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  1. The Banda Arc subduction enigma

    NASA Astrophysics Data System (ADS)

    Spakman, Wim; Hall, Robert

    2010-05-01

    The spectacularly curved Banda arc comprises young oceanic crust enclosed by a volcanic inner arc, outer arc islands, and a trough parallel to the Australian continental margin. Seismicity defines a spoon-shaped lithospheric fold in the upper mantle for which there are two contrasting explanations: deformation of a single subducted slab, or two different slabs subducted from north and south. We show that the Banda arc resulted from subduction of a single slab. Based on geology and seismic tomography, we argue that the arc formed since 15 Ma by subduction of a Jurassic oceanic embayment within the Australian plate. Viewed in an Atlantic-Indian hotspot reference frame, the stationary E-W striking Java trench propagated ESE into the Banda embayment by hinge rollback. Extension of the upper plate formed oceanic crust in the present Banda Sea between stretched continental crust of Australian origin. Slab morphology depends primarily on the geometry of the continental margin enclosing the embayment. Our model explains the first order tectonic development of the Banda region and links slab deformation to absolute plate motion.

  2. Initial development of the Banda Volcanic Arc

    SciTech Connect

    Hartono, H.M.S. )

    1990-06-01

    The initial development of the Banda Volcanic Arc can be determined by obtaining absolute ages of granites or volcanics, stratigraphy of the Eocene Metan Volcanics of Timor as the oldest formation containing Banda Volcanic Arc extrusives, and tectonic analysis. Banda Arc volcanism is the result of subduction of oceanic crust under the volcanic arc. The time of initial subduction is related to initial seafloor spreading between Australia and Antarctica, which is identical to geomagnetic polarity time 34 (82 mybp). Therefore, 82 mybp can be used as one of the criteria to determine the birth of the Banda Volcanic Arc. With present available time data for determining the birth of the Banda Volcanic Arc, the minimum age coincides with the age of the Metan Volcanics (Eocene, 39-56 mybp) and the maximum age coincides with initial seafloor spreading between Australia and Antarctica (82 mybp). This time span is too long. With the assumption that it needs some time to develop from transcurrent faulting to subduction and volcanism, it is proposed that the initial development of Banda Arc volcanism was during early Tertiary.

  3. Map showing mineral resource potential of the Sierra Ancha Wilderness and Salome Study Area, Gila County, Arizona

    USGS Publications Warehouse

    Otton, James K.; Light, Thomas D.; Shride, Andrew F.; Bergquist, Joel R.; Wrucke, Chester T.; Theobald, Paul K.; Duval, Joseph S.; Wilson, Dolores M.

    1981-01-01

    The Wilderness Act (Public Law 88-577, Sept. 3, 1964) and certain related Acts require the Geological Survey and the Bureau of Mines to survey certain areas on Federal lands to determine their mineral-resource potential. Results must be made available to the public and be submitted to the Administration and the Congress. These maps and reports present the results of a geologic and mineral survey of the Sierra Ancha Wilderness and Salome Study Area, Gila County, Arizona.

  4. Geodynamic Evolution of the Banda Sea Region

    NASA Astrophysics Data System (ADS)

    Kaymakci, N.; Decker, J.; Orange, D.; Teas, P.; Van Heiningen, P.

    2013-12-01

    We've carried out a large on- and offshore study in Eastern Indonesia to characterize the major structures and to provide constraints on the Neogene geodynamic evolution of the Banda Sea region. The onshore portion utilized remote sensing data and published geology. We tied the onshore to the offshore using recently acquired high resolution bathymetric data (16m and 25m bin size) and 2D seismic profiles that extend from Sulawesi in the west to Irian Jaya in the east across the northern part of the Banda Arc. We interpret the northern boundary of the 'Birds Head' (BH) of Papua, the Sorong Fault, to be a sinistral strike-slip fault zone with a minimum of 48 km displacement over the last few million years. The western boundary fault of Cendrawasih Basin defines the eastern boundary of BH and corresponds to the Wandamen Peninsula which comprises high pressure metamorphic rocks, including eclogite and granulite facies rocks, with exhumation ages from 4 to 1 Ma. Earthquake focal mechanism solutions indicate that the eastern boundary of BH is linked with a large scale offshore normal fault which we suggest may be related to the exhumation of the Wandamen Peninsula. The eastern boundary of Cendrawasih Basin is defined by a large transpressive belt along which BH is decoupled from the rest of Papua / Irian Jaya. This interpretation is supported by recent GPS studies. We propose that the BH and the Pacific plate are coupled, and therefore the Birds Head is therefore completely detached from Irian Jaya. Furthermore, Aru Basin, located at the NE corner of Banda Arc, is a Fault-Fault-Transform (FFT) type triple junction. According to available literature information the Banda Sea includes three distinct basins with different geologic histories; the North Banda Sea Basin (NBSB) was opened during 12-7 Ma, Wetar-Damar Basin (WDB) during 7-3.5 Ma and Weber Basin (WB) 3-0 Ma. Our bathymetric and seismic data indicated that the NBSB and Weber Basin lack normal oceanic crust and are

  5. Towards Understanding the Sunda and Banda Arcs

    NASA Astrophysics Data System (ADS)

    Hall, R.

    2014-12-01

    The present change from oceanic subduction beneath the Sunda Arc to arc-continent collision east of Sumba is merely the latest stage in a complex collision history that began more than 20 million years ago. Understanding present-day tectonics requires restoring the pre-collisional margins and unravelling the history of the entire Sunda-Banda Arc, not just a segment centred on Sumba. Seismic tomography displays a single folded slab beneath the Banda Arc around which mantle has flowed. Above this is a wide actively deforming zone of complex geology. Australian crust was first added to the Sunda margin in the Cretaceous. Early Miocene closure of the oceanic gap north of Australia led to further additions of continental crust during collision of the Sula Spur. Few microcontinental fragments were sliced from New Guinea as commonly interpreted. Most are parts of the Sula Spur fragmented by extension and strike-slip faulting during development of subduction zones and rollback into the Banda embayment. Many metamorphic 'basement' rocks are significantly younger than expected. They were metamorphosed during multiple episodes of extension which also exhumed the sub-lithospheric mantle, melted the deep continental crust, created new ocean basins, and dispersed continental crust throughout the inner and outer arc, and forearc, so that in places Australian crust is colliding with Australian crust. Thus, many of the arc volcanoes are built on continental not oceanic crust, and sediment eroded from recently emergent islands is compositionally different to subducted sediment that contributed to arc magmas. The published literature is inadequate. New fieldwork and data are required, particularly in remote areas, with integration of information from a variety of sources (e.g. industry seismic and multibeam bathymetry, remotely acquired imagery) and sub-disciplines (e.g. geochronology, geochemistry, seismology, modelling). No single methodology can provide a complete solution.

  6. Exploration of the Banda orogen, Indonesia

    SciTech Connect

    Harris, R.A. ); Audley-Charles, M.G. ); Tobing, S.L. )

    1990-06-01

    An integrated geologic evaluation of the late Miocene to present Banda orogen and its petroleum potential is in progress. The focus of the investigation involves sedimentary sections of the NW Australian continental margin incorporated into the Banda orogen. The islands of Timor and Seram, and several other islands throughout the Banda orogenic arc, are the closest exposed lithostratigraphic equivalents of the hydrocarbon producing NW Australian subsurface stratigraphy. Hydrocarbon occurrences are well documented on many of the islands, and over 13 million barrels of oil have been produced from the Bula field in Seram. Recent studies of seeps in Timor and associated stratigraphic, structural, and geochemical relations indicate that (1) oil and gas seeps occur throughout the Permian to Pliocene stratigraphic section; (2) bituminous limestones of the Triassic Aituti Formation are the most likely source for many of the seeps; (3) preliminary geochemical analyses of the oils indicate a mixed terrestrial and marine organic source, and suggest a genetic link between the Aitutu oils and oils seeping from Tertiary reservoirs; (4) triterpane and sterane parameters indicate some of these oils are highly mature; (5) palynomorph coloration, conodont alteration, and clay mineralogy data yield paleotemperature estimates in the range of hydrocarbon generation from much of the pre-rift sequence (Permian-Jurassic); (6) structural modeling suggests that the initial decollement zone of the orogenic wedge formed near the Jurassic breakup unconformity of the underthrust NW Australian margin, imbricating the post-rift sequence; (7) in Timor and Seram the decollement has stepped to deeper levels involving prerift sequences that form structural culminations in the core of the orogen. The culminations are expressed as topographic highs as in New Guinea and Oman.

  7. Active tectonics of the eastern Sunda and Banda arcs

    NASA Astrophysics Data System (ADS)

    McCaffrey, Robert

    1988-12-01

    The mechanism of collision of the Australian continent with the East Sunda and Banda island arcs is examined. Depths and fault plane solutions of large earthquakes are estimated and are used to constrain the active, shallow tectonics of the collision zone. The convergence of the Australian continent with eastern Indonesia is accommodated to some degree by N-S crustal shortening throughout the forearc, arc, and back arc regions. Within the back arc (the Banda Basin), strike-slip and thrust faulting reveal convergence between Timor and Seram. Back arc thrusting plays an important role in the convergence across the collision zone. The Banda Basin probably formed as slices of northern New Guinea were transported westward with the Pacific plate and collided with an island arc in eastern Sulawesi.

  8. Arc-continent collision in Banda Sea region

    SciTech Connect

    Bowin, C.; Purdy, G.M.; Johnston, C.; Shor, G.; Lawver, L.; Hartono, H.M.S.; Jezek, P.

    1980-06-01

    A 2-month marine geophysical study of the Banda arc region was conducted in late 1976 using the R/V Atlantis II of WHOI' and the R/V Thomas Washington of SIO; 19 seismic refraction lines were successfully completed. Oceanic crust underlies the Banda Sea and Weber Deep. Continental crust 35 to 40 km thick underlies the Australian Shelf. Thick continental crust is also present beneath the Timor and Aru Troughs. Low-amplitude magnetic anomalies are present over the Australian Shelf and extend to near the western edge of the Banda outer arc and, together with the presence of metamorphic rocks, suggest that continental crust may extend to the eastern lip of the Weber Deep. Continuous seismic reflection profiling shows the Australian Shelf sedimentary sequence dipping beneath the accretionary prisms of the outer Banda arc at the Timor and Seram Troughs: the tectonic front of the subduction zone lies along the axis of these troughs. The bathymetric profile on the outer flank of the Timor and Seram Troughs is unusual in that the profile asymptotically approaches a shallow depth near sea level and no outer rise is present as at oceanic trenches. It is concluded that the Outer Banda arc from Buru around to Timor, and possibly to Sumba, contained Australian continental crustal blocks and fragments prior to its collision with the Australian margin in the last 3 to 6 m.y. Continuous convergence following the addition of a thick Australian margin sedimentary sequence to the south Banda subduction zone has led to deformation being distributed over the width of the arc and not simply being taken up on a single thrust surface. This scenario helps reconcile the geologic relations on Timor, Seram, and Buru with the structural continuity of the Timor Trough with the Java Trench. 30 figures, 1 table.

  9. Seismological constraints and speculations on Banda arc tectonics

    NASA Astrophysics Data System (ADS)

    McCaffrey, Robert

    Fault plane solutions of shallow earthquakes show that the collision of the Australian continent with the Banda Arc shortens the overriding Indonesian plate in the north-south direction and elongates it in the east-west direction by a combination of strike-slip and thrust faulting. The shallow tectonics and the distribution of deep earthquakes beneath the Banda Basin both indicate that two plates subduct beneath the Banda Arc; the Australia-Indian Ocean plate northward beneath the Java Trench, Timor Trough, and Aru Troughs, and the Bird's Head southwestward beneath the Seram Trough. The slab of the Indian Ocean plate forms a westward plunging synform beneath the Banda Basin. Its unusual shape in interpreted to have been caused by subduction beneath the westward moving Pacific plate which transported slivers of New Guinea into the back arc. The lithosphere of the Bird's Head was subducted beneath the Seram Trough and now reaches 300 km depth. At the surface decoupling between Australian and the Bird's Head probably occurs by left-lateral strike slip at the Tarera-Aiduna fault zone in western Irian Jaya and by convergence in the New Guinea fold-and-thrust belt. Seismic quiescence occurs at depths of 50 to 380 km beneath both Timor and the inactive volcanic arc to its north but the efficient propagation of S-waves through the same volume suggests that the lithospheric slab is continuous there. The lack of seismic and volcanic activity may result from removal of part of the Australian continental crust prior to subduction of the lower part of the lithosphere. This crust was stacked up to form the island of Timor.

  10. Seismic expression of Late Quaternary Banda submarine canyon and fan offshore northern Baja California

    SciTech Connect

    Legg, M.R.

    1987-05-01

    High-resolution seismic reflection profiles obtained throughout the inner California continental borderland offshore northwestern Baja California, Mexico, show the presence of numerous modern submarine canyons and associated fans. One set of these, the Banda submarine canyon/fan, is of relatively recent origin, as demonstrated by onlap of the basal fan sediments against an acoustically transparent, presumably hemipelagic deposit. Late Quaternary sedimentation rates inferred from isotopically dated piston core samples place the age of the postulated hemipelagic unit at approximately 650,000 years ago. The Banda submarine canyon heads within the Bahia Todos Santo and passes through a narrow gorge between Punta Banda and Islas Todos Santos. It is proposed that this submarine canyon and fan system formed entirely during late Quaternary time, following the breach of the Punta Banda ridge during a late Pleistocene high sea level stand. The presence of an ancient, buried channel exiting to the north out of Bahia Todos Santos probably marks the head of an earlier submarine canyon which acted as the conduit of clastic sediments from Valle Maneadero to the deep borderland basins. The now active Banda submarine canyon pirated the supply of terrigenous clastics from this older canyon. The active Agua Blanca fault zone cuts across the head of Banda submarine canyon, suggesting that tectonic movements may have played a role in the development of the Banda submarine canyon and fan system.

  11. Provenance of Mesozoic Sandstones in the Banda Arc, Indonesia

    NASA Astrophysics Data System (ADS)

    Zimmermann, S.; Hall, R.

    2014-12-01

    Quartz-rich sandstones in the Banda Arc islands of Tanimbar, Babar, Timor and Sumba are equivalent of Mesozoic sandstones on the Australian margin where they are important hydrocarbon reservoirs. They have been exposed by on-going collision providing an opportunity to study their provenance. Previous studies suggested that rivers draining Australia provided most input. New light mineral, heavy mineral and detrital zircon data provide information on sources of sediments and constraints on palaeogeographic models. Conventional light mineral plots of sandstones from the islands typically show a recycled orogen and continental block origin, consistent with an Australian source. However many of the sandstones are texturally immature. Many samples also contain volcanic quartz and volcanic lithic fragments. Heavy mineral assemblages of most samples contain material from acid igneous and metamorphic rocks, with few indications of mafic or ultramafic sources. Rounded ultrastable minerals are typical, but these are commonly mixed with angular grains. Detrital zircon (LA-ICP-MS) U-Pb ages range from Archean to Mesozoic, but variations in age populations indicate differences in source areas along the Banda Arc in locality and time. We recognise distinctive Permo-Triassic, older Palaeozoic and Proterozoic ages characteristic of a Bird's Head, New Guinea, acid igneous source and this component diminishes from east to west. On Tanimbar and Babar, sediment came from both Australia and the Bird's Head. Sandstones in Timor have immature textures and show differences from east to west. They contain zircons derived from the Birds Head, as well as Precambrian zircons suggesting a northern Australian origin. In contrast, immature textures, heavy minerals and Cretaceous zircon ages in rocks from Sumba suggest that they were mainly derived from metamorphic sources. Mesozoic to Archean zircons indicate derivation from Australian crust that had collided in Sulawesi during the Cretaceous.

  12. Delineating Biophysical Environments of the Sunda Banda Seascape, Indonesia

    PubMed Central

    Wang, Mingshu; Ahmadia, Gabby N.; Chollett, Iliana; Huang, Charles; Fox, Helen; Wijonarno, Anton; Madden, Marguerite

    2015-01-01

    The Sunda Banda Seascape (SBS), located in the center of the Coral Triangle, is a global center of marine biodiversity and a conservation priority. We proposed the first biophysical environmental delineation of the SBS using globally available satellite remote sensing and model-assimilated data to categorize this area into unique and meaningful biophysical classes. Specifically, the SBS was partitioned into eight biophysical classes characterized by similar sea surface temperature, chlorophyll a concentration, currents, and salinity patterns. Areas within each class were expected to have similar habitat types and ecosystem functions. Our work supplemented prevailing global marine management schemes by focusing in on a regional scale with finer spatial resolution. It also provided a baseline for academic research, ecological assessments and will facilitate marine spatial planning and conservation activities in the area. In addition, the framework and methods of delineating biophysical environments we presented can be expanded throughout the whole Coral Triangle to support research and conservation activities in this important region. PMID:25648170

  13. Paleomagnetic Study of Core MD012380 from Banda Sea

    NASA Astrophysics Data System (ADS)

    Lee, T.; Huang, Y.; Chen, C.; Yang, T.; Hsu, S.; Wei, K.

