the South Asian subcontinent geographically. The people of <span class="hlt">India</span> have had a continuous civilization since about 2500 B.C., when the inhabitants of the Indus River Valley developed an urban culture based on commerce, trade, and, to a lesser degree, agriculture. This civilization declined about 1500 B.C. and Aryan tribes originating in central Asia absorbed parts of its culture as they spread out over the South Asian subcontinent. During the next few centuries, <span class="hlt">India</span> flourished under several successive empires. The 1st British outpost in South Asia was established in 1619 at Surat on the northwestern coast of <span class="hlt">India</span>. The British gradually expanded their influence until, by the 1850s, they controlled almost the entire area of present-day <span class="hlt">India</span>. Independence was attained on August 15, 1947, and <span class="hlt">India</span> became a dominion within the Commonwealth of Nations with Jawaharlal Nehru as prime minister. According to its constitution, <span class="hlt">India</span> is a "sovereign socialist secular democratic republic." Like the US, <span class="hlt">India</span> has a federal form of government, but the central government in <span class="hlt">India</span> has greater power in relation to its states, and government is patterned after the British parliamentary system. The Congress Party has ruled <span class="hlt">India</span> since independence with the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA539361','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA539361"><span>A Profile of Tehrik-i-Taliban Pakistan</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2008-01-01</p> <p>virgins of paradise. Even senior Muntada al-Ansar administrators contributed eulogies in honor of Rahman, such as the notorious Saif al-Islam al...large segments of the population. <span class="hlt">Gujarat</span> has contributed further to Muslim alienation within <span class="hlt">India</span>.17 One of India’s premier security...commemorate a national holiday in central Baghdad were targeted by a suicide bomber, leaving nine people dead. – Reuters, January 6 January 7</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.S34B..08H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.S34B..08H"><span>Continuing Megathrust <span class="hlt">Earthquake</span> Potential in northern Chile after the 2014 Iquique <span class="hlt">Earthquake</span> Sequence</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hayes, G. P.; Herman, M. W.; Barnhart, W. D.; Furlong, K. P.; Riquelme, S.; Benz, H.; Bergman, E.; Barrientos, S. E.; Earle, P. S.; Samsonov, S. V.</p> <p>2014-12-01</p> <p>The seismic gap theory, which identifies regions of elevated hazard based on a lack of recent seismicity in comparison to other portions of a fault, has successfully explained past <span class="hlt">earthquakes</span> and is useful for qualitatively describing where future large <span class="hlt">earthquakes</span> might occur. A large <span class="hlt">earthquake</span> had been expected in the subduction zone adjacent to northern Chile, which until recently had not ruptured in a megathrust <span class="hlt">earthquake</span> since a M~8.8 event in 1877. On April 1 2014, a M 8.2 <span class="hlt">earthquake</span> occurred within this northern Chile seismic gap, offshore of the city of Iquique; the size and spatial extent of the rupture indicate it was not the <span class="hlt">earthquake</span> that had been anticipated. Here, we present a rapid assessment of the seismotectonics of the March-April 2014 seismic sequence offshore northern Chile, including analyses of <span class="hlt">earthquake</span> (fore- and aftershock) relocations, moment tensors, finite fault models, moment deficit calculations, and cumulative Coulomb stress transfer calculations over the duration of the sequence. This ensemble of information allows us to place the current sequence within the context of historic seismicity in the region, and to assess areas of remaining and/or elevated hazard. Our results indicate that while accumulated strain has been released for a portion of the northern Chile seismic gap, significant sections have not ruptured in almost 150 years. These observations suggest that large-to-great sized megathrust <span class="hlt">earthquakes</span> will occur north and south of the 2014 Iquique sequence sooner than might be expected had the 2014 events ruptured the entire seismic gap.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018JSeis..22..217Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018JSeis..22..217Z"><span><span class="hlt">Earthquake</span> precursors: spatial-temporal gravity changes before the great <span class="hlt">earthquakes</span> in the Sichuan-Yunnan area</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zhu, Yi-Qing; Liang, Wei-Feng; Zhang, Song</p> <p>2018-01-01</p> <p>Using multiple-scale mobile gravity data in the Sichuan-Yunnan area, we systematically analyzed the relationships between spatial-temporal gravity changes and the 2014 Ludian, Yunnan Province Ms6.5 <span class="hlt">earthquake</span> and the 2014 Kangding Ms6.3, 2013 Lushan Ms7.0, and 2008 Wenchuan Ms8.0 <span class="hlt">earthquakes</span> in Sichuan Province. Our main results are as follows. (1) Before the occurrence of large <span class="hlt">earthquakes</span>, gravity anomalies occur in a large area around the epicenters. The directions of gravity change gradient belts usually agree roughly with the directions of the main fault zones of the study area. Such gravity changes might reflect the increase of crustal stress, as well as the significant active tectonic movements and surface deformations along fault zones, during the period of gestation of great <span class="hlt">earthquakes</span>. (2) Continuous significant changes of the multiple-scale gravity fields, as well as greater gravity changes with larger time scales, can be regarded as medium-range precursors of large <span class="hlt">earthquakes</span>. The subsequent large <span class="hlt">earthquakes</span> always occur in the area where the gravity changes greatly. (3) The spatial-temporal gravity changes are very useful in determining the epicenter of coming large <span class="hlt">earthquakes</span>. The large gravity networks are useful to determine the general areas of coming large <span class="hlt">earthquakes</span>. However, the local gravity networks with high spatial-temporal resolution are suitable for determining the location of epicenters. Therefore, denser gravity observation networks are necessary for better forecasts of the epicenters of large <span class="hlt">earthquakes</span>. (4) Using gravity changes from mobile observation data, we made medium-range forecasts of the Kangding, Ludian, Lushan, and Wenchuan <span class="hlt">earthquakes</span>, with especially successful forecasts of the location of their epicenters. Based on the above discussions, we emphasize that medium-/long-term potential for large <span class="hlt">earthquakes</span> might exist nowadays in some areas with significant gravity anomalies in the study region. Thus, the monitoring</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013AGUFM.T24C..05M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013AGUFM.T24C..05M"><span>Geomorphology, active duplexing, and <span class="hlt">earthquakes</span> within the Central Himalayan seismic gap</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Morell, K. D.; Sandiford, M.; Rajendran, C. C.; Rajendran, K.