    2003-12-01

    This study presents the paleomagnetic results of core MD012380 taken from Banda Sea during IMAGES VII cruise in 2001. The locality of the coring site is 126o 54.25­ÝE and 5o45.64­ÝS, and the water depth is about 3232m. The total recovered length of this core is 39.9 m. The simulated paleo-intensity pattern is well correlated to that of the SINT 800 (Guyodo and Valet, 1999). Several magnetic events and excursions, such as Blake, Jarmaica, Lavantine, Big Lost Emperor, Delta and B/M Boundary could be identified. These events appeared at the depths of about 13.84 m, 18.05 m, 22.75 m, 31.81 m, 35.89 m, 38.70 m, respectively. Paleoinclination data also indicate that the boundary of Brunhes and Matuyama epochs appeared at the depth of 38.7 m. So, the paleomagnetic result is used to construct the age model of this core. Then, apply it to the studied oxygen isotope pattern and compare to that proposed by Bassinot et al. (1994), they are well correlated. In addition, the LAD of P. lacunosa is found at the depth of 28.4 m, which also supports the proposed age model. Result of magnetic susceptibility (c) shows several high peaks, especially at the bottom portion, which might relate to the volcanic activity in the surrounding area. Generally, high values occurred at the interglacial periods and low values appeared at the interglacial periods. However, magnetic susceptibility has a special increasing trend from stage 8 to the early stage 5. It may be worthy of further study.

  14. Surface deformation and slab-mantle interaction during Banda arc subduction rollback

    NASA Astrophysics Data System (ADS)

    Spakman, Wim; Hall, Robert

    2010-08-01

    The spectacularly curved Banda arc comprises young oceanic crust enclosed by a volcanic inner arc, outer arc islands and a trough parallel to the Australian continental margin. Strong seismic activity in the upper mantle defines a folded surface, for which there are two contrasting explanations: deformation of a single slab or two separate slabs subducting from the north and south. Here we combine seismic tomography with the plate tectonic evolution of the region to infer that the Banda arc results from subduction of a single slab. Our palaeogeographic reconstruction shows that a Jurassic embayment, which consisted of dense oceanic lithosphere enclosed by continental crust, once existed within the Australian plate. Banda subduction began about 15million years ago when active Java subduction tore eastwards into the embayment. The present morphology of the subducting slab is only partially controlled by the shape of the embayment. As the Australian plate moved northward at a high speed of about 7cmyr-1, the Banda oceanic slab rolled back towards the south-southeast accompanied by active delamination separating the crust from the denser mantle. Increasing resistance of the mantle to plate motion progressively folded the slab and caused strong deformation of the crust. The Banda arc represents an outstanding example of large-scale deformation of the Earth's crust in response to coupling between the crust, slab and surrounding mantle.

  15. [Tsunami in South-East Asia--rapid response deployment in Banda Aceh].

    PubMed

    Streuli, Rolf A

    2008-01-01

    On December 26, 2004 the second largest earthquake ever seismographically registered occurred in South-East Asia. It had a magnitude of 9.3 on Richter's scale and its epicentre was located on sea ground 160 km West of Banda Aceh, the capital of the province of Aceh on the island of Sumatra. The earthquake resulted in a tsunami which almost completely destroyed the city of Banda Aceh. Its death toll on the island of Sumatra was 168,000. The Swiss Humanitarian Aid Unit was deployed within a few days after the catastrophe with an advance team, which had to evaluate the need for supplies and personal in Banda Aceh. In close collaboration with relief forces of the Australian armed forces the team was able to deliver efficient medical and technical support. The most prevalent medical problems were: (1) Tsunami associated aspiration pneumonia; (2) Infected wounds of lower extremities; (3) Open bone fractures of lower extremities; (4) Tetanus infection. PMID:18399180

  16. Banda-Celebes-Sulu basin - a trapped Cretaceous-Eocene oceanic crust

    SciTech Connect

    Lee, C.S.; McCabe, R.

    1985-01-01

    The Banda, Celebes and Sulu Basins are three poorly understood marginal seas that are located at the junction of the Eurasian, Indian-Australian, Pacific and Philippine Sea plates. The incomplete data sets from each of these three marginal basins, the complex geological arrangement of the surrounding islands, and the compound late Cenozoic evolutions involving subduction, rifting, transform faulting and island arc collision have complicated any tectonic interpretations of this region. On the bases of marine geophysical data and on-land geology, the authors propose that the Banda, Celebes and Sulu Basins are the remanents of a once-continuous Cretaceous to Eocene ocean basin. Magnetic anomalies from the Banda, Celebes and Sulu Basins show the similar trends of about N70/sup 0/E, N60/sup 0/E and N55/sup 0/E respectively. Their best fit to the reversal models are as follows: (1) anomalies M1-M11 in the Banda Basin, (2) anomalies 30-33 in the Celebes Basin and (3) anomalies 17-20 in the Sulu Basin. The heat flow data from each of these basins is consistent with the relationship of our assigned magnetic ages. The on-land geology of this region is complicated by numerous land masses which dissect this old oceanic basin into the present configuration of marginal seas. The authors argue that each of these land masses arrived at its present location by either late Tertiary tectonic movements or has been built in place upon this older oceanic basement.

  17. The source rupture process of the Great Banda Sea earthquake of November 4, 1963

    NASA Astrophysics Data System (ADS)

    Welc, Joan L.; Thorne, Lay

    1987-04-01

    The Banda Sea earthquake of November 4, 1963 is one of the largest ( Mw = 8.3) intraplate events. It involved oblique thrusting at an intermediate depth within the subducted lithosphere near the abrupt bend in the southeastern Banda arc (6.86° S, 129.58° E). To better understand the tectonic significance of this earthquake, the detailed source process of the Banda Sea event was determined by body wave analysis. The rupture history was established by deconvolving source time functions from long-period P wave seismograms, using both individual station and multi-station time-domain deconvolution methods. The seismic moment release occurred within the first 50 s of rupture, initiating at a depth near 120 km and expanding laterally and downdip over a vertical extent of about 50 km. Slip and moment release were concentrated in one main region near the hypocenter, at depths between 110 and 130 km. The along-strike rupture length was only about 100 km, so it is difficult to resolve any horizontal directivity. The compressional stress orientation inferred from the focal mechanism parallels the strike of the slab, and reflects the importance of contortion of the lithosphere in this region. The Banda Sea event may be part of a major detachment at the leading edge of the subducted Australian continental shelf.

  18. Seismic response to recent tectonic processes in the Banda Arc region

    NASA Astrophysics Data System (ADS)

    Špičák, Aleš; Matějková, Radka; Vaněk, Jiří

    2013-03-01

    Internal structure and recent tectonics of the geologically complex Banda Arc region (latitude 1-9°S, longitude 124-135°E) have been studied by means of the analysis of global seismological data. Relocated hypocentral determinations of the International Seismological Center (EHB data) and fault plane solutions of the Global Centroid Moment Tensor Project have been used together with previously published information on regional geology and dynamics. The analysis considered earthquakes in the lithospheric wedges above subducting slabs and earthquakes in the uppermost portions of the Wadati-Benioff zones (focal depth < 100 km); we avoided intermediate-depth and deep earthquakes that are clearly separated from shallow ones by distinct discontinuities in the Wadati-Benioff zones. Such a selection best reflects present manifestations of tectonic processes. We delimitated 11 domains of earthquakes, each of them spatially distinct and with similar earthquake focal mechanisms. The number of events that did not fit in any domain was negligible. We associated each domain of earthquakes with distinct structural units and/or tectonic processes in the studied region. This correlation revealed that two discrete recent subduction zones act in the region - northward dipping Banda subduction in the south and southward dipping Seram subduction in the north. Though the shallow parts of the WBZs of both these subduction zones reach a similar depth of 100 km, the two WBZs differ substantially by dip angle and relation between shallow and intermediate-depth portions. A depth of 100 km of the shallow WBZs corresponds to - assuming an invariable plate convergence rate - a subduction cycle starting about 1-1.5 Ma ago. The present Banda subduction cycle follows the collisional event of the Timor-Tanimbar segment of the Australian plate; this collision now persists west and east of the Banda subduction zone around Timor and Tanimbar, as revealed by respective domains of earthquakes. No

  19. Recilia banda Kramer (Hemiptera: Cicadellidae), a vector of Napier stunt phytoplasma in Kenya.

    PubMed

    Obura, Evans; Midega, Charles A O; Masiga, Daniel; Pickett, John A; Hassan, Mohamed; Koji, Shinsaku; Khan, Zeyaur R

    2009-10-01

    Napier grass (Pennisetum purpureum) is the most important fodder crop in smallholder dairy production systems in East Africa, characterized by small zero-grazing units. It is also an important trap crop used in the management of cereal stemborers in maize in the region. However, production of Napier grass in the region is severely constrained by Napier stunt disease. The etiology of the disease is known to be a phytoplasma, 16SrXI strain. However, the putative insect vector was yet unknown. We sampled and identified five leafhopper and three planthopper species associated with Napier grass and used them as candidates in pathogen transmission experiments. Polymerase chain reaction (PCR), based on the highly conserved 16S gene, primed by P1/P6-R16F2n/R16R2 nested primer sets was used to diagnose phytoplasma on test plants and insects, before and after transmission experiments. Healthy plants were exposed for 60 days to insects that had fed on diseased plants and acquired phytoplasma. The plants were then incubated for another 30 days. Nested PCR analyses showed that 58.3% of plants exposed to Recilia banda Kramer (Hemiptera: Cicadellidae) were positive for phytoplasma and developed characteristic stunt disease symptoms while 60% of R. banda insect samples were similarly phytoplasma positive. We compared the nucleotide sequences of the phytoplasma isolated from R. banda, Napier grass on which these insects were fed, and Napier grass infected by R. banda, and found them to be virtually identical. The results confirm that R. banda transmits Napier stunt phytoplasma in western Kenya, and may be the key vector of Napier stunt disease in this region.

  20. Recilia banda Kramer (Hemiptera: Cicadellidae), a vector of Napier stunt phytoplasma in Kenya

    NASA Astrophysics Data System (ADS)

    Obura, Evans; Midega, Charles A. O.; Masiga, Daniel; Pickett, John A.; Hassan, Mohamed; Koji, Shinsaku; Khan, Zeyaur R.

    2009-10-01

    Napier grass ( Pennisetum purpureum) is the most important fodder crop in smallholder dairy production systems in East Africa, characterized by small zero-grazing units. It is also an important trap crop used in the management of cereal stemborers in maize in the region. However, production of Napier grass in the region is severely constrained by Napier stunt disease. The etiology of the disease is known to be a phytoplasma, 16SrXI strain. However, the putative insect vector was yet unknown. We sampled and identified five leafhopper and three planthopper species associated with Napier grass and used them as candidates in pathogen transmission experiments. Polymerase chain reaction (PCR), based on the highly conserved 16S gene, primed by P1/P6-R16F2n/R16R2 nested primer sets was used to diagnose phytoplasma on test plants and insects, before and after transmission experiments. Healthy plants were exposed for 60 days to insects that had fed on diseased plants and acquired phytoplasma. The plants were then incubated for another 30 days. Nested PCR analyses showed that 58.3% of plants exposed to Recilia banda Kramer (Hemiptera: Cicadellidae) were positive for phytoplasma and developed characteristic stunt disease symptoms while 60% of R. banda insect samples were similarly phytoplasma positive. We compared the nucleotide sequences of the phytoplasma isolated from R. banda, Napier grass on which these insects were fed, and Napier grass infected by R. banda, and found them to be virtually identical. The results confirm that R. banda transmits Napier stunt phytoplasma in western Kenya, and may be the key vector of Napier stunt disease in this region.

  1. Mapping magma sources in the east Sunda-Banda arcs, Indonesia: Constraints from helium isotopes

    NASA Astrophysics Data System (ADS)

    Hilton, D. R.; Hoogewerff, J. A.; van Bergen, M. J.; Hammerschmidt, K.

    1992-02-01

    We report new helium isotope analyses of olivine and clinopyroxene separates from recent lavas for eleven volcanoes from Flores in the east Sunda arc through the inactive segment between the arcs to Banda Island at the extreme of the contiguous Banda arc. In the east Sunda arc, 3He /4He ratios ( R) vary between 4.5 RA ( R A = air 3He /4He ) for the leucitic Batu Tara volcano to a remarkable low of pure radiogenic helium (0.0075 RA) for Werung at the southern tip of Lomblen Island. Lavas from the inactive zone, which represents the locus of collision of the Australian continent with the arc, have a narrower range in R/R A - from 3.9 for Kisu in the straits of Pantar to 1.0 for Romang Island. Our one locality (Banda Island) in the Banda arc gives the highest R/R A ratio (3.1) observed along this arc to date. The results are consistent with the involvement of crustal material in magma genesis throughout the east Sunda/Banda arcs, as far west as Iya in central Flores. We combine these helium isotope results with published and on-going strontium isotope studies, and show that the source of the helium in the crustal component is unlikely to be terrigenous sediments derived from the Australian continent; rather, degassing of Australian continental crust appears to be the dominant process controlling the helium budget. The He-Sr isotope systematics also provide a framework to account for the areal pattern of 3He /4He in this part of the arcs: the radiogenic crustal component is diluted with mantle helium both in a down-dip direction and with increasing lateral distance from the collision zone. These factors result in an excellent first-order relationship between the 3He /4He ratio, degree of He/Sr enrichment (relative to the postulated mantle endmember), and alkalinity of the erupted lavas. Such a relationship has a direct bearing on models of the tectonic evolution of the collision zone, and on the observation that helium isotopes are decoupled from strontium and other

  2. 40 CFR 180.1319 - Banda de Lupinus albus doce (BLAD); exemption from the requirement of a tolerance.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... catabolism of a seed storage protein (β-conglutin) of sweet lupines (Lupinus albus), in or on all food... RESIDUES IN FOOD Exemptions From Tolerances § 180.1319 Banda de Lupinus albus doce (BLAD); exemption...

  3. Estimation of primary productivity in Banda Sea using the vertical distribution model

    NASA Astrophysics Data System (ADS)

    Kemili, Putri; Putri, Mutiara R.

    2014-03-01

    To estimate Net Primary Productivity (NPP) which more represent nature condition, it is important to know both horizontal and vertical distribution. Carbon-based Productivity Model (CbPM) used to calculate NPP in 15 layers of depth. Gauss equation and Lambert Beer Law used to estimate chlorophyll-a and light intensity in each layer from satellite-derived data, whereas the temperature data obtained from model result of HAMburg Shelf Ocean Model (HAMSOM). This model is being applied to verified and describe how the NPP had been distributed in Banda Sea on 2006. Verification results show that CbPM algorithm has clearly give less error in data observation than what Vertically Generalized Production Model (VGPM) algorithm did, which stand on the error average approximately 33%. The results also show that the vertical distribution of NPP in Banda Sea indicate a seasonal variation.