</p> <p>2013-12-01</p> <p>The ~500 km long 'Central Himalayan seismic gap' of northwest <span class="hlt">India</span>, is the largest section of the Himalaya that has not experienced a very large <span class="hlt">earthquake</span> (Mw > 7.0) in the past 200-500 years. The slip deficit associated with this seismic quiescence has led many to suggest that the region is overdue for a great <span class="hlt">earthquake</span> (Mw >8), an event which could be potentially devastating given the region's high population (>10 million). Despite the recognition that the region is under considerable seismic risk, the geometry of active fault structures that could potentially fail during large <span class="hlt">earthquakes</span> remains poorly defined. This has arisen, to a certain extent, because moderate <span class="hlt">earthquakes</span>, such as the Mw 6.3 1999 event near the city of Chamoli and the Mw 7.0 1991 <span class="hlt">earthquake</span> near Uttarkashi (responsible for ~1000 deaths), have not produced obvious surface ruptures and do not appear to coincide with surficially mapped faults. We present new geomorphic and river longitudinal profile data that define a prominent ~400 km long distinctive geomorphic transition at the base of the high Himalaya in the seismic gap, defined as a sharp dividing line north of which there are significant increases in normalized river steepness (ksn), hillslope angles, and local relief. We interpret the morphologic changes across the geomorphic boundary to be produced due to a northward increase in rock uplift rate, given that the boundary cross-cuts mapped structures and lithologic contacts, yet coincides exactly with: 1) the axial trace of the geophysically-imaged ramp-flat transition in the Main Himalayan Thrust, 2) significant northward increases in instrumentally-recorded seismicity, and 3) an order of magnitude change in published Ar-Ar bedrock cooling ages. The available datasets suggest that such an increase in rock uplift rate is best explained by a ~400 km long by ~50 km wide active duplex along the Main Himalayan Thrust ramp, with the leading edge of the duplex giving rise to the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/of/2011/1117/','USGSPUBS'); return false;" href="https://pubs.usgs.gov/of/2011/1117/"><span><span class="hlt">Earthquakes</span> in Mississippi and vicinity 1811-2010</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Dart, Richard L.; Bograd, Michael B.E.</p> <p>2011-01-01</p> <p>This map summarizes two centuries of <span class="hlt">earthquake</span> activity in Mississippi. Work on the Mississippi map was done in collaboration with the Mississippi Department of Environmental Quality, Office of Geology. The <span class="hlt">earthquake</span> data plotted on the map are from several sources: the Mississippi Department of Environmental Quality, the Center for <span class="hlt">Earthquake</span> Research and Information, the National Center for <span class="hlt">Earthquake</span> Engineering Research, and the Arkansas Geological Survey. In addition to <span class="hlt">earthquake</span> locations, other materials include seismic hazard and isoseismal maps and related text. <span class="hlt">Earthquakes</span> are a legitimate concern in Mississippi and parts of adjacent States. Mississippi has undergone a number of felt <span class="hlt">earthquakes</span> since 1811. At least two of these events caused property damage: a magnitude 4.7 <span class="hlt">earthquake</span> in 1931, and a magnitude 4.3 <span class="hlt">earthquake</span> in 1967. The map shows all historical and instrumentally located <span class="hlt">earthquakes</span> in Mississippi and vicinity between 1811 and 2010. The largest historic <span class="hlt">earthquake</span> in the vicinity of the State was an intensity XI event, on December 16, 1811; the first <span class="hlt">earthquake</span> in the New Madrid sequence. This violent event and the <span class="hlt">earthquakes</span> that followed caused considerable damage to the then sparsely settled region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017GSL.....4...19A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017GSL.....4...19A"><span>Overestimation of the <span class="hlt">earthquake</span> hazard along the Himalaya: constraints in bracketing of medieval <span class="hlt">earthquakes</span> from paleoseismic studies</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Arora, Shreya; Malik, Javed N.</p> <p>2017-12-01</p> <p>The Himalaya is one of the most seismically active regions of the world. The occurrence of several large magnitude <span class="hlt">earthquakes</span> viz. 1905 Kangra <span class="hlt">earthquake</span> (Mw 7.8), 1934 Bihar-Nepal <span class="hlt">earthquake</span> (Mw 8.2), 1950 Assam <span class="hlt">earthquake</span> (Mw 8.4), 2005 Kashmir (Mw 7.6), and 2015 Gorkha (Mw 7.8) are the testimony to ongoing tectonic activity. In the last few decades, tremendous efforts have been made along the Himalayan arc to understand the patterns of <span class="hlt">earthquake</span> occurrences, size, extent, and return periods. Some of the large magnitude <span class="hlt">earthquakes</span> produced surface rupture, while some remained blind. Furthermore, due to the incompleteness of the <span class="hlt">earthquake</span> catalogue, a very few events can be correlated with medieval <span class="hlt">earthquakes</span>. Based on the existing paleoseismic data certainly, there exists a complexity to precisely determine the extent of surface rupture of these <span class="hlt">earthquakes</span> and also for those events, which occurred during historic times. In this paper, we have compiled the paleo-seismological data and recalibrated the radiocarbon ages from the trenches excavated by previous workers along the entire Himalaya and compared <span class="hlt">earthquake</span> scenario with the past. Our studies suggest that there were multiple <span class="hlt">earthquake</span> events with overlapping surface ruptures in small patches with an average rupture length of 300 km limiting Mw 7.8-8.0 for the Himalayan arc, rather than two or three giant <span class="hlt">earthquakes</span> rupturing the whole front. It has been identified that the large magnitude Himalayan <span class="hlt">earthquakes</span>, such as 1905 Kangra, 1934 Bihar-Nepal, and 1950 Assam, that have occurred within a time frame of 45 years. Now, if these events are dated, there is a high possibility that within the range of ±50 years, they may be considered as the remnant of one giant <span class="hlt">earthquake</span> rupturing the entire Himalayan arc. Therefore, leading to an overestimation of seismic hazard scenario in Himalaya.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010AGUFMED41B0637D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010AGUFMED41B0637D"><span>Simulating <span class="hlt">Earthquake</span> Early Warning Systems in the Classroom as a New Approach to Teaching <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>D'Alessio, M. A.</p> <p>2010-12-01</p> <p>A discussion of P- and S-waves seems an ubiquitous part of studying <span class="hlt">earthquakes</span> in the classroom. Textbooks from middle school through university level typically define the differences between the waves and illustrate the sense of motion. While many students successfully memorize the differences between wave types (often utilizing the first letter as a memory aide), textbooks rarely give tangible examples of how the two waves would "feel" to a person sitting on the ground. One reason for introducing the wave types is to explain how to calculate <span class="hlt">earthquake</span> epicenters using seismograms and travel time charts -- very abstract representations of <span class="hlt">earthquakes</span>. Even when the skill is mastered using paper-and-pencil activities or one of the excellent online interactive versions, locating an epicenter simply does not excite many of our students because it evokes little emotional impact, even in students located in <span class="hlt">earthquake</span>-prone areas. Despite these limitations, huge numbers of students are mandated to complete the task. At the K-12 level, California requires that all students be able to locate <span class="hlt">earthquake</span> epicenters in Grade 6; in New York, the skill is a required part of the Regent's Examination. Recent innovations in <span class="hlt">earthquake</span> early warning systems around the globe give us the opportunity to address the same content standard, but with substantially more emotional impact on students. I outline a lesson about <span class="hlt">earthquakes</span> focused on <span class="hlt">earthquake</span> early warning systems. The introductory activities include video clips of actual <span class="hlt">earthquakes</span> and emphasize the differences between the way P- and S-waves feel when they arrive (P arrives first, but is weaker). I include an introduction to the principle behind <span class="hlt">earthquake</span> early warning (including a summary of possible uses of a few seconds warning about strong shaking) and show examples from Japan. Students go outdoors to simulate P-waves, S-waves, and occupants of two different cities who are talking to one another on cell phones</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.nicee.org/wcee/','USGSPUBS'); return false;" href="http://www.nicee.org/wcee/"><span>Demand surge following <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Olsen, Anna H.</p> <p>2012-01-01</p> <p>Demand surge is understood to be a socio-economic phenomenon where repair costs for the same damage are higher after large- versus small-scale natural disasters. It has reportedly increased monetary losses by 20 to 50%. In previous work, a model for the increased costs of reconstruction labor and materials was developed for hurricanes in the Southeast United States. The model showed that labor cost increases, rather than the material component, drove the total repair cost increases, and this finding could be extended to <span class="hlt">earthquakes</span>. A study of past large-scale disasters suggested that there may be additional explanations for demand surge. Two such explanations specific to <span class="hlt">earthquakes</span> are the exclusion of insurance coverage for <span class="hlt">earthquake</span> damage and possible concurrent causation of damage from an <span class="hlt">earthquake</span> followed by fire or tsunami. Additional research into these aspects might provide a better explanation for increased monetary losses after large- vs. small-scale <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70168524','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70168524"><span>Intermediate-term <span class="hlt">earthquake</span> prediction</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Knopoff, L.</p> <p>1990-01-01</p> <p>The problems in predicting <span class="hlt">earthquakes</span> have been attacked by phenomenological methods from pre-historic times to the present. The associations of presumed precursors with large <span class="hlt">earthquakes</span> often have been remarked upon. the difficulty in identifying whether such correlations are due to some chance coincidence or are real precursors is that usually one notes the associations only in the relatively short time intervals before the large events. Only rarely, if ever, is notice taken of whether the presumed precursor is to be found in the rather long intervals that follow large <span class="hlt">earthquakes</span>, or in fact is absent in these post-<span class="hlt">earthquake</span> intervals. If there are enough examples, the presumed correlation fails as a precursor in the former case, while in the latter case the precursor would be verified. Unfortunately, the observer is usually not concerned with the 'uniteresting' intervals that have no large <span class="hlt">earthquakes</span>. </p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMED41A0763A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMED41A0763A"><span><span class="hlt">Earthquakes</span> on Your Dinner Table</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alexeev, N. A.; Tape, C.; Alexeev, V. A.</p> <p>2016-12-01</p> <p><span class="hlt">Earthquakes</span> have interesting physics applicable to other phenomena like propagation of waves, also, they affect human lives. This study focused on three questions, how: depth, distance from epicenter and ground hardness affect <span class="hlt">earthquake</span> strength. Experimental setup consisted of a gelatin slab to simulate crust. The slab was hit with a weight and <span class="hlt">earthquake</span> amplitude was measured. It was found that <span class="hlt">earthquake</span> amplitude was larger when the epicenter was deeper, which contradicts observations and probably was an artifact of the design. <span class="hlt">Earthquake</span> strength was inversely proportional to the distance from the epicenter, which generally follows reality. Soft and medium jello were implanted into hard jello. It was found that <span class="hlt">earthquakes</span> are stronger in softer jello, which was a result of resonant amplification in soft ground. Similar results are found in Minto Flats, where <span class="hlt">earthquakes</span> are stronger and last longer than in the nearby hills. <span class="hlt">Earthquakes</span> waveforms from Minto Flats showed that that the oscillations there have longer periods compared to the nearby hills with harder soil. Two gelatin pieces with identical shapes and different hardness were vibrated on a platform at varying frequencies in order to demonstrate that their resonant frequencies are statistically different. This phenomenon also occurs in Yukon Flats.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70017701','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70017701"><span>Damaging <span class="hlt">earthquakes</span>: A scientific laboratory</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hays, Walter W.; ,</p> <p>1996-01-01</p> <p>This paper reviews the principal lessons learned from multidisciplinary postearthquake investigations of damaging <span class="hlt">earthquakes</span> throughout the world during the past 15 years. The unique laboratory provided by a damaging <span class="hlt">earthquake</span> in culturally different but tectonically similar regions of the world has increased fundamental understanding of <span class="hlt">earthquake</span> processes, added perishable scientific, technical, and socioeconomic data to the knowledge base, and led to changes in public policies and professional practices for <span class="hlt">earthquake</span> loss reduction.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_24 --> <div id="page_25" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="481"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..1215701B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..1215701B"><span>2010 Chile <span class="hlt">Earthquake</span> Aftershock Response</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Barientos, Sergio</p> <p>2010-05-01</p> <p>The Mw=8.8 <span class="hlt">earthquake</span> off the coast of Chile on 27 February 2010 is the 5th largest megathrust <span class="hlt">earthquake</span> ever to be recorded and provides an unprecedented opportunity to advance our understanding of megathrust <span class="hlt">earthquakes</span> and associated phenomena. The 2010 Chile <span class="hlt">earthquake</span> ruptured the Concepcion-Constitucion segment of the Nazca/South America plate boundary, south of the Central Chile region and triggered a tsunami along the coast. Following the 2010 <span class="hlt">earthquake</span>, a very energetic aftershock sequence is being observed in an area that is 600 km along strike from Valparaiso to 150 km south of Concepcion. Within the first three weeks there were over 260 aftershocks with magnitude 5.0 or greater and 18 with magnitude 6.0 or greater (NEIC, USGS). The Concepcion-Constitucion segment lies immediately north of the rupture zone associated with the great magnitude 9.5 Chile <span class="hlt">earthquake</span>, and south of the 1906 and the 1985 Valparaiso <span class="hlt">earthquakes</span>. The last great subduction <span