  4. Continent-arc collision in the Banda Arc imaged by ambient noise tomography

    NASA Astrophysics Data System (ADS)

    Porritt, Robert W.; Miller, Meghan S.; O'Driscoll, Leland J.; Harris, Cooper W.; Roosmawati, Nova; Teofilo da Costa, Luis

    2016-09-01

    The tectonic configuration of the Banda region in southeast Asia captures the spatial transition from subduction of Indian Ocean lithosphere to subduction and collision of the Australian continental lithosphere beneath the Banda Arc. An ongoing broadband seismic deployment funded by NSF is aimed at better understanding the mantle and lithospheric structure in the region and the relationship of the arc-continent collision to orogenesis. Here, we present results from ambient noise tomography in the region utilizing this temporary deployment of 30 broadband instruments and 39 permanent stations in Indonesia, Timor Leste, and Australia. We measure dispersion curves for over 21,000 inter-station paths resulting in good recovery of the velocity structure of the crust and upper mantle beneath the Savu Sea, Timor Leste, and the Nusa Tenggara Timur (NTT) region of Indonesia. The resulting three dimensional model indicates up to ∼25% variation in shear velocity throughout the plate boundary region; first-order velocity anomalies are associated with the subducting oceanic lithosphere, subducted Australian continental lithosphere, obducted oceanic sediments forming the core of the island of Timor, and high velocity anomalies in the Savu Sea and Sumba. The structure in Sumba and the Savu Sea is consistent with an uplifting forearc sliver. Beneath the island of Timor, we confirm earlier inferences of pervasive crustal duplexing from surface mapping, and establish a link to underlying structural features in the lowermost crust and uppermost mantle that drive upper crustal shortening. Finally, our images of the volcanic arc under Flores, Wetar, and Alor show high velocity structures of the Banda Terrane, but also a clear low velocity anomaly at the transition between subduction of oceanic and continental lithosphere. Given that the footprint of the Banda Terrane has previously been poorly defined, this model provides important constraints on tectonic reconstructions that

  5. The Vrancea seismic zone and its analogue in the Banda Arc, eastern Indonesia

    NASA Astrophysics Data System (ADS)

    Milsom, John

    2005-12-01

    It is now widely, although not universally, accepted that the Carpathian orogen marks the site of an arc-continent collision that followed the subduction of a now vanished small ocean basin. Seismic tomography has defined a high-velocity anomaly in the upper mantle similar to those associated with subduction zones worldwide. There is, however, no recognisable Wadati-Benioff Zone (WBZ), and intermediate-depth seismicity is confined to a relatively small, roughly cylindrical and vertically elongated region beneath the extreme southeastern corner of the mountain chain. There is no consensus in the published studies as to the origin of this 'Vrancea Zone'. The Banda Sea region of eastern Indonesia has sometimes been cited as an analogue for the Pannonian/Transylvanian basin and the enclosing Carpathian orocline, but at first sight the patterns of seismicity appear very different. Intermediate depth seismic activity defines a subducted slab that dips north, south and west beneath the Banda Sea, a configuration explained as a consequence of the rapid expansion of the sea during roll-back subduction. If the similar scenario proposed for the Carpathians is correct, then it is the absence of a Carpathian WBZ that is actually anomalous. Closer examination of Banda Arc seismicity shows that it can be divided into two parts, these being a scoop-shaped WBZ and an adjacent 'Damar Zone' of much more intense intermediate-depth activity. At its eastern end the Damar Zone merges with the WBZ, but in the west there is evidence for separation from it. A plausible explanation of this pattern is that a lower layer of the downgoing slab is peeling away from the remainder. The Banda/Australia collision is now almost complete and the activity in the WBZ proper can be expected to decrease. Damar Zone activity, on the other hand, may persist for a much longer period, migrating towards the foreland as the detaching layer separates from the remainder of the subducted lithosphere. In a few

  6. Major earthquakes and tsunami of the Banda Arc region, Indonesia: the past 400 years

    NASA Astrophysics Data System (ADS)

    Fisher, T. L.; Harris, R. A.; Liu, Y.; Major, J. R.; Baird, N.

    2011-12-01

    Dutch historical records document several large earthquakes and tsunami throughout eastern Indonesia that we use to assess geophysical hazards in this densely populated region. For example, a large earthquake in 1629 generated a tsunami at least 15 m high. The first wave arrived at Banda Neira 30 minuets after violent shaking ceased. The event was followed by at least 8 years of aftershocks and other strong earthquakes over the next few decades. These data are consistent with a mega-thrust earthquake of Mw > 8.8 on the Seram Trough to the east or a >Mw 9.0 earthquake on the Timor-Tanimbar Trough to the south. Smaller tsunami from regional earthquakes that inflicted heavy damage throughout the Banda Arc is also documented in 1648, 1672, 1674 (2 m wave), 1710, 1754, 1778, 1802, 1820 (>20 m wave), 1835, 1836 (wave) and 1852 (8 m wave). These events are likely associated with earthquake activity along the thrust front of the collision zone or along a developing thrust system in the back arc. For example, the > 20 m wave from the 1820 event struck SE Sulawesi after 2-4 minuets of violent shaking throughout a region spanning over 1000 km. The most likely source for this event is the Flores Thrust, which produced a much smaller tsunami from a Mw 7.8 earthquake in 1992. However, the 1820 event is most likely > Mw 8.5 to produce a tsunami as large as the one recorded, 17 years of aftershocks and two possible related nearby volcanic eruptions. Since the seismic drama of 1629-1852, only one earthquake of > Mw 8 is documented in the Banda Arc region, and it was not along the subduction zone interface (Okal and Reymond, 2003). During this time of relative seismic quiescence at least 11 m of strain has accumulated across the active Banda arc-continent collision. A similar scenario is currently playing out in western Indonesia where Dutch records proved extremely reliable in documenting several mega-thrust earthquakes during the 18th and 19th centuries that are reoccurring and

  7. Imaging the Subduction of Continental Lithosphere in the Banda Sea Region

    NASA Astrophysics Data System (ADS)

    Fichtner, A.; De Wit, M.; van Bergen, M.

    2014-12-01

    We present a 3D tomographic model of Australasia obtained by full seismic waveform inversion. Our model features a sharp lateral velocity contrast extending to >200 km depth, coincident with the abrupt transition from low to high Helium ratios in arc volcanics near 123°E (see figure). The joint analysis of the tomographic model and isotope data (for He, Pb, Nd, Sr) suggests that the North Australian craton subducted beneath the Banda Sea to around 100 km depth. The continuous increase of computing power combined with advances in numerical seismology allow us to develop full waveform inversion techniques that translate complete seismograms into 3D Earth models. The natural incorporation of any type of body and surface waves in full waveform inversion improves tomographic resolution in terms of both resolution length and amplitude recovery. We applied full waveform inversion to Australasia, including the Sunda and Banda arcs. The correlation of the tomographic model with isotope signatures of arc volcanics supports the shallow-angle subduction of North Australian lithosphere. The integrated data suggest that the late Jurassic ocean lithosphere north of the North Australian craton was capable of entraining large volumes of continental lithosphere. A plausible explanation involves delamination within the continental crust, separating upper from lower crustal units. This interpretation is consistent with the existence of a massive accretionary complex on Timor island, with evidence from Pb isotope analysis for lower-crust involvement in arc volcanism; and with the approximate gravitational stability of the subducted lithosphere as inferred from the tomographic images. The Banda arc example demonstrates that continental lithosphere in arc-continent collisions may not generally be preserved, thus increasing the complexity of tectonic reconstructions and models of recycling continental crust.

  8. Extreme extension across Seram and Ambon, eastern Indonesia: evidence for Banda slab rollback

    NASA Astrophysics Data System (ADS)

    Pownall, J. M.; Hall, R.; Watkinson, I. M.

    2013-09-01

    The island of Seram, which lies in the northern part of the 180°-curved Banda Arc, has previously been interpreted as a fold-and-thrust belt formed during arc-continent collision, which incorporates ophiolites intruded by granites thought to have been produced by anatexis within a metamorphic sole. However, new geological mapping and a re-examination of the field relations cause us to question this model. We instead propose that there is evidence for recent and rapid N-S extension that has caused the high-temperature exhumation of lherzolites beneath low-angle lithospheric detachment faults that induced high-temperature metamorphism and melting in overlying crustal rocks. These "Kobipoto Complex" migmatites include highly residual Al-Mg-rich garnet + cordierite + sillimanite + spinel + corundum granulites (exposed in the Kobipoto Mountains) which contain coexisting spinel + quartz, indicating that peak metamorphic temperatures likely approached 900 °C. Associated with these residual granulites are voluminous Mio-Pliocene granitic diatexites, or "cordierite granites", which crop out on Ambon, western Seram, and in the Kobipoto Mountains and incorporate abundant schlieren of spinel- and sillimanite-bearing residuum. Quaternary "ambonites" (cordierite + garnet dacites) emplaced on Ambon were also evidently sourced from the Kobipoto Complex migmatites as demonstrated by granulite-inherited xenoliths. Exhumation of the hot peridotites and granulite-facies Kobipoto Complex migmatites to shallower structural levels caused greenschist- to lower-amphibolite facies metapelites and amphibolites of the Tehoru Formation to be overprinted by sillimanite-grade metamorphism, migmatisation, and limited localised anatexis to form the Taunusa Complex. The extreme extension required to have driven Kobipoto Complex exhumation evidently occurred throughout Seram and along much of the northern Banda Arc. The lherzolites must have been juxtaposed against the crust at typical

  9. DDT in Mytilus edulis: Spatio-temporal variations in the Punta Banda estuary, Baja California, Mexico

    SciTech Connect

    Galindo-Bect, M.S.; Flores-Baez, B.P. )

    1991-02-01

    The mussel Mytilus sp. has been widely used as a sentinel organism or biological indicator of organic pollutants in the marine environment. In studies recently carried out in Baja California, Mexico, it was found that the spatial and temporal variations of DDT in samples of the mussel Mytilus californianus collected from the area exposed to the ocean do not follow a defined pattern and that the highest values of DDT are found at the border with the US. The Maneadero Valley in Baja California, Mexico, is an agricultural area where important volumes of pesticides are applied, part of which are transported to the Punta Banda Estuary where they remain for an undetermined period of time during which they are consumed and bioaccumulated by organisms. The main objective of the present work is to determine the levels and temporal variation of DDT in the mussel Mytilus edulis in the Punta Banda Estuary, Baja California. With the results, the authors will define the dynamics of this pollutant in the estuary.

  10. Autocracy and AIDS: the post-Banda challenge. Country focus: Malawi.

    PubMed

    Mhone, C S

    1996-10-01

    Hastings Banda ruled Malawi for three decades until 1993. During that period, it was considered taboo to publicly discuss sexual matters. Efforts to prevent and control the spread of HIV/AIDS therefore got fully underway only after the end of Banda's autocratic regime. There are now an estimated 225,000 cases of AIDS in Malawi. The Ministry of Health estimates that 33% of urban adults and 17% of rural adults are HIV positive, approximately 10% of the total population. In some urban areas, 33% of women attending antenatal clinics and 70-98% of prostitutes are HIV positive. The high prevalence of sexually transmitted diseases and the practice of dry sex are thought to be major cofactors in bringing about such high rates of HIV infection. Several surveys do, however, indicate that the rate of growth of the HIV epidemic may be slowing. Even if the projected decrease in the incidence of new infections actually occurs, the cumulative HIV prevalence will continue to increase. Malawi, one of the world's poorest nations, with a per capita income of $140 and a literacy rate of 47%, cannot afford the overwhelming burden of providing comprehensive care to the segment of its population which suffers with AIDS. The author stresses the need for AIDS education in primary schools, especially since many students drop out prior to secondary school.

  11. A Neogene back-arc origin for the Banda Sea basins: geochemical and geochronological constraints from the Banda ridges (East Indonesia)

    NASA Astrophysics Data System (ADS)

    Honthaas, Christian; Réhault, Jean-Pierre; Maury, René C.; Bellon, Hervé; Hémond, Christophe; Malod, Jacques-André; Cornée, Jean-Jacques; Villeneuve, Michel; Cotten, Joseph; Burhanuddin, Safri; Guillou, Hervé; Arnaud, Nicolas

    1998-12-01

    Dredgings conducted during the French-Indonesian cruises Banda Sea II and III collected volcanic rocks from several ridges of the Banda Sea area (Tukang Besi ridge, site 218; Lucipara ridge, sites 214 and 305; Nieuwerkerk-Emperor of China, sites 219 and 220). With the exception of one 46-Ma-old N-MORB type basalt, thought to belong to an ophiolitic complex, K-Ar and Ar-Ar datings indicate that all the dredged volcanics are Neogene. They range in age from ca. 10 Ma (Tukang Besi back-arc basalts) to 8-7 Ma (Nieuwerkerk-Emperor of China calc-alkaline andesites) and to 7-3 Ma (Lucipara OIB-type transitional basalts and cordierite-bearing andesites). Radiogenic isotopic signatures of andesites are consistent with an AFC (Assimilation coupled with Fractional Crystallization) process involving assimilation of continental crust. 8-3-Ma-old calc-alkaline volcanic activity is also recorded on the Wetar segment, an inactive part of the East Sunda arc, and corresponding isotopic compositions are also consistent with an AFC process involving continental crust. These features suggest that Lucipara-Nieuwerkerk-Emperor of China ridges and the Wetar segment were representing a single volcanic arc 8-7 Ma ago. The corresponding calc-alkaline activity was related to the subduction of the Indian oceanic lithosphere beneath continental blocks of Australian origin. Back-arc opening processes occurred from 6 to 3 Ma as a multi-rift opening for the Wetar basin and as a single-rift opening for the Damar basin while subduction-related magmatism was still active in the Wetar segment. Volcanic activity stopped at 7 Ma in the Nieuwerkerk-Emperor of China ridge. On Lucipara ridge, 6-3 Ma volcanic activity emplaced concomitantly transitional basalts and cordierite-bearing andesites. The mineralogical and chemical features of the latter are consistent with an AFC process involving assimilation of continental crust by mantle-derived basaltic magmas. The end of magmatic activity on both volcanic

  12. Short-wavelength, high-amplitude gravity anomalies around the Banda Sea, and the collapse of the Sulawesi orogen

    NASA Astrophysics Data System (ADS)

    Milsom, J.; Sardjono; Susilo, A.

    2001-04-01

    In eastern Indonesia, high-density ophiolitic rocks outcropping on islands surrounding the Banda Sea are in many cases associated with strong gravity anomalies and steep gravity gradients. However, the relationships are not always straightforward. Bouguer gravity levels and gradients over the extensive East Sulawesi Ophiolite are generally relatively low, although short-wavelength, high amplitude anomalies indicate rapid changes in thickness of high-density rocks in a few places. In the Banda Arc, most local positive anomalies due to ophiolites are superimposed on a steep regional gravity gradient but in one case, in western Seram, there is a distinct and important spatial separation between the two. On Buru, west of Seram, a gradient of more than 10 mGal/km testifies to the presence of very dense rocks in the near subsurface, despite the absence of ophiolites in the outcrop. Gravity variations and ophiolite distribution around the Banda Sea are compatible with extension having occurred in the Sulawesi region following, and as a result of, Oligo-Miocene collision with an Australian-derived microcontinent. Similar histories have been proposed for many Mediterranean deep basins of similar size, shape and character, and emplacement of some of the high-density masses in the Banda Arc has probably resembled at least the later stages in the emplacement of peridotite massifs in the Rif-Betic belt. In both areas the present close association of the ultramafic rocks and their associated local anomalies with a strong regional gravity gradient is largely coincidental.

  13. Extreme extension across Seram and Ambon, eastern Indonesia: Evidence for Banda slab rollback

    NASA Astrophysics Data System (ADS)

    Pownall, J. M.; Hall, R.; Watkinson, I. M.

    2013-04-01

    The island of Seram, which lies in the northern part of the 180°-curved Banda Arc, has previously been interpreted as a fold-and-thrust belt formed during arc-continent collision, which incorporates ophiolites intruded by granites thought to have been produced by anatexis within a metamorphic "sole". However, new geological mapping and a re-examination of the field relations cause us to question this model. We instead propose that there is evidence for recent N-S extension that has caused the high-temperature exhumation of hot mantle peridotites, granites, and granulites (the "Kobipoto Complex") beneath low-angle lithospheric detachment faults. Greenschist- to lower-amphibolite facies metapelites and amphibolites of the Tehoru Formation, which comprise the hanging wall above the detachment faults, were overprinted by sillimanite-grade metamorphism, migmatisation and limited localised diatexis to form the Taunusa Complex. Highly aluminous metapelitic garnet + cordierite + sillimanite + spinel + corundum + quartz granulites exposed in the Kobipoto Mountains (central Seram) are intimately associated with the peridotites. Spinel + quartz inclusions in garnet, which indicate that peak metamorphic temperatures for the granulites likely approached 900 °C, confirm that peridotite was juxtaposed against the crust at typical lithospheric mantle temperatures and could not have been part of a cooled ophiolite. Some granulites experienced slight metatexis, but the majority underwent more advanced in situ anatexis to produce widespread granitic diatexites characterised by abundant cordierite and garnet xenocrysts and numerous restitic sillimanite + spinel "clots". These Mio-Pliocene "cordierite granites", which are present throughout Ambon, western Seram, and the Kobipoto Mountains in direct association with peridotites, demonstrate that the extreme extension required to have driven Kobipoto Complex exhumation must have occurred along much of the northern Banda Arc. In central

  14. Preliminary results of characteristic seismic anisotropy beneath Sunda-Banda subduction-collision zone

    SciTech Connect

    Wiyono, Samsul H.; Nugraha, Andri Dian

    2015-04-24

    Determining of seismic anisotropy allowed us for understanding the deformation processes that occured in the past and present. In this study, we performed shear wave splitting to characterize seismic anisotropy beneath Sunda-Banda subduction-collision zone. For about 1,610 XKS waveforms from INATEWS-BMKG networks have been analyzed. From its measurements showed that fast polarization direction is consistent with trench-perpendicular orientation but several stations presented different orientation. We also compared between fast polarization direction with absolute plate motion in the no net rotation and hotspot frame. Its result showed that both absolute plate motion frame had strong correlation with fast polarization direction. Strong correlation between the fast polarization direction and the absolute plate motion can be interpreted as the possibility of dominant anisotropy is in the asthenosphere.