class="hlt">earthquake</span> in the region dates back to the February 1835 event described by Darwin (1871). Since 1835, part of the region was affected in the north by the Talca <span class="hlt">earthquake</span> in December 1928, interpreted as a shallow dipping thrust event, and by the Chillan <span class="hlt">earthquake</span> (Mw 7.9, January 1939), a slab-pull intermediate depth <span class="hlt">earthquake</span>. For the last 30 years, geodetic studies in this area were consistent with a fully coupled elastic loading of the subduction interface at depth; this led to identify the area as a mature seismic gap with potential for an <span class="hlt">earthquake</span> of magnitude of the order 8.5 or several <span class="hlt">earthquakes</span> of lesser magnitude. What was less expected was the partial rupturing of the 1985 segment toward north. Today, the 2010 <span class="hlt">earthquake</span> raises some disturbing questions: Why and how the rupture terminated where it did at the northern end? How did the 2010 <span class="hlt">earthquake</span> load the adjacent segment to the north and did the 1985 <span class="hlt">earthquake</span> only partially ruptured the plate interface leaving loaded asperities since</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1915410B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1915410B"><span>Sensing the <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bichisao, Marta; Stallone, Angela</p> <p>2017-04-01</p> <p>Making science visual plays a crucial role in the process of building knowledge. In this view, art can considerably facilitate the representation of the scientific content, by offering a different perspective on how a specific problem could be approached. Here we explore the possibility of presenting the <span class="hlt">earthquake</span> process through visual dance. From a choreographer's point of view, the focus is always on the dynamic relationships between moving objects. The observed spatial patterns (coincidences, repetitions, double and rhythmic configurations) suggest how objects organize themselves in the environment and what are the principles underlying that organization. The identified set of rules is then implemented as a basis for the creation of a complex rhythmic and visual dance system. Recently, scientists have turned seismic waves into sound and animations, introducing the possibility of "feeling" the <span class="hlt">earthquakes</span>. We try to implement these results into a choreographic model with the aim to convert <span class="hlt">earthquake</span> sound to a visual dance system, which could return a transmedia representation of the <span class="hlt">earthquake</span> process. In particular, we focus on a possible method to translate and transfer the metric language of seismic sound and animations into body language. The objective is to involve the audience into a multisensory exploration of the <span class="hlt">earthquake</span> phenomenon, through the stimulation of the hearing, eyesight and perception of the movements (neuromotor system). In essence, the main goal of this work is to develop a method for a simultaneous visual and auditory representation of a seismic event by means of a structured choreographic model. This artistic representation could provide an original entryway into the physics of <span class="hlt">earthquakes</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70022248','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70022248"><span>Discrepancy between <span class="hlt">earthquake</span> rates implied by historic <span class="hlt">earthquakes</span> and a consensus geologic source model for California</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Petersen, M.D.; Cramer, C.H.; Reichle, M.S.; Frankel, A.D.; Hanks, T.C.</p> <p>2000-01-01</p> <p>We examine the difference between expected <span class="hlt">earthquake</span> rates inferred from the historical <span class="hlt">earthquake</span> catalog and the geologic data that was used to develop the consensus seismic source characterization for the state of California [California Department of Conservation, Division of Mines and Geology (CDMG) and U.S. Geological Survey (USGS) Petersen et al., 1996; Frankel et al., 1996]. On average the historic <span class="hlt">earthquake</span> catalog and the seismic source model both indicate about one M 6 or greater <span class="hlt">earthquake</span> per year in the state of California. However, the overall <span class="hlt">earthquake</span> rates of <span class="hlt">earthquakes</span> with magnitudes (M) between 6 and 7 in this seismic source model are higher, by at least a factor of 2, than the mean historic <span class="hlt">earthquake</span> rates for both southern and northern California. The <span class="hlt">earthquake</span> rate discrepancy results from a seismic source model that includes <span class="hlt">earthquakes</span> with characteristic (maximum) magnitudes that are primarily between M 6.4 and 7.1. Many of these faults are interpreted to accommodate high strain rates from geologic and geodetic data but have not ruptured in large <span class="hlt">earthquakes</span> during historic time. Our sensitivity study indicates that the rate differences between magnitudes 6 and 7 can be reduced by adjusting the magnitude-frequency distribution of the source model to reflect more characteristic behavior, by decreasing the moment rate available for seismogenic slip along faults, by increasing the maximum magnitude of the <span class="hlt">earthquake</span> on a fault, or by decreasing the maximum magnitude of the background seismicity. However, no single parameter can be adjusted, consistent with scientific consensus, to eliminate the <span class="hlt">earthquake</span> rate discrepancy. Applying a combination of these parametric adjustments yields an alternative <span class="hlt">earthquake</span> source model that is more compatible with the historic data. The 475-year return period hazard for peak ground and 1-sec spectral acceleration resulting from this alternative source model differs from the hazard resulting from the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMNH21C1846P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMNH21C1846P"><span>GPS Technologies as a Tool to Detect the Pre-<span class="hlt">Earthquake</span> Signals Associated with Strong <span class="hlt">Earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pulinets, S. A.; Krankowski, A.; Hernandez-Pajares, M.; Liu, J. Y. G.; Hattori, K.; Davidenko, D.; Ouzounov, D.</p> <p>2015-12-01</p> <p>The existence of ionospheric anomalies before <span class="hlt">earthquakes</span> is now widely accepted. These phenomena started to be considered by GPS community to mitigate the GPS signal degradation over the territories of the <span class="hlt">earthquake</span> preparation. The question is still open if they could be useful for seismology and for short-term <span class="hlt">earthquake</span> forecast. More than decade of intensive studies proved that ionospheric anomalies registered before <span class="hlt">earthquakes</span> are initiated by processes in the boundary layer of atmosphere over <span class="hlt">earthquake</span> preparation zone and are induced in the ionosphere by electromagnetic coupling through the Global Electric Circuit. Multiparameter approach based on the Lithosphere-Atmosphere-Ionosphere Coupling model demonstrated that <span class="hlt">earthquake</span> forecast is possible only if we consider the final stage of <span class="hlt">earthquake</span> preparation in the multidimensional space where every dimension is one from many precursors in ensemble, and they are synergistically connected. We demonstrate approaches developed in different countries (Russia, Taiwan, Japan, Spain, and Poland) within the framework of the ISSI and ESA projects) to identify the ionospheric precursors. They are also useful to determine the all three parameters necessary for the <span class="hlt">earthquake</span> forecast: impending <span class="hlt">earthquake</span> epicenter position, expectation time and magnitude. These parameters are calculated using different technologies of GPS signal processing: time series, correlation, spectral analysis, ionospheric tomography, wave propagation, etc. Obtained results from different teams demonstrate the high level of statistical significance and physical justification what gives us reason to suggest these methodologies for practical validation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.S53A2794B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.S53A2794B"><span><span class="hlt">Earthquake</span> Fingerprints: Representing <span class="hlt">Earthquake</span> Waveforms for Similarity-Based Detection</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bergen, K.; Beroza, G. C.</p> <p>2016-12-01</p> <p>New <span class="hlt">earthquake</span> detection methods, such as Fingerprint and Similarity Thresholding (FAST), use fast approximate similarity search to identify similar waveforms in long-duration data without templates (Yoon et al. 2015). These methods have two key components: fingerprint extraction and an efficient search algorithm. Fingerprint extraction converts waveforms into fingerprints, compact signatures that represent short-duration waveforms for identification and search. <span class="hlt">Earthquakes</span> are detected using an efficient indexing and search scheme, such as locality-sensitive hashing, that identifies similar waveforms in a fingerprint database. The quality of the search results, and thus the <span class="hlt">earthquake</span> detection results, is strongly dependent on the fingerprinting scheme. Fingerprint extraction should map similar <span class="hlt">earthquake</span> waveforms to similar waveform fingerprints to ensure a high detection rate, even under additive noise and small distortions. Additionally, fingerprints corresponding to noise intervals should have mutually dissimilar fingerprints to minimize false detections. In this work, we compare the performance of multiple fingerprint extraction approaches for the <span class="hlt">earthquake</span> waveform similarity search problem. We apply existing audio fingerprinting (used in content-based audio identification systems) and time series indexing techniques and present modified versions that are specifically adapted for seismic data. We also explore data-driven fingerprinting approaches that can take advantage of labeled or unlabeled waveform data. For each fingerprinting approach we measure its ability to identify similar waveforms in a low signal-to-noise setting, and quantify the trade-off between true and false detection rates in the presence of persistent noise sources. We compare the performance using known event waveforms from eight independent stations in the Northern California Seismic Network.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3220027','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3220027"><span><span class="hlt">Earthquake</span>-related versus non-<span class="hlt">earthquake</span>-related injuries in spinal injury patients: differentiation with multidetector computed tomography</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p></p> <p>2010-01-01</p> <p>Introduction In recent years, several massive <span class="hlt">earthquakes</span> have occurred across the globe. Multidetector computed tomography (MDCT) is reliable in detecting spinal injuries. The purpose of this study was to compare the features of spinal injuries resulting from the Sichuan <span class="hlt">earthquake</span> with those of non-<span class="hlt">earthquake</span>-related spinal trauma using MDCT. Methods Features of spinal injuries of 223 Sichuan <span class="hlt">earthquake</span>-exposed patients and 223 non-<span class="hlt">earthquake</span>-related spinal injury patients were retrospectively compared using MDCT. The date of non-<span class="hlt">earthquake</span>-related spinal injury patients was collected from 1 May 2009 to 22 July 2009 to avoid the confounding effects of seasonal activity and clothing. We focused on anatomic sites, injury types and neurologic deficits related to spinal injuries. Major injuries were classified according to the grid 3-3-3 scheme of the Magerl (AO) classification system. Results A total of 185 patients (82.96%) in the <span class="hlt">earthquake</span>-exposed cohort experienced crush injuries. In the <span class="hlt">earthquake</span> and control groups, 65 and 92 patients, respectively, had neurologic deficits. The anatomic distribution of these two cohorts was significantly different (P < 0.001). Cervical spinal injuries were more common in the control group (risk ratio (RR) = 2.12, P < 0.001), whereas lumbar spinal injuries were more common in the <span class="hlt">earthquake</span>-related spinal injuries group (277 of 501 injured vertebrae; 55.29%). The major types of injuries were significantly different between these cohorts (P = 0.002). Magerl AO type A lesions composed most of the lesions seen in both of these cohorts. Type B lesions were more frequently seen in <span class="hlt">earthquake</span>-related spinal injuries (RR = 1.27), while we observed type C lesions more frequently in subjects with non-<span class="hlt">earthquake</span>-related spinal injuries (RR = 1.98, P = 0.0029). Conclusions Spinal injuries sustained in the Sichuan <span class="hlt">earthquake</span> were located mainly in the lumbar spine, with a peak prevalence of type A lesions and a high occurrence of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/EJ1164614.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/EJ1164614.pdf"><span><span class="hlt">Earthquake</span> Emergency Education in Dushanbe, Tajikistan</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Mohadjer, Solmaz; Bendick, Rebecca; Halvorson, Sarah J.; Saydullaev, Umed; Hojiboev, Orifjon; Stickler, Christine; Adam, Zachary R.</p> <p>2010-01-01</p> <p>We developed a middle school <span class="hlt">earthquake</span> science and hazards curriculum to promote <span class="hlt">earthquake</span> awareness to students in the Central Asian country of Tajikistan. These materials include pre- and post-assessment activities, six science activities describing physical processes related to <span class="hlt">earthquakes</span>, five activities on <span class="hlt">earthquake</span> hazards and mitigation…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.5891A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.5891A"><span>Intensity <span class="hlt">earthquake</span> scenario (scenario event - a damaging <span class="hlt">earthquake</span> with higher probability of occurrence) for the city of Sofia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Aleksandrova, Irena; Simeonova, Stela; Solakov, Dimcho; Popova, Maria</p> <p>2014-05-01</p> <p>Among the many kinds of natural and man-made disasters, <span class="hlt">earthquakes</span> dominate with regard to their social and economical impact on the urban environment. Global seismic risk to <span class="hlt">earthquakes</span> are increasing steadily as urbanization and development occupy more areas that a prone to effects of strong <span class="hlt">earthquakes</span>. Additionally, the uncontrolled growth of mega cities in highly seismic areas around the world is often associated with the construction of seismically unsafe buildings and infrastructures, and undertaken with an insufficient knowledge of the regional seismicity peculiarities and seismic hazard. The assessment of seismic hazard and generation of <span class="hlt">earthquake</span> scenarios is the first link in the prevention chain and the first step in the evaluation of the seismic risk. The <span class="hlt">earthquake</span> scenarios are intended as a basic input for developing detailed <span class="hlt">earthquake</span> damage scenarios for the