  15. Arc-parallel extrusion of the Timor sector of the Banda arc-continent collision

    NASA Astrophysics Data System (ADS)

    Duffy, Brendan; Quigley, Mark; Harris, Ron; Ring, Uwe

    2013-06-01

    studies of synorogenic basins in Timor using field and remote sensing techniques provide new structural and geomorphic evidence for syn-collisional extension in the converging plate boundary zone between the Australian Plate and Banda Arc. Fault mapping and kinematic analysis at scales ranging from outcrop (<1 m2) to the dimensions of the active orogen in East Timor (~100 km2) identify a predominance of NW-SE oriented dextral-normal faults and NE-SW oriented sinistral-normal faults that collectively bound large (5-20 km2) bedrock massifs throughout the island. These fault systems intersect at non-Andersonian conjugate angles of approximately 120° and accommodate an estimated 20 km of NE-directed extension across the Timor orogen based on reconstructions of fault-dismembered massifs. Major orogen-parallel ENE-oriented faults on the northern and southern sides of Timor exhibit normal-sinistral and normal-dextral kinematics, respectively. The overall pattern of deformation is one of lateral crustal extrusion sub-parallel to the Banda Arc. Stratigraphic relationships suggest that extrusion began prior to 5.5 Ma, before pronounced rapid uplift of the orogen. We link this to progressive coupling of the fore-arc to an underthrust plateau on the Australian Plate and subduction of its ocean crust. Our results enable us to track the structural evolution of the upper crust during dramatic plate-boundary reorganizations accompanying the transition from subduction to collision. The deformation structures that we document suggest that both upper and lower plate deformation during incipient island arc-continent collision was largely controlled by the geometry and topography of the lower plate.

  16. Late Miocene obduction and microplate migration around the southern Banda Sea and the closure of the Indonesian Seaway

    NASA Astrophysics Data System (ADS)

    Linthout, Kees; Helmers, Henk; Sopaheluwakan, Jan

    1997-11-01

    Miocene shallowing and closure of the Indonesian Seaway between the Indian Ocean and the Pacific is related to plate-tectonic developments at the southern margins of the Banda Sea. Ultramafites, mainly lherzolite, closely associated with quartzo-pelitic metamorphic rocks, on the northern coast of Timor and on smaller islands in the southern Outer Banda Arc and also on southwest Seram in the northern Banda Arc, are fragments of Middle Miocene oceanic lithosphere obducted in the Late Miocene on sole rock of Australian continental origin. Initially cool sole rock was dynamo-thermally metamorphosed by heating from above by very hot, overriding oceanic lithosphere. Temperature equilibration between the sole and the Kaibobo lherzolitic complex (southwest Seram) took place at about 740°C and 4-5 kbar. Anatectic granitic magma formed in the sole and intruded in the ultramafite. 40Ar 39Ar determinations on muscovite and biotite from the sole and anatectic granite indicate that the system cooled through 400°C 6.0 Ma ago and through 320°C 0.5 Ma later. P-T-t modelling of the obduction/post-obduction exhumation curve, which is based on thermobarometry of the Kaibobo ultramafic complex and its sole, suggests that obduction started about 9.5 Ma, emplacement was completed about 8 Ma ago and that fast vertical movements continued until about 7 Ma. The obduction of the Kaibobo lherzolitic complex actually took place in an area northeast of the current position of Tanimbar, where Seram (as a micro-continental Australian fragment) lay 8 Ma ago, as it migrated northward with the Australian Plate. The reconstructed obduction site of the southwest Seram ultramafites and those between northern Timor and Tanimbar determine an 850 km-long, ENE-trending zone along the southern margin of the Banda Sea. As the obduction of the lherzolitic complex on northern Timor also took place 8 Ma ago and cooling to 300°C occurred 5.5 Ma ago, a similar time setting to Kaibobo is inferred. It is

  17. Tectonic Evolution of the Banda Arc-Continent Collision in the Timor Region

    NASA Astrophysics Data System (ADS)

    Harris, R. A.

    2011-12-01

    Recent detailed studies of the active Banda arc-continent collision reveal many new features about its tectonic evolution, such as (1) when collision initiated, (2) conditions and age of metamorphism, (3) timing of island emergence and exhumation, (4) how the arc is affected by collision, (5) differences between rock and surface uplift rates, (6) the temporal distribution of strain and (7) natural hazards. (1) The youngest Australian continental margin material incorporated into the Banda orogen is 7-8 Ma in East Timor and 6 Ma in West Timor. (2) Collision-related metamorphic rocks in East Timor yield max. temperatures of 850 °C and pressures of 12 kb. The age of the metamorphism is constrained by zircon U/Pb ages of 6.7 Ma. (3) Island emergence and erosional exhumation is constrained by foraminifera depth vs. age estimates of the transition from deep marine chalk to distal turbidite deposition at 4.2 Ma in East Timor and younger to the east and west. Exhumation of metamorphic rocks is constrained by amphibole with Ar/Ar cooling ages of ~6 Ma (~525°C), zircons with U/He ages of 4.5 Ma (215°C), and apatite with U/He ages of 3.5 Ma (90°C). Younger exhumation ages are found to the south. (4) Contamination of the volcanic arc by subducted continental material is first detected in eroded arc islands near East Timor at 5 Ma. The age of contamination youngs both east and west in less eroded, active arc islands. The main arc edifice north of East Timor is abandoned at 1-3 Ma and is shifted 30 km to the north by the Wetar backarc thrust. A new volcanic center emerges further north. (5) Coral terraces encrust the rising islands and yield highly variable uplift rates, with some as high as 1.5 mm/a. The highest rates correspond with active thrust faults and diapirs. Rock uplift rates associated with exhumation of the schist belt are as high as 8 mm/a. (6) GPS velocities in the most advanced part of the collision (central Timor) show that 70% of the 70 mm/a convergence

  18. Lithofacies and depositional pattern of sea floor sediments in the North Banda Sea, Indonesia

    NASA Astrophysics Data System (ADS)

    Situmorang, M.

    A systematic coring and seismic survey across the northern Banda Arc reveals various Quaternary lithofacies deposited in particular morphotectonic environments. Terrigenous and volcanogenic deposits exist in volcanic arc areas, in step-faulted basins and large local structural escarpments with steep slopes which generate debris and mass-gravity flows. Sedimentologic data suggest that volcanogenic sediments are derived from the Bandaneira volcanic complex. The eastern part is marked by benches and notches that exhibit peculiar flat-lying layers mostly of sandy turbidites. Silt turbidites are found in the deepest part in the Weber Deep. Furthermore, spatial distribution of the gravels and their lithology suggest source areas in the west and northeast. Whilst the structural highs represented by isolated sharp ridges are characterized by the presence of gravel deposits, slumping and mass-gravity flows play a major role in sediment deposition. Seram Trench is indicated by distinct flat-lying seismic reflections of trench-fill deposits of pelagic and sand turbidite deposits. The continental slopes consist of blocks of slides and slumps, and are prone to slumping. They are covered by ooze and pelagic deposits. On the other hand a flat terrace-like morphology represents the continental shelf with uniform, consistent lithology of biogenous sand and mud.

  19. Lutzomyia migonei as putative vector of visceral leishmaniasis in La Banda, Argentina.

    PubMed

    Salomón, Oscar D; Quintana, María G; Bezzi, Gisela; Morán, María L; Betbeder, Eduardo; Valdéz, Daniel V

    2010-01-01

    Four autochthonous cases of human visceral leishmaniasis (VL) were reported in La Banda, Santiago del Estero from June 2007 to May 2008. In the vicinity of these cases there were 3/47 rK39 sero-positive dogs, and another 4 dogs with VL were reported by passive surveillance. The sero-positive dogs and infected humans lived within a 3.1 km radius. Phebotomine sand fly captures were performed twice during November/December 2007 and April 2008. In 20 of the 59 sampled sites in the areas of the human and canine cases (220 night/traps) 151 phlebotomine sand flies were collected and consisted of: Lutzomyia migonei 93%, Lutzomyia cortelezzii 5.6% and Lutzomyia neivai 1.4%. We propose that there was an enzootic cycle of VL with accidental human transmission due to L. migonei and suggest that there be a surveillance of human isolated cases of VL within the L. migonei dispersion area. PMID:19716797

  20. Geophysical characterization of subaerial hydrothermal manifestations in Punta Banda, Baja California, Mexico.

    NASA Astrophysics Data System (ADS)

    Flores-Marquez, L.; Prol-Ledesma, R. M.; Arango, C.; Canet, C.

    2009-04-01

    Important growth of population in Baja California Peninsula has triggered the need for energy and fresh water. The most sustainable possibility for increasing the availability of fresh water is the use of renewable energy sources in desalination plants. The abundance of geothermal manifestations in the peninsula provides a reliable energy source for desalination purposes. Geothermal development of the Baja California Peninsula dates from the 70's, when the Cerro Prieto geothermal field started producing electricity. Two important cities, Tijuana and Ensenada, are located in the north-western area of Baja California. The city of Ensenada has a desalination plant that is due to be replaced and the geothermal resources of the area could be an option for the new desalination plant. Punta Banda, a region near Ensenada, was specially investigated to determine its geothermal potential. Subaerial springs and the submarine vents were sampled and studied in this work, also geological and geochemical studies were performed, moreover geoelectrical surveys were accomplished to characterize the hydrothermal system at depth. Even though saline intrusion is a severe problem in Ensenada (TDS higher than 3000), thermal springs away from the coast and coastal springs have salinities lower than sea water. According to the geoelectrical models obtained from profiles, the inferred conductive features can be related to thermal anomalies. The existence of hot springs located along a trend suggests that the dynamic of the thermal fluid is restricted by secondary faults.

  1. Geoelectrical Characterization of the Punta Banda System: A Possible Structural Control for the Geothermal Anomalies

    NASA Astrophysics Data System (ADS)

    Arango-Galvan, C.; Flores-Marquez, E.; Prol-Ledesma, R.; Working Group, I.

    2007-05-01

    The lack of sufficient drinking water in México has become a very serious problem, especially in the northern desert regions of the country. In order to give a real solution to this phenomenon the IMPULSA research program has been created to develope novel technologies based on desalination of sea and brackish water using renewable sources of energy to face the problem. The Punta Banda geothermal anomaly is located towards the northern part of Baja California Peninsula (Mexico). High water temperatures in some wells along the coast depicted a geothermal anomaly. An audiomagnetotelluric survey was carried out in the area as a preliminary study, both to understand the process generating these anomalous temperatures and to assess its potential exploitation to supply hot water to desalination plants. Among the electromagnetic methods, the audiomagnetotellurics (AMT) method is appropriated for deep groundwater and geothermal studies. The survey consisted of 27 AMT stations covering a 5 km profile along the Agua Blanca Fault. The employed array allowed us to characterize the geoelectrical properties of the main structures up to 500 m depth. Two main geoelectrical zones were identified: 1) a shallow low resistivity media located at the central portion of the profile, coinciding with the Maneadero valley and 2) two high resitivity structures bordering the conductive zone possibly related to NS faulting, already identified by previous geophysical studies. These results suggest that the main geothermal anomalies are controlled by the dominant structural regime in the zone.

  2. Sulu-Celebes-Banda basins: a trapped piece of Cretaceous to Eocene oceanic crust

    SciTech Connect

    McCabe, R.J.; Hilde, T.W.; Cole, J.T.; Sager, W.; Lee, C.S.

    1986-07-01

    The Sulu-Celebes-Banda basin is composed of three poorly understood marginal basins located between northwest Australia and southeast Asia. Recent studies have proposed that these three basins are remnants of once-continuous ocean basin. The on-land geology of this region is complicated. However, numerous stratigraphic and paleomagnetic studies on pre-Oligocene rocks are consistent with the interpretation that older landmasses presently dissecting the basin were translated into their present position during the middle to late Tertiary. Paleomagnetic data from the Philippines suggest that the Philippine arc is a composite of Early Cretaceous to Holocene arcs that were translated clockwise and from the southeast. Paleomagnetic and stratigraphic data from Kalimantan and Sulawesi suggest that these landmasses share a common origin and that Sulawesi was rifted eastward off of Borneo during the late Tertiary. Stratigraphic studies from the Sula microcontinent, Buru, Ceram, and Timor show close correlation to the stratigraphy of northwest Australia or New Guinea. In addition, paleomagnetic studies from Timor suggest that a portion of the island was part of Australia since the early Mesozoic.

  3. Seismicity gaps and the shape of the seismic zone in the Banda Sea region from relocated hypocenters

    NASA Astrophysics Data System (ADS)

    Das, S.

    2004-12-01

    We relocate hypocenters for more than 800 earthquakes deeper than 50 km with mb ≳ 5.0, along the Banda arc, using several thousand handpicked direct, depth, and core-reflected phases, in addition to phases reported by the International Seismological Centre. The seismicity distribution is found to be very nonuniform both along the arc and in depth. Gaps in the relocated hypocenters exist along depth in most places of the arc, with the upper edge of the gaps varying from 100 to 450 km depth and the lower edge varying from 350 to 670 km in different portions of the arc. The seismic zone between 129 and 131°E in the 100-200 km depth range is the widest along the arc both in strike and downdip. This region, near the highest arc curvature, has the highest seismic activity and is the only part of the arc with earthquakes continuously occurring from the surface down to below 600 km. The very deep earthquakes under Sulawesi are shown to be part of the west-southwest dipping Seram slab. In the westernmost part of the Banda arc the slab is under downdip tension in the 50-250 km depth range, while the deepest portion of the slab in this region is under compression. From 128 to 131°E the slab between 100 and 200 km depth is under mainly horizontal compression. Our study supports the "two-slab" model for the Banda arc. The depth of the Wadati-Benioff zone below the volcanoes is ˜60-100 km for the five volcanoes between 128 and 130°E and ˜150 km for the 23 volcanoes between 118 and 124°E.

  4. Subduction of continental lithosphere in the Banda Sea region: Combining evidence from full waveform tomography and isotope ratios

    NASA Astrophysics Data System (ADS)

    Fichtner, Andreas; De Wit, Maarten; van Bergen, Manfred

    2010-09-01

    We provide new insight into the subduction of old continental lithosphere to depths of more than 100 km beneath the Banda arc, based on a spatial correlation of full waveform tomographic images of its lithosphere with He, Pb, Nd and Sr isotope signatures in its arc volcanics. The thickness of the subducted lithosphere of around 200 km coincides with the thickness of Precambrian lithosphere as inferred from surface wave tomography. While the deep subduction of continental material in continent-continent collisions is widely recognised, the analogue process in the arc-continent collision of the Banda region is currently unique. The integrated data suggest that the late Jurassic ocean lithosphere north of the North Australian craton was capable of entraining large volumes of continental lithosphere. The Banda arc example demonstrates that continental lithosphere in arc-continent collisions is not generally preserved, thus increasing the complexity of tectonic reconstructions. In the particular case of Timor, the tomographic images indicate that this island is not located directly above the northern margin of the North Australian craton, and that decoupled oceanic lithosphere must be located at a considerable distance north of Timor, possibly as far north as the northern margin of the volcanically extinct arc sector. The tomographic images combined with isotope data suggest that subduction of the continental lithosphere did not lead to the delamination of its complete crust. A plausible explanation involves delamination within the continental crust, separating upper from lower crustal units. This interpretation is consistent with the existence of a massive accretionary complex on Timor island, with evidence from Pb isotope analysis for lower-crust involvement in arc volcanism; and with the approximate gravitational stability of the subducted lithosphere as inferred from the tomographic images. The subduction of continental lithosphere including crustal material beneath

  5. Ethnobotanical assessment of plant resources of Banda Daud Shah, District Karak, Pakistan

    PubMed Central

    2013-01-01

    Background The Indigenous knowledge of plants is scientifically and culturally very significant. This paper elucidates the empirical findings of an ethnobotanical survey of Banda Daud Shah, District Karak, Pakistan. Methods Data collection was carried out from October 2011 to September 2012. Total twelve survey trips were made, three in each season. About 100 respondents were interviewed; most of them were aged people between 60–70 years. Interviews were conducted using structured questionnaire composed of variety of questions regarding ethnomedicinal uses of plants of the study area. Direct matrix ranking (DMR), informant citations and market survey of multipurpose plants were also carried out. Results The local community was using 58 plant species belonging to 52 genera and 34 families for different purposes. A total of 25 plant species were herbs followed by 18 shrubs. Leaf (45%) was the most commonly used plant part followed by the whole plants (23%). In total, 40 plant species were medicinally used to treat variety of diseases, of which highest number of species being used for gastro-intestinal problems (19 spp.), expectorant (3 spp.) and antipyretic (3 spp.). Beside medicinal values, 25 species were used for fuel and 18 for fodder purposes. Informant consensus showed that gastrointestinal and respiratory infections were ranked highest (FIC = 0.75) among all ailments. According to DMR output, Dalbergia sisso ranked first due to high multipurpose uses among all species and was found most threatened with higher market value. Conclusion The investigated area is rural in nature and the inhabitants are highly dependent on the native plants for their health care needs and other requirements like fuel wood and fodder due to financial constraints and unavailability of resources. Medicinal plants for high ranked diseases may be phtyochemicaly and pharmacologically investigated to prove their efficacy. The local medicinal flora is facing overexploitation

  6. Highly variable structure along the Banda arc imaged by ambient noise tomography

    NASA Astrophysics Data System (ADS)

    Porritt, R. W.; Miller, M. S.; O'Driscoll, L.; Harris, C. W.; Roosmawati, N.