cities and can be used in <span class="hlt">earthquake</span>-safe town and infrastructure planning. The city of Sofia is the capital of Bulgaria. It is situated in the centre of the Sofia area that is the most populated (the population is of more than 1.2 mil. inhabitants), industrial and cultural region of Bulgaria that faces considerable <span class="hlt">earthquake</span> risk. The available historical documents prove the occurrence of destructive <span class="hlt">earthquakes</span> during the 15th-18th centuries in the Sofia zone. In 19th century the city of Sofia has experienced two strong <span class="hlt">earthquakes</span>: the 1818 <span class="hlt">earthquake</span> with epicentral intensity I0=8-9 MSK and the 1858 <span class="hlt">earthquake</span> with I0=9-10 MSK. During the 20th century the strongest event occurred in the vicinity of the city of Sofia is the 1917 <span class="hlt">earthquake</span> with MS=5.3 (I0=7-8 MSK). Almost a century later (95 years) an <span class="hlt">earthquake</span> of moment magnitude 5.6 (I0=7-8 MSK) hit the city of Sofia, on May 22nd, 2012. In the present study as a deterministic scenario event is considered a damaging <span class="hlt">earthquake</span> with higher probability of occurrence that could affect the city with intensity less than or equal to VIII</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70046871','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70046871"><span><span class="hlt">Earthquake</span> recurrence models fail when <span class="hlt">earthquakes</span> fail to reset the stress field</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Tormann, Thessa; Wiemer, Stefan; Hardebeck, Jeanne L.</p> <p>2012-01-01</p> <p>Parkfield's regularly occurring M6 mainshocks, about every 25 years, have over two decades stoked seismologists' hopes to successfully predict an <span class="hlt">earthquake</span> of significant size. However, with the longest known inter-event time of 38 years, the latest M6 in the series (28 Sep 2004) did not conform to any of the applied forecast models, questioning once more the predictability of <span class="hlt">earthquakes</span> in general. Our study investigates the spatial pattern of b-values along the Parkfield segment through the seismic cycle and documents a stably stressed structure. The forecasted rate of M6 <span class="hlt">earthquakes</span> based on Parkfield's microseismicity b-values corresponds well to observed rates. We interpret the observed b-value stability in terms of the evolution of the stress field in that area: the M6 Parkfield <span class="hlt">earthquakes</span> do not fully unload the stress on the fault, explaining why time recurrent models fail. We present the 1989 M6.9 Loma Prieta <span class="hlt">earthquake</span> as counter example, which did release a significant portion of the stress along its fault segment and yields a substantial change in b-values.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMNG13A1860S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMNG13A1860S"><span>The Virtual Quake <span class="hlt">Earthquake</span> Simulator: <span class="hlt">Earthquake</span> Probability Statistics for the El Mayor-Cucapah Region and Evidence of Predictability in Simulated <span class="hlt">Earthquake</span> Sequences</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schultz, K.; Yoder, M. R.; Heien, E. M.; Rundle, J. B.; Turcotte, D. L.; Parker, J. W.; Donnellan, A.</p> <p>2015-12-01</p> <p>We introduce a framework for developing <span class="hlt">earthquake</span> forecasts using Virtual Quake (VQ), the generalized successor to the perhaps better known Virtual California (VC) <span class="hlt">earthquake</span> simulator. We discuss the basic merits and mechanics of the simulator, and we present several statistics of interest for <span class="hlt">earthquake</span> forecasting. We also show that, though the system as a whole (in aggregate) behaves quite randomly, (simulated) <span class="hlt">earthquake</span> sequences limited to specific fault sections exhibit measurable predictability in the form of increasing seismicity precursory to large m > 7 <span class="hlt">earthquakes</span>. In order to quantify this, we develop an alert based forecasting metric similar to those presented in Keilis-Borok (2002); Molchan (1997), and show that it exhibits significant information gain compared to random forecasts. We also discuss the long standing question of activation vs quiescent type <span class="hlt">earthquake</span> triggering. We show that VQ exhibits both behaviors separately for independent fault sections; some fault sections exhibit activation type triggering, while others are better characterized by quiescent type triggering. We discuss these aspects of VQ specifically with respect to faults in the Salton Basin and near the El Mayor-Cucapah region in southern California USA and northern Baja California Norte, Mexico.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=20130000020&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dearthquakes','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=20130000020&hterms=earthquakes&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D10%26Ntt%3Dearthquakes"><span><span class="hlt">Earthquake</span> Damage Assessment Using Objective Image Segmentation: A Case Study of 2010 Haiti <span class="hlt">Earthquake</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Oommen, Thomas; Rebbapragada, Umaa; Cerminaro, Daniel</p> <p>2012-01-01</p> <p>In this study, we perform a case study on imagery from the Haiti <span class="hlt">earthquake</span> that evaluates a novel object-based approach for characterizing <span class="hlt">earthquake</span> induced surface effects of liquefaction against a traditional pixel based change technique. Our technique, which combines object-oriented change detection with discriminant/categorical functions, shows the power of distinguishing <span class="hlt">earthquake</span>-induced surface effects from changes in buildings using the object properties concavity, convexity, orthogonality and rectangularity. Our results suggest that object-based analysis holds promise in automatically extracting <span class="hlt">earthquake</span>-induced damages from high-resolution aerial/satellite imagery.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28077808','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28077808"><span>Rupture, waves and <span class="hlt">earthquakes</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Uenishi, Koji</p> <p>2017-01-01</p> <p>Normally, an <span class="hlt">earthquake</span> is considered as a phenomenon of wave energy radiation by rupture (fracture) of solid Earth. However, the physics of dynamic process around seismic sources, which may play a crucial role in the occurrence of <span class="hlt">earthquakes</span> and generation of strong waves, has not been fully understood yet. Instead, much of former investigation in seismology evaluated <span class="hlt">earthquake</span> characteristics in terms of kinematics that does not directly treat such dynamic aspects and usually excludes the influence of high-frequency wave components over 1 Hz. There are countless valuable research outcomes obtained through this kinematics-based approach, but "extraordinary" phenomena that are difficult to be explained by this conventional description have been found, for instance, on the occasion of the 1995 Hyogo-ken Nanbu, Japan, <span class="hlt">earthquake</span>, and more detailed study on rupture and wave dynamics, namely, possible mechanical characteristics of (1) rupture development around seismic sources, (2) <span class="hlt">earthquake</span>-induced structural failures and (3) wave interaction that connects rupture (1) and failures (2), would be indispensable.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5406623','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5406623"><span>Rupture, waves and <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>UENISHI, Koji</p> <p>2017-01-01</p> <p>Normally, an <span class="hlt">earthquake</span> is considered as a phenomenon of wave energy radiation by rupture (fracture) of solid Earth. However, the physics of dynamic process around seismic sources, which may play a crucial role in the occurrence of <span class="hlt">earthquakes</span> and generation of strong waves, has not been fully understood yet. Instead, much of former investigation in seismology evaluated <span class="hlt">earthquake</span> characteristics in terms of kinematics that does not directly treat such dynamic aspects and usually excludes the influence of high-frequency wave components over 1 Hz. There are countless valuable research outcomes obtained through this kinematics-based approach, but “extraordinary” phenomena that are difficult to be explained by this conventional description have been found, for instance, on the occasion of the 1995 Hyogo-ken Nanbu, Japan, <span class="hlt">earthquake</span>, and more detailed study on rupture and wave dynamics, namely, possible mechanical characteristics of (1) rupture development around seismic sources, (2) <span class="hlt">earthquake</span>-induced structural failures and (3) wave interaction that connects rupture (1) and failures (2), would be indispensable. PMID:28077808</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2011NHESS..11.2235D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2011NHESS..11.2235D"><span>The CATDAT damaging <span class="hlt">earthquakes</span> database</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Daniell, J. E.; Khazai, B.; Wenzel, F.; Vervaeck, A.</p> <p>2011-08-01</p> <p>The global CATDAT damaging <span class="hlt">earthquakes</span> and secondary effects (tsunami, fire, landslides, liquefaction and fault rupture) database was developed to validate, remove discrepancies, and expand greatly upon existing global databases; and to better understand the trends in vulnerability, exposure, and possible future impacts of such historic <span class="hlt">earthquakes</span>. Lack of consistency and errors in other <span class="hlt">earthquake</span> loss databases frequently cited and used in analyses was a major shortcoming in the view of the authors which needed to be improved upon. Over 17 000 sources of information have been utilised, primarily in the last few years, to present data from over 12 200 damaging <span class="hlt">earthquakes</span> historically, with over 7000 <span class="hlt">earthquakes</span> since 1900 examined and validated before insertion into the database. Each validated <span class="hlt">earthquake</span> includes seismological information, building damage, ranges of social losses to account for varying sources (deaths, injuries, homeless, and affected), and economic losses (direct, indirect, aid, and insured). Globally, a slightly increasing trend in economic damage due to <span class="hlt">earthquakes</span> is not consistent with the greatly increasing exposure. The 1923 Great Kanto (214 billion USD damage; 2011 HNDECI-adjusted dollars) compared to the 2011 Tohoku (>300 billion USD at time of writing), 2008 Sichuan and 1995 Kobe <span class="hlt">earthquakes</span> show the increasing concern for economic loss in urban areas as the trend should be expected to increase. Many economic and social loss values not reported in existing databases have been collected. Historical GDP (Gross Domestic Product), exchange rate, wage information, population, HDI (Human Development Index), and insurance information have been collected globally to form comparisons. This catalogue is the largest known cross-checked global historic damaging <span class="hlt">earthquake</span> database and should have far-reaching consequences for <span class="hlt">earthquake</span> loss estimation, socio-economic analysis, and the global reinsurance field.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1985Tectp.118..257G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1985Tectp.118..257G"><span>The present status of reservoir induced seismicity investigations with special emphasis on Koyna <span class="hlt">earthquakes</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gupta, Harsh K.</p> <p>1985-10-01</p> <p>The status of Reservoir Induced Seismicity (RIS) has been reviewed periodically (Rothé, 1968, 1973; Gupta and Rastogi, 1976; Simpson, 1976; Packer et al., 1979). In the present paper, the significant work carried out during the last three years on RIS is reviewed. An <span class="hlt">earthquake</span> of magnitude 5 {1}/{2} occurred on November 14, 1981 in the vicinity of Aswan Lake, Egypt, 17 years after the filling started in 1964. This event occurred 4 days after the seasonal maximum in the reservoir water level and was followed by a long sequence of aftershocks. Another event of magnitude 4 {1}/{2} occurred in the vicinity of Aswan Lake on August 20, 1982. Results of preliminary investigations indicate that this seismic activity is reservoir induced. Recent analyses of induced seismic events at Nurek Reservoir U.S.S.R., show that the second stage of filling during August to December 1976, increasing the maximum depth from 120 m to 200 m, was accompanied by an intense burst of shallow seismic activity. An outward migration from the centre of the reservoir, possibly associated with diffusion of pore pressure, is revealed by the temporal distribution of <span class="hlt">earthquake</span> foci. A variety of investigations including the in situ measurement of tectonic stress, pore pressure, permeability, distribution of faults, etc., in addition to monitoring seismicity, have been undertaken in the vicinity of the Monticello Reservoir, South Carolina. The largest reservoir induced <span class="hlt">earthquake</span> is predicted not to exceed magnitude 5. The Koyna Reservoir, <span class="hlt">India</span>, continues to be the most outstanding example of RIS. Three <span class="hlt">earthquakes</span> of magnitude $˜5 occurred in September 1980. <span class="hlt">Earthquakes</span> of magnitude 4 occur frequently in the vicinity of Koyna, the latest being on February 5, 1983. Events that occurred during the period 1967-1973 have been relocated using better procedures and are found to be much shallower and the epicentres less diffused. Location of 12 <span class="hlt">earthquakes</span> of Ms ⩾ 4.0, their foreshocks and aftershocks</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70119141','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70119141"><span>Bayesian historical <span class="hlt">earthquake</span> relocation: an example from the 1909 Taipei <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Minson, Sarah E.; Lee, William H.K.</p> <p>2014-01-01</p> <p>Locating <span class="hlt">earthquakes</span> from the beginning of the modern instrumental period is complicated by the fact that there are few good-quality seismograms and what traveltimes do exist may be corrupted by both large phase-pick errors and clock errors. Here, we outline a Bayesian approach to simultaneous inference of not only the hypocentre location but also the clock errors at each station and the origin time of the <span class="hlt">earthquake</span>. This methodology improves the solution for the source location and also provides an uncertainty analysis on all of the parameters included in the inversion. As an example, we applied this Bayesian approach to the well-studied 1909 Mw 7 Taipei <span class="hlt">earthquake</span>. While our epicentre location and origin time for the 1909 Taipei <span class="hlt">earthquake</span> are consistent with earlier studies, our focal depth is significantly shallower suggesting a higher seismic hazard to the populous Taipei metropolitan area than previously supposed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S21B0700L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S21B0700L"><span>Comparison of aftershock sequences between 1975 Haicheng <span class="hlt">earthquake</span> and 1976 Tangshan <span class="hlt">earthquake</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Liu, B.