    2015-12-01

    The tectonic configuration of the Banda region in southeast Asia captures the spatial transition from subduction of Indian Ocean lithosphere to subduction and collision of the Australian continental lithosphere beneath the Timor Sea, which can be considered as the temporal transition of the initiation of continental collision. An ongoing broadband seismic deployment funded by NSF is aimed at better understanding the mantle and lithospheric structure in the region and the relationship of the arc-continent collision to orogenesis. Here, we present results from ambient noise tomography in the region utilizing this temporary deployment of 30 broadband instruments and 38 permanent stations in Indonesia and Australia. Despite having only a year of data from the new experiment and about 2.5 years of data in total, we are already able to measure stable dispersion curves for several paths resulting in good recovery for the Savu Sea, Timor Leste, and the Nusa Tenggara Timur (NTT) region of Indonesia. The resulting initial three dimensional shear velocity model indicates significant lateral heterogeneity along the plate boundary. The model contains clear anomalies associated with the subducting oceanic lithosphere, subducted Australian continental lithosphere, and perhaps delaminated oceanic sediments forming the core of the island of Timor. In this initial 3D model, the subducted lithosphere appears to shallow under the islands of Timor and Sumba relative its position beneath to the Savu Sea where oceanic or transitional lithosphere is being subducted. Additionally, a low velocity anomaly associated with the island of Timor from near the surface to ~8 km depth is observed. Under the island of Sumba, a high velocity anomaly is observed between 10 and 20 km depths. These differences may reflect variation in the stage of subduction along strike, compositional variations, or the influences of subducting seamounts such as the Scott Plateau. Finally, we observe localized low

  7. A emissão em 8mm e as bandas de Merrill-Sanford em estrelas carbonadas

    NASA Astrophysics Data System (ADS)

    de Mello, A. B.; Lorenz-Martins, S.

    2003-08-01

    Estrelas carbonadas possuem bandas moleculares em absorção no visível e, no infravermelho (IR) as principais características espectrais se devem a emissão de grãos. Recentemente foi detectada a presença de bandas de SiC2 (Merrill-Sanford, MS) em emissão sendo atribuída à presença de um disco rico em poeira. Neste trabalho analisamos uma amostra de 14 estrelas carbonadas, observadas no telescópio de 1.52 m do ESO em 4 regiões espectrais diferentes, a fim de detectar as bandas de MS em emissão. Nossa amostra é composta de estrelas que apresentam além da emissão em 11.3 mm, outra em 8 mm. Esta última emissão, não usual nestes objetos, tem sido atribuída ou a moléculas de C2H2, ou a um composto sólido ainda indefinido. A detecção de emissões de MS e aquelas no IR, simultaneamente, revelaria um cenário mais complexo que o habitualmente esperado para os ventos destes objetos. No entanto como primeiro resultado, verificamos que as bandas de Merrill-Sanford encontram-se em absorção, não revelando nenhuma conexão com a emissão a 8 mm. Assim, temos duas hipóteses: (a) a emissão a 8 mm se deve à molécula C2H2 ou (b) essa emissão é resultado da emissão térmica de grãos. Testamos a segunda hipótese modelando a amostra com grãos não-homogêneos de SiC e quartzo, o qual emite em aproximadamente 8mm. Este grão seria produzido em uma fase evolutiva anterior a das carbonadas (estrelas S) e por terem uma estrutura cristalina são destruídos apenas na presença de campos de radiação ultravioleta muito intensos. Os modelos para os envoltórios utilizam o método de Monte Carlo para descrever o problema do transporte da radiação. As conclusões deste trabalho são: (1) as bandas de Merrill-Sanford se encontram em absorção, sugerindo um cenário usual para os ventos das estrelas da amostra; (2) neste cenário, a emissão em 8 mm seria resultado de grãos de quartzo com mantos de SiC, indicando que o quartzo poderia sobreviver a fase

  8. Source of 1629 Banda Mega-Thrust Earthquake and Tsunami: Implications for Tsunami Hazard Evaluation in Eastern Indonesia

    NASA Astrophysics Data System (ADS)

    Major, J. R.; Liu, Z.; Harris, R. A.; Fisher, T. L.

    2011-12-01

    Using Dutch records of geophysical events in Indonesia over the past 400 years, and tsunami modeling, we identify tsunami sources that have caused severe devastation in the past and are likely to reoccur in the near future. The earthquake history of Western Indonesia has received much attention since the 2004 Sumatra earthquakes and subsequent events. However, strain rates along a variety of plate boundary segments are just as high in eastern Indonesia where the earthquake history has not been investigated. Due to the rapid population growth in this region it is essential and urgent to evaluate its earthquake and tsunami hazards. Arthur Wichmann's 'Earthquakes of the Indian Archipelago' shows that there were 30 significant earthquakes and 29 tsunami between 1629 to 1877. One of the largest and best documented is the great earthquake and tsunami effecting the Banda islands on 1 August, 1629. It caused severe damage from a 15 m tsunami that arrived at the Banda Islands about a half hour after the earthquake. The earthquake was also recorded 230 km away in Ambon, but no tsunami is mentioned. This event was followed by at least 9 years of aftershocks. The combination of these observations indicates that the earthquake was most likely a mega-thrust event. We use a numerical simulation of the tsunami to locate the potential sources of the 1629 mega-thrust event and evaluate the tsunami hazard in Eastern Indonesia. The numerical simulation was tested to establish the tsunami run-up amplification factor for this region by tsunami simulations of the 1992 Flores Island (Hidayat et al., 1995) and 2006 Java (Katoet al., 2007) earthquake events. The results yield a tsunami run-up amplification factor of 1.5 and 3, respectively. However, the Java earthquake is a unique case of slow rupture that was hardly felt. The fault parameters of recent earthquakes in the Banda region are used for the models. The modeling narrows the possibilities of mega-thrust events the size of the one

  9. Tsunami damage reduction performance of a mangrove forest in Banda Aceh, Indonesia inferred from field data and a numerical model

    NASA Astrophysics Data System (ADS)

    Yanagisawa, H.; Koshimura, S.; Miyagi, T.; Imamura, F.

    2010-06-01

    Since the 26 December 2004 Indian Ocean tsunami, the role of mangrove forests as natural defenses protecting coastal communities from tsunami disaster has been highlighted. However, some mangrove forests were destroyed by that tsunami. They are expected to have lost their protective functions. In this study, we develop a fragility function to assess the mangrove trees' vulnerability, expressed as the damage probability of mangrove trees, based on field surveys and numerical modeling of the 2004 Indian Ocean tsunami in Banda Aceh, Indonesia. Based on the fragility function, we reconstruct a numerical model of tsunami inundation including the performance of mangrove forests in terms of reducing tsunami damage. The model reveals that a 10 year old mangrove forest in a 500 m wide area can reduce a tsunami's hydrodynamic force by approximately 70% for an incident wave of 3.0 m inundation depth and a wave period of 40 min at the shoreline. The model also shows, for a tsunami inundation depth of greater than 4 m, that a 10 year old mangrove forest would be mostly destroyed and that it would lose its force reduction capacity. Moreover, approximately 80% of a 30 year old mangrove forest would survive a 5 m tsunami and absorb 50% of the tsunami's hydrodynamic force.

  10. A study on crustal shear wave splitting in the western part of the Banda arc-continent collision

    NASA Astrophysics Data System (ADS)

    Syuhada, Hananto, Nugroho D.; Puspito, Nanang T.; Anggono, Titi; Yudistira, Tedi

    2016-03-01

    We analyzed shear wave splitting parameters from local shallow (< 30 km) earthquakes recorded at six seismic stations in the western part of the Banda arc-continent collision. We determined fast polarization and delay time for 195 event-stations pairs calculated from good signal-to-noise ratio waveforms. We observed that there is evidence for shear wave splitting at all stations with dominant fast polarization directions oriented about NE-SW, which are parallel to the collision direction of the Australian plate. However, minor fast polarization directions are oriented around NW-SE being perpendicular to the strike of Timor through. Furthermore, the changes in fast azimuths with the earthquake-station back azimuth suggest that the crustal anisotropy in the study area is not uniform. Splitting delay times are within the range of 0.05 s to 0.8 s, with a mean value of 0.29±0.18 s. Major seismic stations exhibit a weak tendency increasing of delay times with increasing hypocentral distance suggesting the main anisotropy contribution of the shallow crust. In addition, these variations in fast azimuths and delay times indicate that the crustal anisotropy in this region might not only be caused by extensive dilatancy anisotropy (EDA), but also by heterogeneity shallow structure such as the presence of foliations in the rock fabric and the fracture zones associated with active faults.

  11. Subducted upper and lower continental crust contributes to magmatism in the collision sector of the Sunda-Banda arc, Indonesia

    NASA Astrophysics Data System (ADS)

    Elburg, M. A.; van Bergen, M. J.; Foden, J. D.

    2004-01-01

    Pb isotopes in igneous rocks from the Banda-Sunda arc show extreme along-arc variations, which correspond to major lithologic changes in crustal components entering the subduction system. An increase in 206Pb/204Pb ratios toward the zone of collision with the Australian continent reflects input of subducted upper-crustal material; maximum values coincide with anomalously radiogenic 3He/4He ratios that have been earlier attributed to the involvement of the continental margin. The collision zone is further characterized by 208Pb/204Pb ratios that are higher for a given 207Pb/204Pb value than observed in the noncollisional sectors, and in the central part of the collision zone, the 206Pb/204Pb ratios are lower than the most radiogenic values in the adjacent areas. We propose that these Pb isotope signatures reflect input of subducted lower crust, mobilized as a result of slab-window formation during arc-continent collision. Variations in Pb isotopes in the collision zone are solely determined by variations in the nature and proportions of different subducted components. The Pb isotope arrays in the noncollision area may be dominated by slab components as well and could reflect mixing between subducted oceanic crust and entrained sediments, rather than between subarc mantle and subducted sediments. Our new interpretation of the Indonesian Pb isotope data does not call for involvement of ocean-island basalt (OIB) type mantle or Australian subcontinental lithospheric mantle, as has been suggested previously.

  12. Evolution of Ataúro Island: Temporal constraints on subduction processes beneath the Wetar zone, Banda Arc

    NASA Astrophysics Data System (ADS)

    Ely, Kim S.; Sandiford, Mike; Hawke, Margaret L.; Phillips, David; Quigley, Mark; Reis, Joao Edmundo dos

    2011-06-01

    Ataúro is a key to understanding the late stage volcanic and subduction history of the Banda Arc to the north of Timor. A volcanic history of bi-modal subaqueous volcanism has been established and new whole rock and trace element geochemical data show two compositional groups, basaltic andesite and dacite-rhyolite. 40Ar/ 39Ar geochronology of hornblende from rhyo-dacitic lavas confirms that volcanism continued until 3.3 Ma. Following the cessation of volcanism, coral reef marine terraces have been uplifted to elevations of 700 m above sea level. Continuity of the terraces at constant elevations around the island reflects regional-scale uplift most likely linked to sublithospheric processes such as slab detachment. Local scale landscape features of the eastern parts of Ataúro are strongly controlled by normal faults. The continuation of arc-related volcanism on Ataúro until at least 3.3 Ma suggests that subduction of Australian lithosphere continued until near this time. This data is consistent with findings from the earthquake record where the extent of the Wetar seismic gap to a depth of 350 km suggests slab breakoff, as a result of collision, commenced at ˜4 Ma, leading to subsequent regional uplift recorded in elevated terraces on Ataúro and neighbouring islands.

  13. The introduced ribbed mussel (Geukensia demissa) in Estero de Punta Banda, Mexico: Interactions with the native cord grass, Spartina foliosa

    USGS Publications Warehouse

    Torchin, M.E.; Hechinger, R.F.; Huspeni, T.C.; Whitney, K.L.; Lafferty, K.D.

    2005-01-01

    Introduced populations of Guekensia demissa occur on the west coast of North America. They have been reported in San Francisco Bay, four southern California wetlands, and in Estero de Punta Banda (EPB), Baja California Norte, Mexico. We randomly sampled benthic invertebrates in four habitat types within EPB: marsh, channel, mudflat and pan. Geukensia demissa was the most abundant bivalve in the wetland at EPB. It was significantly associated with the native cordgrass, Spartina foliosa, and occurred at higher average densities in vegetated marsh sites (24/m2) and Spartina-dominated tidal channels (35/m2), compared to mudflat (0/m2), and pan (0/m 2) sites. We estimated that the total biomass of this invader was over four times that of the next most abundant bivalve, Tagelus spp., in EPB. We examined G. demissa for parasites and found that only a few native parasites colonized this introduced host at very low prevalences and intensities. We performed bird surveys to determine the habitat overlap and potential impact of this mussel on the EPB population of light-footed clapper rails (Rallus longirostrus levipes), an endangered species in the United States. The high abundance of G. demissa in EPB, its presence in clapper rail habitat, and its known effects on salt marsh habitat in it's native range, warrant further investigations of the impact of this invader in EPB and elsewhere. ?? Springer 2005.

  14. New insights into regional tectonics of the Sunda-Banda Arcs region from integrated magnetic and gravity modelling

    NASA Astrophysics Data System (ADS)

    Zubaidah, Teti; Korte, Monika; Mandea, Mioara; Hamoudi, Mohamed

    2014-02-01

    The Lombok Island (Indonesia), situated along the Sunda-Banda Arcs transition region, lies between zones characterized by very large intensity magnetic anomalies. These anomalies have been noted as being part of the eight most important ones seen on the 1st edition of the World Digital Magnetic Anomaly Map. Unfortunately, only marine magnetic data of surroundings are available, and no regional high-resolution magnetic surveys of this island had been done. Since 2004, we have carried out several geomagnetic ground surveys in this region. Here, we present modelling results for a new geological and tectonic interpretation of the magnetic anomalies. The new results confirm the general pattern of contiguous negative-positive anomalies, revealing two active Quaternary normal faults and a magmatic arc related to a subduction region. This outcome agrees with earlier results in surrounding areas obtained by satellite, aeromagnetic, and marine platforms, and provides a more detailed picture of strong anomalies on this island. Considering both magnetic anomalies and gravity models, it is possible to suggest an extension of the Flores Thrust zone (reaching the northwest off the Lombok Island). The Flores Thrust zone may be considered as a mature subduction in the back arc region, showing a tendency of progressive subduction during last decades.

  15. Suture Dynamics of the Banda Arc Collision Zone: Geochemical and Age Analysis of Ultramafic and Mafic Bodies in Timor, Indonesia

    NASA Astrophysics Data System (ADS)

    Valenza, J. M.; Harris, R. A.; Spencer, C. J.; Hoiland, C. W.; Flores, J. A.

    2013-12-01

    New age and geochemical data confirm that most ultramafic bodies on the north coast of Timor are derived from the distal reaches of the Australian continental margin lower plate that was exhumed by extension during Late Paleozoic to Mesozoic rifting. The ultramafic bodies were accreted to Timor during Late Miocene to present arc-continent collision. One of the lherzolitic ultramafic bodies near Caicua was previously unknown, but yields clear isotopic indicators that it is kin to the Hili Manu mafic and ultramafic complex further to the west. Zircon grains from metagabbro of the Hili Manu complex have cores with mostly Early Permian ages and rims of Latest Miocene ages. Isotopic analysis indicates abyssal plain, or passive margin affinity of the Caicua ultramafic body. One important exception to this pattern are mafic and ultramafic bodies associated with the Ocussi volcanics, which yield Miocene and Pliocene ages and supra-subduction zone chemical signatures. The Ocussi body is clearly part of the upper plate of the collision and formed after collision initiated further to the east. It is also structurally higher than the Hili Manu complex and has no affinities with the Australian plate. This study documents that both the upper and lower plates of the active arc-continent collision contribute mafic and ultramafic rocks to the evolving suture zone between the Indo-Australian and Asian plates in the Banda Arc region.