</p> <p>2017-12-01</p> <p>The 1975 ML 7.3 Haicheng <span class="hlt">earthquake</span> and the 1976 ML 7.8 Tangshan <span class="hlt">earthquake</span> occurred in the same tectonic unit. There are significant differences in spatial-temporal distribution, number of aftershocks and time duration for the aftershock sequence followed by these two main shocks. As we all know, aftershocks could be triggered by the regional seismicity change derived from the main shock, which was caused by the Coulomb stress perturbation. Based on the rate- and state- dependent friction law, we quantitative estimated the possible aftershock time duration with a combination of seismicity data, and compared the results from different approaches. The results indicate that, aftershock time durations from the Tangshan main shock is several times of that form the Haicheng main shock. This can be explained by the significant relationship between aftershock time duration and <span class="hlt">earthquake</span> nucleation history, normal stressand shear stress loading rateon the fault. In fact the obvious difference of <span class="hlt">earthquake</span> nucleation history from these two main shocks is the foreshocks. 1975 Haicheng <span class="hlt">earthquake</span> has clear and long foreshocks, while 1976 Tangshan <span class="hlt">earthquake</span> did not have clear foreshocks. In that case, abundant foreshocks may mean a long and active nucleation process that may have changed (weakened) the rocks in the source regions, so they should have a shorter aftershock sequences for the reason that stress in weak rocks decay faster.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/27316652','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/27316652"><span>Spatio-temporal variation in chemical characteristics of PM10 over Indo Gangetic Plain of <span class="hlt">India</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Sharma, S K; Mandal, T K; Srivastava, M K; Chatterjee, A; Jain, Srishti; Saxena, M; Singh, B P; Saraswati; Sharma, A; Adak, A; K Ghosh, S</p> <p>2016-09-01</p> <p>The paper presents the spatio-temporal variation of chemical compositions (organic carbon (OC), elemental carbon (EC), and water-soluble inorganic ionic components (WSIC)) of particulate matter (PM10) over three locations (Delhi, Varanasi, and Kolkata) of Indo Gangetic Plain (IGP) of <span class="hlt">India</span> for the year 2011. The observational sites are chosen to represent the characteristics of upper (Delhi), middle (Varanasi), and lower (Kolkata) IGP regions as converse to earlier single-station observation. Average mass concentration of PM10 was observed higher in the middle IGP (Varanasi 206.2 ± 77.4 μg m(-3)) as compared to upper IGP (Delhi 202.3 ± 74.3 μg m(-3)) and lower IGP (Kolkata 171.5 ± 38.5 μg m(-3)). Large variation in OC values from 23.57 μg m(-3) (Delhi) to 12.74 μg m(-3) (Kolkata) indicating role of formation of secondary aerosols, whereas EC have not shown much variation with maximum concentration over Delhi (10.07 μg m(-3)) and minimum over Varanasi (7.72 μg m(-3)). As expected, a strong seasonal variation was observed in the mass concentration of PM10 as well as in its chemical composition over the three locations. Principal component analysis (PCA) identifies the contribution of secondary aerosol, biomass burning, fossil fuel combustion, vehicular emission, and sea salt to PM10 mass concentration at the observational sites of IGP, <span class="hlt">India</span>. Backward trajectory analysis indicated the influence of continental type aerosols being transported from the Bay of Bengal, Pakistan, Afghanistan, Rajasthan, <span class="hlt">Gujarat</span>, and surrounding areas to IGP region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/21789386','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/21789386"><span>Thoracic Injuries in <span class="hlt">earthquake</span>-related versus non-<span class="hlt">earthquake</span>-related trauma patients: differentiation via Multi-detector Computed Tomography.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Dong, Zhi-Hui; Yang, Zhi-Gang; Chen, Tian-Wu; Chu, Zhi-Gang; Deng, Wen; Shao, Heng</p> <p>2011-01-01</p> <p>Massive <span class="hlt">earthquakes</span> are harmful to humankind. This study of a historical cohort aimed to investigate the difference between <span class="hlt">earthquake</span>-related crush thoracic traumas and thoracic traumas unrelated to <span class="hlt">earthquakes</span> using a multi-detector Computed Tomography (CT). We retrospectively compared an <span class="hlt">earthquake</span>-exposed cohort of 215 thoracic trauma crush victims of the Sichuan <span class="hlt">earthquake</span> to a cohort of 215 non-<span class="hlt">earthquake</span>-related thoracic trauma patients, focusing on the lesions and coexisting injuries to the thoracic cage and the pulmonary parenchyma and pleura using a multi-detector CT. The incidence of rib fracture was elevated in the <span class="hlt">earthquake</span>-exposed cohort (143 vs. 66 patients in the non-<span class="hlt">earthquake</span>-exposed cohort, Risk Ratio (RR) = 2.2; p<0.001). Among these patients, those with more than 3 fractured ribs (106/143 vs. 41/66 patients, RR=1.2; p<0.05) or flail chest (45/143 vs. 11/66 patients, RR=1.9; p<0.05) were more frequently seen in the <span class="hlt">earthquake</span> cohort. <span class="hlt">Earthquake</span>-related crush injuries more frequently resulted in bilateral rib fractures (66/143 vs. 18/66 patients, RR= 1.7; p<0.01). Additionally, the incidence of non-rib fracture was higher in the <span class="hlt">earthquake</span> cohort (85 vs. 60 patients, RR= 1.4; p<0.01). Pulmonary parenchymal and pleural injuries were more frequently seen in <span class="hlt">earthquake</span>-related crush injuries (117 vs. 80 patients, RR=1.5 for parenchymal and 146 vs. 74 patients, RR = 2.0 for pleural injuries; p<0.001). Non-rib fractures, pulmonary parenchymal and pleural injuries had significant positive correlation with rib fractures in these two cohorts. Thoracic crush traumas resulting from the <span class="hlt">earthquake</span> were life threatening with a high incidence of bony thoracic fractures. The ribs were frequently involved in bilateral and severe types of fractures, which were accompanied by non-rib fractures, pulmonary parenchymal and pleural injuries.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/fs/2006/3016/2006-3016.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/fs/2006/3016/2006-3016.pdf"><span><span class="hlt">Earthquake</span> hazards: a national threat</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>,</p> <p>2006-01-01</p> <p><span class="hlt">Earthquakes</span> are one of the most costly natural hazards faced by the Nation, posing a significant risk to 75 million Americans in 39 States. The risks that <span class="hlt">earthquakes</span> pose to society, including death, injury, and economic loss, can be greatly reduced by (1) better planning, construction, and mitigation practices before <span class="hlt">earthquakes</span> happen, and (2) providing critical and timely information to improve response after they occur. As part of the multi-agency National <span class="hlt">Earthquake</span> Hazards Reduction Program, the U.S. Geological Survey (USGS) has the lead Federal responsibility to provide notification of <span class="hlt">earthquakes</span> in order to enhance public safety and to reduce losses through effective forecasts based on the best possible scientific information.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_25 --> <div class="footer-extlink text-muted" style="margin-bottom:1rem; text-align:center;">Some links on this page may take you to non-federal websites. 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