  16. Crustal structure beneath two seismic stations in the Sunda-Banda arc transition zone derived from receiver function analysis

    SciTech Connect

    Syuhada; Hananto, Nugroho D.; Handayani, Lina; Puspito, Nanang T; Yudistira, Tedi; Anggono, Titi

    2015-04-24

    We analyzed receiver functions to estimate the crustal thickness and velocity structure beneath two stations of Geofon (GE) network in the Sunda-Banda arc transition zone. The stations are located in two different tectonic regimes: Sumbawa Island (station PLAI) and Timor Island (station SOEI) representing the oceanic and continental characters, respectively. We analyzed teleseismic events of 80 earthquakes to calculate the receiver functions using the time-domain iterative deconvolution technique. We employed 2D grid search (H-κ) algorithm based on the Moho interaction phases to estimate crustal thickness and Vp/Vs ratio. We also derived the S-wave velocity variation with depth beneath both stations by inverting the receiver functions. We obtained that beneath station PLAI the crustal thickness is about 27.8 km with Vp/Vs ratio 2.01. As station SOEI is covered by very thick low-velocity sediment causing unstable solution for the inversion, we modified the initial velocity model by adding the sediment thickness estimated using high frequency content of receiver functions in H-κ stacking process. We obtained the crustal thickness is about 37 km with VP/Vs ratio 2.2 beneath station SOEI. We suggest that the high Vp/Vs in station PLAI may indicate the presence of fluid ascending from the subducted plate to the volcanic arc, whereas the high Vp/Vs in station SOEI could be due to the presence of sediment and rich mafic composition in the upper crust and possibly related to the serpentinization process in the lower crust. We also suggest that the difference in velocity models and crustal thicknesses between stations PLAI and SOEI are consistent with their contrasting tectonic environments.

  17. Quaternary hinterland evolution of the active Banda Arc: Surface uplift and neotectonic deformation recorded by coral terraces at Kisar, Indonesia

    NASA Astrophysics Data System (ADS)

    Major, Jonathan; Harris, Ron; Chiang, Hong-Wei; Cox, Nicole; Shen, Chuan-Chou; Nelson, Stephen T.; Prasetyadi, Carolus; Rianto, Arif

    2013-09-01

    Coral terrace surveys and U-series ages of coral yield a surface uplift rate of ∼0.5 m/ka for Kisar Island, which is an emergent island in the hinterland of the active Banda arc-continent collision. Based on this rate, Kisar first emerged from the ocean as recently as ∼450 ka. These uplifted terraces are gently warped in a pattern of east-west striking folds. These folds are strike parallel to more developed thrust-related folds of similar wavelength imaged by a seismic reflection profile just offshore. This deformation shows that the emergence of Kisar is influenced by forearc closure along the south-dipping Kisar Thrust. However, the pinnacle shape of Kisar and the protrusion of its metamorphic rocks through the forearc basin sediments also suggest a component of extrusion along shear zones or active doming. Coral encrusts the island coast in many locations over 100 m above sea level. Terrace morphology and coral ages are best explained by recognizing major surfaces as mostly growth terraces and minor terraces as mostly erosional into older terraces. All reliable and referable coral U-series ages determined by MC-ICP-MS correlate with marine isotope stage (MIS) 5e (118-128 ka). The only unaltered coral samples are found below 6 m elevation; however an unaltered Tridacna (giant clam) shell in growth position at 95 m elevation yields a U-series age of 195 ± 31 ka, which corresponds to MIS 7. This age agrees with the best-fit uplift model for the island. Loose deposits of unaltered coral fragments found at elevations between 8 and 20 m yield U-series ages of <100 years and may represent paleotsunami deposits from previously undocumented tectonic activity in the region.

  18. Crustal structure beneath two seismic stations in the Sunda-Banda arc transition zone derived from receiver function analysis

    NASA Astrophysics Data System (ADS)

    Syuhada, Hananto, Nugroho D.; Puspito, Nanang T.; Anggono, Titi; Handayani, Lina; Yudistira, Tedi

    2015-04-01

    We analyzed receiver functions to estimate the crustal thickness and velocity structure beneath two stations of Geofon (GE) network in the Sunda-Banda arc transition zone. The stations are located in two different tectonic regimes: Sumbawa Island (station PLAI) and Timor Island (station SOEI) representing the oceanic and continental characters, respectively. We analyzed teleseismic events of 80 earthquakes to calculate the receiver functions using the time-domain iterative deconvolution technique. We employed 2D grid search (H-κ) algorithm based on the Moho interaction phases to estimate crustal thickness and Vp/Vs ratio. We also derived the S-wave velocity variation with depth beneath both stations by inverting the receiver functions. We obtained that beneath station PLAI the crustal thickness is about 27.8 km with Vp/Vs ratio 2.01. As station SOEI is covered by very thick low-velocity sediment causing unstable solution for the inversion, we modified the initial velocity model by adding the sediment thickness estimated using high frequency content of receiver functions in H-κ stacking process. We obtained the crustal thickness is about 37 km with VP/Vs ratio 2.2 beneath station SOEI. We suggest that the high Vp/Vs in station PLAI may indicate the presence of fluid ascending from the subducted plate to the volcanic arc, whereas the high Vp/Vs in station SOEI could be due to the presence of sediment and rich mafic composition in the upper crust and possibly related to the serpentinization process in the lower crust. We also suggest that the difference in velocity models and crustal thicknesses between stations PLAI and SOEI are consistent with their contrasting tectonic environments.

  19. Mantle Dynamics of Australia-Banda Arc Collision as Inferred from Shear Wave Splitting Analysis of Teleseismic and Local Slab Events

    NASA Astrophysics Data System (ADS)

    Harris, C. W.; Miller, M. S.; O'Driscoll, L.; Porritt, R. W.; Roosmawati, N.; Widiyantoro, S.

    2015-12-01

    Arc-continent collision is an important factor in continent building, orogensis, and ocean closure, yet the details associated with it are not fully understood. East-Timor and the Nusa Tenggara Timur region of Indonesia provide a unique setting to study a young arc-continent collision (~8 Ma) and incipient orogenesis. The NSF funded Banda Arc project affords a rare opportunity to investigate unconstrained processes such as active continental subduction and slab rupture beneath a regional deployment of broadband seismometers. We use data from 35 broadband sensors to analyze seismic anisotropy through measuring shear wave splitting. These stations span the roughly east-west transition from normal oceanic subduction at the Sunda Arc to collision at the Banda Arc, and cross areas associated with back-arc thrusting, arc volcanism, extinct volcanism and a rapidly exhuming forearc. Thirty of the sensors used in the analysis are temporary stations installed by our research team in 2014 and will remain in the field until 2016 or later. The remaining stations are part of the open-access GFZ GEOFON global seismic network. We present preliminary shear wave splitting results for teleseismic (*KS core phases) and local (direct S phase) arrivals in order to inspect the sub-slab mantle and the supra-slab mantle wedge for anisotropic patterns related to olivine flow fabric. These results can be used to assess regional strain linked to ongoing collision and may elucidate any slab tearing that has resulted from the (partial) subduction of buoyant continental material of Australian affinity. Presently, we observe a trend of primarily trench-parallel sub-slab fast polarization directions and perhaps more complicated anisotropy in the mantle wedge. Relative to the trench, there appears to be more spatial variation in fast axis orientation for direct arrivals than teleseismic phases. We discuss how the interpretation of our initial results provides insight into the mantle dynamics of the

  20. Health diplomacy through collaboration and a story of hope in tsunami-ravaged Banda Aceh, Indonesia: A U.S. Public Health Service nurse officer perspective.

    PubMed

    Pryor, Thomas

    2006-10-01

    As a registered nurse, I have witnessed the powerful influence of bedside care for > 10 years. Yet my experience aboard the USNS Mercy--the first interagency deployment designed to provide humanitarian assistance to tsunami-stricken Indonesia--revealed a direct link between individual bedside care and health diplomacy. Despite desperate medical and humanitarian needs in the province of Banda Aceh, the Mercy was met with suspicion and resistance by the Indonesian government. In the first few days, it seemed uncertain that the Mercy would be asked to assist in any humanitarian capacity. The Mercy crew and staff agreed only to assist at the request of the Indonesian government. Ultimately it was the emergent medical needs of a 10-year-old survior, evacuated to the ship by Australian and German organizations, which established the seeds of health diplomacy between the United States and Indonesia. This article explores the ways in which health diplomacy can be fostered by individual medical and nursing care, through the story of one young survivor of the East Asian tsunami. My experience of compassionate and culturally centered care aboard the USNS Mercy touched the hearts and minds of care providers and, ultimately, won the trust of local government officials and the people of Banda Aceh.

  1. Health diplomacy through collaboration and a story of hope in tsunami-ravaged Banda Aceh, Indonesia: A U.S. Public Health Service nurse officer perspective.

    PubMed

    Pryor, Thomas

    2006-10-01

    As a registered nurse, I have witnessed the powerful influence of bedside care for > 10 years. Yet my experience aboard the USNS Mercy--the first interagency deployment designed to provide humanitarian assistance to tsunami-stricken Indonesia--revealed a direct link between individual bedside care and health diplomacy. Despite desperate medical and humanitarian needs in the province of Banda Aceh, the Mercy was met with suspicion and resistance by the Indonesian government. In the first few days, it seemed uncertain that the Mercy would be asked to assist in any humanitarian capacity. The Mercy crew and staff agreed only to assist at the request of the Indonesian government. Ultimately it was the emergent medical needs of a 10-year-old survior, evacuated to the ship by Australian and German organizations, which established the seeds of health diplomacy between the United States and Indonesia. This article explores the ways in which health diplomacy can be fostered by individual medical and nursing care, through the story of one young survivor of the East Asian tsunami. My experience of compassionate and culturally centered care aboard the USNS Mercy touched the hearts and minds of care providers and, ultimately, won the trust of local government officials and the people of Banda Aceh. PMID:17447623

  2. Discontinuous character of the Wadati-Benioff zone in the Banda Arc region: a consequence of a cyclic character of the process of subduction

    NASA Astrophysics Data System (ADS)

    Matejkova, R.; Spicak, A.; Vanek, J.

    2010-12-01

    Our former investigation into heterogeneous distribution of earthquakes at convergent plate margins led us to an idea of discontinuities in the process of subduction (e.g. Hanuš and Vaněk, 1978; Špičák et al., 2007). This idea suggests the existence of subduction cycles lasting several million years. A fade-out of a subduction process should be caused e.g. by a collision of the slab with the 670 boundary, convergence of hardly subductable seamount provinces, collision with a thick continental crust etc. Such a fade-out of subduction may be followed by an onset of a new subduction cycle, with important consequences to, e.g., position of the volcanic arc. In this contribution, we analyse spatial distribution of intermediate-depth and deep earthquakes in the southern part of the Banda Arc region (5°-10°S and 127°-132°E). The EHB global hypocentral determinations (Engdahl et al., 1998) covering the period 1964-2007 have been used. To visualize depth distribution of earthquake foci, we covered the region of interest by narrow (25 km width) swaths, oriented perpendicular to the plate margin, and displayed earthquake foci in vertical sections. The vertical sections show concentration of earthquake foci of the Wadati-Benioff zone (hereafter denoted as WBZ) in four distinct domains that do not fit a continuous plate-like body. These domains can be clearly distinguished from each other by a distinct gap in seismicity between them and/or a noticeable change in dip angle of neighbouring domains. This observation casts doubt on a generally accepted idea that the seismically active domains of the Banda WBZ represent one continuous slab. The deepest domain D1 of earthquakes (400-700 km depth) is probably associated with deep earthquakes north of Java and corresponds to a subduction cycle that faded about 8 Ma ago. Our estimate of the age of the cycle is based on the assumption of a steady convergence rate of about 7 cm/yr. The domain D2 of earthquakes at depths between

  3. Tsunamis as geomorphic crises: Lessons from the December 26, 2004 tsunami in Lhok Nga, West Banda Aceh (Sumatra, Indonesia)

    NASA Astrophysics Data System (ADS)

    Paris, Raphaël; Wassmer, Patrick; Sartohadi, Junun; Lavigne, Franck; Barthomeuf, Benjamin; Desgages, Emilie; Grancher, Delphine; Baumert, Philippe; Vautier, Franck; Brunstein, Daniel; Gomez, Christopher

    2009-03-01

    Large tsunamis are major geomorphic crises, since they imply extensive erosion, sediment transport and deposition in a few minutes and over hundreds of kilometres of coast. Nevertheless, little is known about their geomorphologic imprints. The December 26, 2004 tsunami in Sumatra (Indonesia) was one of the largest and deadliest tsunamis in recorded human history. We present a description of the coastal erosion and boulder deposition induced by the 2004 tsunami in the Lhok Nga Bay, located to the West of Banda Aceh (northwest Sumatra). The geomorphological impact of the tsunami is evidenced by: beach erosion (some beaches have almost disappeared); destruction of sand barriers protecting the lagoons or at river mouths; numerous erosion escarpments typically in the order of 0.5-1.5 m when capped by soil and more than 2 m in dunes; bank erosion in the river beds (the retreat along the main river is in the order of 5-15 m, with local retreats exceeding 30 m); large scars typically 20-50 cm deep on slopes; dislodgement of blocks along fractures and structural ramps on cliffs. The upper limit of erosion appears as a continuous trimline at 20-30 m a.s.l., locally reaching 50 m. The erosional imprints of the tsunami extend to 500 m from the shoreline and exceed 2 km along riverbeds. The overall coastal retreat from Lampuuk to Leupung was 60 m (550,000 m 2) and locally exceeded 150 m. Over 276,000 m 3 of coastal sediments were eroded by the tsunami along the 9.2 km of sandy coast. The mean erosion rate of the beaches was ~ 30 m 3/m of coast and locally exceeded 80 m 3/m. The most eroded coasts were tangent to the tsunami wave train, which was coming from the southwest. The fringing reefs were not efficient in reducing the erosional impact of the tsunami. The 220 boulders measured range from 0.3 to 7.2 m large (typically 0.7-1.5 m), with weights from over 50 kg up to 85 t. We found one boulder, less than 1 m large, at 1 km from the coastline, but all the others were

  4. Geochemistry of quaternary volcanism in the Sunda-Banda arc, Indonesia, and three-component genesis of island-arc basaltic magmas

    NASA Astrophysics Data System (ADS)

    Wheller, G. E.; Varne, R.; Foden, J. D.; Abbott, M. J.

    1987-06-01

    Volcanic rocks of the Sunda and Banda arcs range from tholeiitic through calcalkaline and shoshonitic to leucititic, the widest compositional span of mafic magmatism known from an active arc setting. Mafic rocks in our data set, which includes 315 new analyses of volcanic rocks from twelve Quaternary volcanoes, including Batu Tara in the previously geochemically unknown Flores-Lembata arc sector, are generally similar to those from other island arcs: most contain <1.3 wt. % TiO 2 and 16-22 wt. % Al 2O 3, and have characteristically high K/Nb and La/Nb values. Abundances of P, Ba, Rb, Sr, La, Ce, Nd, Zr and Nb increase sympathetically with increasing K 2O contents of mafic rocks but those of Na, Ti, Y and Sc vary little throughout the geochemical continuum from low-K tholeiitic to high-K leucititic rocks. Excluding Sumatra and Wetar, which possess mainly dacitic and rhyolitic volcanics, the Sunda-Banda arc is divisible into four geochemical arc sectors with boundaries that correlate with major changes in regional tectonic setting and geological history. From west to east, the West Java, Bali and Flores arc sectors each comprise volcanoes which become progressively more K-rich eastwards, culminating in the leucitite volcanoes Muriah, Soromundi and Sangenges, and Batu Tara, respectively. In the most easterly Banda sector, the volcanics vary from high- to low-K eastwards around the arc. Correlations between geochemistry and 87Sr/ 86Sr values show separate trends for each of the four arc sectors, believed to be the result of involvement of at least three geochemically and isotopically distinct components in the source regions of the arc magmatism. A dominant source component with a low K content and a low 87Sr/ 86Sr value, and common to all sectors, is probably peridotitic mantle. A second component, with low K content but high 87Sr/ 86Sr value, appears to be crustal material. This component is most apparent in the Banda sector, in keeping with that sector's tectonic

  5. Effective elastic thickness of the northern Australian continental lithosphere subducting beneath the Banda orogen (Indonesia): inelastic failure at the start of continental subduction

    NASA Astrophysics Data System (ADS)

    Tandon, K.; Lorenzo, J. M.; O'Brien, G. W.

    2000-12-01

    Pliocene-Recent continent-island arc collision of the northern Australian continental lithosphere across the Banda orogen from Roti to the Kai Plateau (˜121-137°E longitude) has formed an underfilled foreland basin within the Timor-Tanimbar-Aru Trough. Continental collision on northern Australian lithosphere is most advanced near central Timor Island in terms of shortening and absorbing the forearc basin (Savu Basin) within the accretionary prism. Australian continental lithosphere north of area around central Timor Island is believed to be detached from the oceanic lithosphere. Effective Elastic Thickness (EET) of the northern Australian continental lithosphere from Roti to the Kai Plateau are derived using an elastic half-beam model. Modeled deflection is matched to the seafloor bathymetry and the marine complete 3D Bouguer gravity anomalies. The EET varies from 27 to 75 km across the northern Australian continental lithosphere from Roti to Kai Plateau when the thickness of the elastic half-beam is kept constant. The highest EET values lies near central Timor. From the shelf to beneath the Banda orogen, the EET of the northern Australian continental lithosphere is reduced from ˜90 to ˜30 km when the thickness of the elastic half-beam is allowed to vary down dip. Elastic half-beam modeling approximates the Banda orogen as a triangular load and hidden subsurface loads as end-point loads. Wider triangular loads modeling the load contribution from Banda orogen need higher values of EET. Such an observation highlights the role of high EET in thin-skinned collisional tectonics by promoting the support of wider accretionary prisms by parts of foreland basins with higher EET. Variations in EET may result from inelastic yielding in the northern Australian continental lithosphere. Oroclinal bending of the Australian continental lithosphere in the east, from Tanimbar to the Kai Plateau, may create additional yielding and further decrease the EET. Change in EET occurred

  6. Progressive Emergence and Warping of Islands in the Active Banda Arc-Continent Collision As Recorded By Uplifted Coral Terraces: Tectonic and Geohazards Implications

    NASA Astrophysics Data System (ADS)

    Harris, R. A.; Cox, N.; Major, J. R.; Merritts, D. J.; Prasetyadi, C.

    2014-12-01

    Uplifted coral terraces throughout the Banda-Sunda Arc transition reveal how strain is distributed over the past thousand to million years in the active arc-continent collision, and are key to identifying hazardous active faults. U-series age analysis of the lowest coral terraces yields surface uplift rates that vary in a non-systematic way along strike from 0.2 to 1.5 mm/a over short wavelengths of a few kms. For example, coral terraces are tilted varying degrees northward in Sumba, SSE in Savu, NNW in Rote and generally south along the north coast of Timor. In all of these cases the tilt is away from zones of active thrusting and folding. In Sumba the forearc is ramping up and over the northern edge of the Scott Plateau along what is likely a north dipping thrust. In Savu the coral terraces rise where the back of the accretionary wedge is ramping up over the forearc basin on the south dipping Savu Thrust. In Rote coral terraces form on the front of the accretionary wedge where it is ramping up over the subducting Australian continental margin. The north coast of East Timor is likely uplifting due to internal thrusting and closure of the Wetar Strait. Localized uplift of circular islands is associated with diapirism. The diapiric island of Kisar is cored by syn-collisional metamorphic rocks. The association of uplift and warping with short wavelength deformational processes argues against the commonly held interpretation that coral terraces in the Banda arc-continent collision manifest the effects of slab tear or some other lithospheric scale process. The pattern of uplift correlates best with proximity to active faults, folds and diapirs. In terms of geohazards, flights of uplifted coral terraces are the smoking gun for sources of large earthquakes and tsunami. Many of the terraces show signs of co-seismic uplift. Tsunami deposits with young corals are found on some of these terraces as high as 20 m above sea level.

  7. Contribution of Anisotropy of Magnetic Susceptibility (AMS) to reconstruct flooding characteristics of a 4220 BP tsunami from a thick unconsolidated structureless deposit (Banda Aceh, Sumatra)

    NASA Astrophysics Data System (ADS)

    Wassmer, Patrick; Gomez, Christopher; Iskandasyah, T. Yan W. M.; Lavigne, Franck; Sartohadi, Junun

    2015-07-01

    One of the main concerns of deciphering tsunami sedimentary records along seashore is to link the emplaced layers with marine high energy events. Based on a combination of morphologic features, sedimentary figures, grain size characteristics, fossils content, microfossils assemblages, geochemical elements, heavy minerals presence; it is, in principle, possible to relate the sedimentary record to a tsunami event. However, experience shows that sometimes, in reason of a lack of any visible sedimentary features, it is hard to decide between a storm and a tsunami origin. To solve this issue, the authors have used the Anisotropy of Magnetic Susceptibility (AMS) to evidence the sediment fabric. The validity of the method for reconstructing flow direction has been proved when applied on sediments in the aftermath of a tsunami event, for which the behaviour was well documented (2004 IOT). We present herein an application of this method for a 56 cm thick paleo-deposit dated 4220 BP laying under the soil covered by the 2004 IOT, SE of Banda Aceh, North Sumatra. We analysed this homogenous deposit, lacking of any visible structure, using methods of classic sedimentology to confirm the occurrence of a high energy event. We then applied AMS technique that allowed the reconstruction of flow characteristics during sediment emplacement. We show that all the sequence was emplaced by uprush phases and that the local topography played a role on the re-orientation of a part of the uprush flow, creating strong reverse current. This particular behaviour was reported by eyewitnesses during the 2004 IOT event.

  8. Desarrollo de un receptor polarimétrico en banda S para aplicación en estudios radioastronómicos

    NASA Astrophysics Data System (ADS)

    Barberis, C. M.; Bava, J. A.; Sanz, A. J.

    Desde el punto de vista tecnológico, el objetivo principal de este proyecto es desarrollar un cabezal de receptor en la frecuencia de 3.3 GHz, con una temperatura del sistema de 60 K y un ancho de banda de 140 MHz. El mismo será instalado en el foco primario de un reflector parabólico de 30 metros de diámetro que funcionará como radiómetro en el IAR. El receptor es del tipo polarimétrico, con lo cual permite la posibilidad de obtener las componentes de polarización lineal y circular. Para tal fin el cabezal constará de dos ramas receptoras que amplificarán la señal y la trasladarán a una frecuencia menor, (frecuencia intermedia), permitiendo de esa forma un mejor transporte de la señal a la sala de control para su posterior procesamiento. El receptor, además de tener características polarimétricas, podrá ser usado en el contínuo y en la línea, utilizando las ventajas observacionales y de procesamiento de señal que actualmente posee el IAR.

  9. A dual doubly vergent orogen in the Banda Arc continent-arc collision zone as observed on deep seismic reflection profiles

    NASA Astrophysics Data System (ADS)

    Snyder, D. B.; Prasetyo, H.; Blundell, D. J.; Pigram, C. J.; Barber, A. J.; Richardson, A.; Tjokosaproetro, S.

    1996-02-01

    New deep seismic reflection profiles across the Banda Arc of Indonesia reveal reflectors in the uppermost 50 km of the lithosphere. Combined with existing earthquake hypocenter locations and focal mechanisms, the new structural geometries inferred from the reflectors yield a more complete analysis of deformation during the past 10 m.y. and provide insights into how strain is partitioned across an orogenic belt in which volcanic arcs and continents converge. A clearly defined Wadati-Benioff zone, and recent deformation of shelf sediments observed on older shallow seismic profiles, indicated to previous workers that substantial convergence occurred at the Timor Trough. A few focal mechanisms, seafloor escarpments, and recent geodetic surveying indicate that convergence at ˜7 cm yr-1 currently (last 200 kyr?) occurs at the northern margin of the now inactive volcanic arc, the Wetar Thrust zone. Reflectors on the new seismic profiles are interpreted as thrust faults and folds that occur throughout the crust and within the uppermost mantle between the Timor Trough and Wetar Thrust. Specifically, basement reflectors beneath the toe of the accretionary complex have reverse-sense offsets that imply blind thrusts. The whole crust is horizontally shortened, not only the sedimentary cover rocks that previously deformed into duplexes above a decollément. Reflectors dipping away from both margins of the forearc basin and at the northern margin of the volcanic arc are interpreted as evidence of thrusting. Thus each arc represents a doubly vergent fold-and-thrust belt, but only the northern one is currently active. Crustal thicknesses inferred from seismic velocities, reflectors, and gravity anomalies are consistent with the merging of a thinned continental shelf margin with oceanic lithosphere to form an orogenic belt with at present 3-4 km of topographic relief in the region of eastern Timor.

  10. Kinematic Analysis of Fold-Thrust-Belt Using Integrated Analogue Sandbox Modeling and 3D Palinspatic Reconstructions in Babar-Selaru Area, Banda Sea Region, Indonesia

    NASA Astrophysics Data System (ADS)

    Sapiie, Benyamin; Hadiana, Meli; Kurniawan, Ade; Daniel, Dicky; Danio, Harya; Fujimoto, Masamichi; Ohara, Michio; Alam Perdana, Lisnanda; Saputra, Afif

    2016-04-01

    Kinematic analysis of Babar-Selaru fold-thrust-belt is challenging and often difficult particularly in conducting seismic interpretation due to complex structural geometries. Resolving such as issue, in this study we proposed to use integrated seismic interpretation, analogue sandbox modeling and 3D palinspatic reconstructions. This paper is presented results of detail kinematic analysis for understanding tectonic evolution as well as mechanism of fold-thrust-belt in relation to their hydrocarbon prospect. Babar-Selaru Area is located within the collisional boundary between Australian continental margin and Banda Arc region of Indonesia. The area is characterized by complex deformation zone of fold-thrust-belt, involving Mesozoic and Tertiary sedimentary sequences of Australian continental margin. The age of deformation is ranging from 8-5 Ma. Seismic interpretations show two styles of faults developed in the area, which are thrust and normal faults system. The last deformation observed in the Babar Selaru area is controlled by south verging imbricated thin-skinned thrust fault system, with the staircase style of fault detachment. Although, both structural styles occurred in separated locations, they are formed not only in the same time but also related in time and space. Total extension is ranging from 1-3 % where average shortening is in the order of 35-38%. Sandbox modeling is an effective way to study and understand the style, pattern and geometry of the deformed sedimentary sequences in the study area. Based on comparison of five settings experiments (mainly different geological boundary condition) with more than 50 different modeling; deformation is particularly controlled by types and thickness of lithology package and detachment geometry. These two parameters were quite sensitive in generating different deformation style and pattern in Babar-Selaru fold-thrust-belt. Therefore, choosing the right combination of stratigraphy model and material setting are

  11. 400 Years of Living Dangerously: Compiling and Communicating to Those in Harms Way the History of Major Earthquake and Tsunami Events in the Sunda-Banda Arc Transition, Eastern Indonesia Region.

    NASA Astrophysics Data System (ADS)

    Harris, R. A.; Major, J. R.; Dunn, R.; Prasetyadi, C.; Ibadurrahman, H.; Cox, N.; Roosmawati, N.; Nugroho, H.; Klein, T.

    2014-12-01

    Historical records as far back as 1600 document 79 damaging earthquakes and 50 tsunamis in the E. Sunda-Banda Arc transition. One of the largest events in 1629 generated a tsunami that reached a height of >16 m. Another event in 1674 caused a submarine landslide that produced a tsunami >100 m based on the vegetation trim line. An earthquake storm struck the region between 1814 and 1857. During this time there were two mega-earthquakes (1820 and 1852) felt throughout most of Indonesia, which generated tsunamis as high as 26 m. Tsunamis also occurred from earthquakes in 1814, 1818, 1836 and 1857, and the eruption of Tambora (1815). This eruption is the one of the most notable extreme historical geohazards not only in the Indonesian region, but globally. The earthquake storm ended with an event along the north coast of East Timor in 1857, which caused a 3 m tsunami that inundated the capital city of Dili and flooded many villages. Tsunamigenic earthquakes have also struck the area around Kupang, West Timor, which is one of the main commercial centers of the region with a population of half a million. The population of the region is now at least 10 million. Another 2 million people live along the coast of the Makassar Strait, which has experienced 18 tsunamis since the 1820 earthquake. Most people now live in cities, most cities have unreinforced masonry construction and some are in historical tsunami inundation zones. Cities along the NW coast of Australia are also at risk of a tsunami from mega-thrust earthquakes along parts of the Timor Trough, which accumulates strain at the rate of 22 mm/a. No major earthquakes are documented along the Timor to Tanimbar part of the plate boundary since historical records have been kept. However, a major mega-thrust earthquake (8.5-9.0) occurred along the Tanimbar trough in 1852, which caused an 8 m tsunami. We have modeled both the 1629 and 1852 mega-thrust events and used these data to map inundation zones for coastal communities

  12. El rol de Ia colaboracion y el Modelo de Aprendizaje Basado en Proyectos (ABPr) mediante el lente de la Teoria de Actividad (CHAT): un estudio de caso con estudiantes de 9no grado

    NASA Astrophysics Data System (ADS)

    Delgado, Isabel C.

    Los modelos de eensenanza y aprendizaje constructivistas conceptualizan el aprendizaje como un proceso activo. El modelo de Aprendizaje Basado en Proyectos (ABPr) se distingue por una serie de componentes, entre los cuales se destaca el aspecto colaborativo y cooperativo como un reto al momento de su implantacion. Son pocas las investigaciones que se concentran en este aspecto del modelo. En este estudio, se analizaron las diversas interacciones que surgen durante la implantacion de una unidad curricular sobre el tema de Geologia de Puerto Rico, la cual se diseno con el modelo ABPr cuyo enfoque es orientacion a proyectos. Particularmente, se examinaron las interacciones sociales que surgen entre los pares y entre pares y docente durante el proceso de planificacion y desarrollo de los productos finales, al igual que las interacciones entre los estudiantes y el material didactico en estas etapas del modelo. La investigacion es de tipo cualitativo e incorpora como diseno el estudio de caso. Las diversas interacciones constituyen la unidad de analisis. En el estudio participaron 19 estudiantes de 9no grado, a quienes se organizaron en 5 grupos colaborativos por temas de interes (Pangea, Placas tectonicas, Volcanes, Tsunamis y Terremotos). Las tecnicas que se utilizaron para recopilar los datos fueron: observaciones participativas, grupos focales y analisis de documentos (cuadernos reflexivos y respuestas de los estudiantes a la pregunta central del proyecto). Para el analisis de los datos se aplico la teoria de actividad (CHAT) que concentra la unidad de analisis en la actividad humana en un contexto particular. Los resultados del estudio senalan que las interacciones entre pares, entre pares y docente, asi como entre estudiantes y material didactico son fundamentales en el proceso de aprendizaje. Una mayor interaccion entre pares durante las etapas de planificar y desarrollar los productos finales de la unidad, promueve una mejor comprension de los conceptos de la

  13. April 2012 intra-oceanic seismicity off Sumatra boosted by the Banda-Aceh megathrust.

    PubMed

    Delescluse, Matthias; Chamot-Rooke, Nicolas; Cattin, Rodolphe; Fleitout, Luce; Trubienko, Olga; Vigny, Christophe

    2012-10-11

    Large earthquakes nucleate at tectonic plate boundaries, and their occurrence within a plate's interior remains rare and poorly documented, especially offshore. The two large earthquakes that struck the northeastern Indian Ocean on 11 April 2012 are an exception: they are the largest strike-slip events reported in historical times and triggered large aftershocks worldwide. Yet they occurred within an intra-oceanic setting along the fossil fabric of the extinct Wharton basin, rather than on a discrete plate boundary. Here we show that the 11 April 2012 twin earthquakes are part of a continuing boost of the intraplate deformation between India and Australia that followed the Aceh 2004 and Nias 2005 megathrust earthquakes, subsequent to a stress transfer process recognized at other subduction zones. Using Coulomb stress change calculations, we show that the coseismic slips of the Aceh and Nias earthquakes can promote oceanic left-lateral strike-slip earthquakes on pre-existing meridian-aligned fault planes. We further show that persistent viscous relaxation in the asthenospheric mantle several years after the Aceh megathrust explains the time lag between the 2004 megathrust and the 2012 intraplate events. On a short timescale, the 2012 events provide new evidence for the interplay between megathrusts at the subduction interface and intraplate deformation offshore. On a longer geological timescale, the Australian plate, driven by slab-pull forces at the Sunda trench, is detaching from the Indian plate, which is subjected to resisting forces at the Himalayan front.

  14. A three-dimensional model of the seismicity in the banda sea region

    NASA Astrophysics Data System (ADS)

    Papp, Z.

    1980-10-01

    Using the data of all registered tectonic earthquakes (independently from their magnitude) which occurred from 1st January 1918 to 31st December 1965, between 120° and 134°E and 2° and 10° S, a three-dimensional model of hypocenters and tectonic flux was constructed using a basic map and strong wires with small pearls on their tops. The pearls represent the earthquake foci while the length of the wires is proportional to the focal depth. The horizontal and vertical dimensions are equal in the model. More exact gross configurations, and consequently the main deformations of the descending slabs, were estimated by the spatial model of the inclined seismic zones (Benioff zones), provided that intermediate and deep shocks occur within the descending (oceanic) lithosphere. The spatial distribution of the tectonic flux in the period investigated, was illustrated by a series of maps (8 charts altogether), representing the tectonic flux distribution at different depths below the area considered. It was found that the most active center of the tectonic flux is related to the western margin of the Weber Basin, indicating that the deformations of the lithosphere are strongest here. The distribution of seismic energy according to the focal depth on the basis of a total of 181 shocks was also investigated. Its characteristics correspond to the pattern known to exist at and underneath typical island arcs, with an outstanding maximum between 0 and 70 km. A secondary maximum was found between 141 and 210 km. This paper is a contribution to the program of Working Group 1, Geodynamics of the Western Pacific—Indonesian Region, of the Inter-Union Commission on Geodynamics.

  15. April 2012 intra-oceanic seismicity off Sumatra boosted by the Banda-Aceh megathrust.

    PubMed

    Delescluse, Matthias; Chamot-Rooke, Nicolas; Cattin, Rodolphe; Fleitout, Luce; Trubienko, Olga; Vigny, Christophe

    2012-10-11

    Large earthquakes nucleate at tectonic plate boundaries, and their occurrence within a plate's interior remains rare and poorly documented, especially offshore. The two large earthquakes that struck the northeastern Indian Ocean on 11 April 2012 are an exception: they are the largest strike-slip events reported in historical times and triggered large aftershocks worldwide. Yet they occurred within an intra-oceanic setting along the fossil fabric of the extinct Wharton basin, rather than on a discrete plate boundary. Here we show that the 11 April 2012 twin earthquakes are part of a continuing boost of the intraplate deformation between India and Australia that followed the Aceh 2004 and Nias 2005 megathrust earthquakes, subsequent to a stress transfer process recognized at other subduction zones. Using Coulomb stress change calculations, we show that the coseismic slips of the Aceh and Nias earthquakes can promote oceanic left-lateral strike-slip earthquakes on pre-existing meridian-aligned fault planes. We further show that persistent viscous relaxation in the asthenospheric mantle several years after the Aceh megathrust explains the time lag between the 2004 megathrust and the 2012 intraplate events. On a short timescale, the 2012 events provide new evidence for the interplay between megathrusts at the subduction interface and intraplate deformation offshore. On a longer geological timescale, the Australian plate, driven by slab-pull forces at the Sunda trench, is detaching from the Indian plate, which is subjected to resisting forces at the Himalayan front. PMID:23023134

  16. Out of Disaster Comes Opportunity: Initial Lessons from Teacher Mentoring in Banda Aceh, Indonesia

    ERIC Educational Resources Information Center

    Lesnick, Joy; Schultz, Katherine

    2006-01-01

    On December 26, 2004, a 9.0 magnitude earthquake--the most powerful in more than 40 years--struck deep under the Indian Ocean. It was centered about 100 miles southwest off the coast of Aceh, Indonesia, and triggered massive tsunamis across the coasts of Asia and Africa. In Aceh province, located at the northwest tip of the island of Sumatra in…

  17. 78 FR 17600 - Banda de Lupinus albus doce (BLAD); Exemption From the Requirement of a Tolerance

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-03-22

    ... mutagen, and is not a developmental toxicant. There are no known effects on endocrine systems via oral... Classification System (NAICS) codes is not intended to be exhaustive, but rather provides a guide to help readers... Findings In the Federal Register of March 14, 2012 (77 FR 15012) (FRL-9335- 9), EPA issued a...

  18. Amplificadores en bandas para receptores de uso radioastronómicos

    NASA Astrophysics Data System (ADS)

    Bava, A. J.; Sanz, A. J.

    Está en curso de realización en el IAR un cabezal de receptor, en la frecuencia de 3.3 GHz. Este receptor, conjuntamente con los sistemas de procesamientos actuales del IAR y con los futuros proyectos de procesamientos, permitirán las observaciones de las líneas de la molécula de CH, de gran interés astrofísico, y las observaciones en el continuo que complementarán las realizadas en 1420 MHz. En este trabajo, se presentan el diseño de los amplificadores de bajo ruido, que van a conformar las primeras etapas del receptor de 3.3 GHz. El desarrollo de los mismos se realizó teniendo en cuenta que la temperatura del sistema, según consideraciones observacionales, deberá ser de 60oK. Por tal motivo se realizó un diseño de bajo ruido utilizando como elemento activo un HEMT. Tanto los métodos de diseño, como el circuito final, fueron realizados y comprobados con programas de simulación, permitiendo de esta forma obtener el amplificador deseado.

  19. Crustal strain partitioning and the associated earthquake hazard in the eastern Sunda-Banda Arc

    NASA Astrophysics Data System (ADS)

    Koulali, A.; Susilo, S.; McClusky, S.; Meilano, I.; Cummins, P.; Tregoning, P.; Lister, G.; Efendi, J.; Syafi'i, M. A.

    2016-03-01

    We use Global Positioning System (GPS) measurements of surface deformation to show that the convergence between the Australian Plate and Sunda Block in eastern Indonesia is partitioned between the megathrust and a continuous zone of back-arc thrusting extending 2000 km from east Java to north of Timor. Although deformation in this back-arc region has been reported previously, its extent and the mechanism of convergence partitioning have hitherto been conjectural. GPS observations establish that partitioning occurs via a combination of anticlockwise rotation of an arc segment called the Sumba Block, and left-lateral movement along a major NE-SW strike-slip fault west of Timor. We also identify a westward extension of the back-arc thrust for 300 km onshore into East Java, accommodating slip of ˜6 mm/yr. These results highlight a major new seismic threat for East Java and draw attention to the pronounced seismic and tsunami threat to Bali, Lombok, Nusa Tenggara, and other coasts along the Flores Sea.

  20. [The levels of bone mineralization are influenced by body composition in children and adolescents].

    PubMed

    Correa Rodríguez, Maria; Rueda Medina, Blanca; González Jiménez, Emilio; Navarro Pérez, Carmen Flores; Schmidt-RioValle, Jacqueline

    2014-10-01

    Introducción: Existe controversia acerca del efecto del sobrepeso y la obesidad en la mineralización ósea en la adolescencia. Objetivo: El objetivo de este estudio fue valorar el nivel de densidad mineral ósea (DMO) en una población de adolescentes y estudiar su relación con la composición corporal. Material y método: La población de estudio estuvo constituida por 157 adolescentes (93 mujeres y 64 varones) de la provincia de Granada (España). La edad media fue de 14,22 ± 1,41 años. Se valoró la DMO mediante osteosonografía del calcáneo. Los parámetros densitométricos fueron: coeficiente de atenuación de banda ancha (BUA), T-score yZ-score. La composición corporal se determinó con bioimpedanciómetro. Resultados: Los sujetos con obesidad y sobrepeso presentaron valores mayores en el BUA frente a los sujetos con normopeso (95,4± 17,77 y 90,0±1,08 vs. 81,1±17,79) encontrándose diferencias significativas (p.

  1. Curva de rotación de la Galaxia Eso 321-25

    NASA Astrophysics Data System (ADS)

    Díaz, R.; Carranza, G.; Ahumada, J.; Arreguine, V.

    Se presenta la curva de rotación de esta galaxia, generada a partir de espectros obtenidos con el Espectrógrafo Multifunción del telescopio de 1.54 m de Bosque Alegre. El análisis de las curvas de velocidad radial obtenidas muestra que el núcleo no coincide con el centro de simetría de las mismas, lo que es consistente con el aspecto morfológico exhibido por la galaxia en imágenes de banda ancha. En estas últimas, el núcleo muestra una estructura peculiar y no coincidiría con el centro geométrico del disco aparente. Los flujos relativos de líneas (Hα /[NII]λ 6583 y [SII]λ 6731/λ 6716) indicarían niveles de excitación y densidad electrónica normales en regiones HII, aún en la zona nuclear. Este trabajo forma parte de un programa de estudio de cinemática, excitación y densidad electrónica del gas ionizado en galaxias peculiares del Atlas de Galaxias Australes de Sérsic.

  2. The Mexico City--Los Angeles Cultural Mosh Pits: Maldita Vecindad, a Chilanga-Chicana Rock Banda de Pueblo

    ERIC Educational Resources Information Center

    Calderon, Hector

    2006-01-01

    This essay chronicles the career of pioneering Mexican rock band Maldita Vecindad y los Hijos del 5 [degree] Patio. I argue that in a post-Chicano movement period, Maldita has become a borderless cultural institution influencing a generation of Mexicans on both sides of the border. Maldita has sought linkages with Mexicans from north and south…

  3. The Application of Portfolios to Assess Progress in Writing of EFL Students at Secondary Schools in Banda Aceh

    ERIC Educational Resources Information Center

    Eridafithri

    2015-01-01

    Portfolios are one of the alternatives that can be used for writing assessment. Portfolios are not common in the curriculum. The lack of dissemination to language teachers have made portfolios disregarded. In order to encourage teachers to use portfolios for assessment of writing, they need to have adequate information about portfolios, how they…

  4. Estudios de clima espacial basados en observaciones solares históricas: recientes progresos y perspectivas

    NASA Astrophysics Data System (ADS)

    Vaquero, J. M.

    During the last decades, an effort has been made to improve the sunspot number time-series, one of the more useful data set for space climate stud- ies, using historical solar observations. Moreover, not only the sunspot number can be studied using these early solar records. During the last years, historical sources (i.e., sunspot drawings and solar radius measurements) have been also used to study the space climate. Here, I review some recent progress on these issues. In a hand, there are some periods with very few sunspot records and sunspot numbers are not so reliable in these intervals. I discuss the quality of sunspot records during these interesting periods: (a) 1610-1645, (b) 1721-1761, and (c) 1779-1795. On the other hand, I dis- cuss the reliability of early sunspot drawings, sunspot position data, and solar diameter determinations to study long-term variations in our Sun. Fi- nally, some information on historical documents from Argentina and Chile related with space climate are summarised. FULL TEXT IN SPANISH

  5. Caracterizacion y optimizacion electroquimica de dispositivos electrocromicos duales basados en polimeros conductores

    NASA Astrophysics Data System (ADS)

    Padilla Martinez, Javier

    The aim of this thesis is to emphasize the existing relations between electrochemical processes, or electrochemical magnitudes, and colour changes. The work is focused on two aspects: individual spectroelectrochemical characterization of the constituent materials followed by an electrochemical and optical study of the performance of the dual system constructed with those materials. The objective is the optimization of both electrochemical and optical processes in dual conducting polymer systems, obtaining experimental methodologies able to characterize, predict, and finally design optimal dual electrochromic devices. The first part of the study is focused on the development of the proper methodology to obtain an optical characterization of any electrochromic material as a function of its electrochemical properties. Materials used were poly((3,4-ethylenedioxy)thiophene) (PEDOT) and poly-(3,6-bis(2-(3,4-ethylenedioxy)thienyl)-N-methylcarbazole) (PBEDOT-NMCz). PEDOT films are coloured under reduction, while PBEDOT-NMCz are coloured under oxidation, showing complementary colouration, and so they can be used to construct a dual electrochromic device. Based on the obtained experimental results, a theoretical study was undertaken to establish the optical responses of a system comprising several electrochromic layers. The theoretically obtained relations were experimentally proved. Relations obtained allow the prediction of the maximum contrast configuration for a dual system, as a function of the individual electrochemical properties of each constituent material. The system studied was PEDOT/PBEDOT-NMCz. The third chapter deals with the proposal and development of a new experimental methodology able to register the individual oxidation states of each electrode during operation of a dual device, obtaining then direct information about device performance. This methodology allows the study of the influence of different physical and chemical variables, like ratio of redox charge between both constituent films, applied potential to the device and initial oxidation state of the constituent polymer films, on the device performance. The final objective of this work is the construction of electrochromic devices that can be use in real applications out of research or academic contexts. It is necessary then, for safety purposes, to use solid electrolytes in the cell. For final applications it is also required to construct devices of appropriate dimensions. In the fourth chapter, the construction and study of large dimensions and solid state devices for the system PEDOT/PBEDOT-NMCz was carried out. The information obtained in previous sections was used to determine maximum contrast combinations. Problems related to electrodeposition of conducting polymers on large surfaces (around 30 cm2) are discussed, together with the optimization of switching speeds when a solid electrolyte is used. Finally the ability to tune colour states and retain them in the absence of an external potential applied was studied and discussed. The last section deals with the study of two new cathodically colouring polymers, poly(3-(Biphenyl-4-ylmethoxymethyl)-3,4-dihydro-2H-thieno(3,4-b)-(1,2)dioxepine) (BPMOM-ProDOT) and poly-dibenzylProDOT (PDiBz-ProDOT), which have been reported to show larger contrasts than PEDOT. For this reason, dual cells were constructed and checked by combination of these two polymers with PBEDOT-NMCz. The methodology previously developed and used to characterize PEDOT and PBEDOT-NMCz was applied to these polymers. The developed theoretical equations were used to determine the maximum contrast for both systems. Finally, the use of standard optical magnitudes as photopic values is emphasized. Photopic values are standardized by the Commission Internationale de l'Eclairage (CIE), and correspond to real sensations perceived by the human eye, whose sensitivity is different for each wavelength. In this sense the use of photopic values, instead of values corresponding to a single wavelength, is encouraged. (Abstract shortened by UMI.)

  6. Provenance of Permian-Triassic Gondwana Sequence Units Accreted to the Banda Arc: Constraints from U/Pb and Hf Analysis of Zircons and Igneous Geochemistry

    NASA Astrophysics Data System (ADS)

    Flores, J. A.; Spencer, C. J.; Harris, R. A.; Hoiland, C.

    2011-12-01

    Analysis of zircons from Australian affinity Permo-Triassic units of the Timor region yield age distributions with large peaks at 230-400 Ma and 1750-1900 Ma (n=435). Similar zircon age peaks are also found in rocks from NE Australia and the eastern Cimmerian block. It is likely that these terranes, which are now widely separated, were once part of the northern edge of Gondwana near what is now the NW margin of Australia. The Cimmerian Block was removed from Gondwana during Early Permian rifting and initiation of the Neo-Tethys Ocean. Hf analysis of zircon from the Aileu Complex in Timor and Kisar shows bimodal (juvenial and evolved) magmatism in the Gondwana Sequence of NW Australia at ~300 Ma. The magmatic event produced basalt with rift valley and ocean floor geochemical affinities, and rhyolite. Similar rock types and isotopic signatures are also found in Permo-Triassic igneous units throughout the Cimmerian continental block. The part of the Cimmerian Block with zircon distributions most like the Gondwana Sequence of NW Australia is the terranes of northern Tibet and Malaysia. The large 1750-1900 Ma zircon peak is much more wide spread, and appears in terranes from Baoshan (SW China) to Borneo. The Permo-Triassic rocks of the Timor region fill syn-rift intracratonic basins that successfully rifted in the Jurassic to form the NW margin of Australia. This passive continental margin first entered the Sunda Trench in the Timor region at around 8 Ma causing the Permo-Triassic rocks to accrete to the edge of the Asian Plate and emerge as a series of mountainous islands in the young collision zone. Eventually, the Australian continental margin will collide with the southern edge of the Asian plate and these Gondwana terranes will rejoin. However, it may be difficult to reconstruct the various ventures of they made over the past 300 Ma.

  7. Aportes del Aprendizaje Basado en Problemas (ABP) en la ensenanza de la Fisiologia Animal en un programa de Zootecnia

    NASA Astrophysics Data System (ADS)

    Reinartz-Estrada, Monica

    Based on difficulties observed on the subject of technical-scientific conceptualization and the integration of theory and practice in learning animal physiology for students in the Animal Science program at the National University of Colombia in Medellin, this research paper proposes a problem-based learning strategy founded on the method of Problem Based Learning (PBL), applied specifically to the issues of thermoregulation and physiological stress in domestic animals. In this case study, a sample size of eight students was presented with a pedagogical problem during the first session that would then be solved during the course. In order to evaluate the process, three surveys were conducted called Level Test Formulations (NF) performed at different times of the trial: one before beginning the topic (NF 1), one after three theoretical classes had been given and before beginning the fieldwork (NF 2), and another one after the end of the process (NF 3). Finally, individual interviews were conducted with each student to know the students' perceptions regarding the method. The information obtained was subjected to a qualitative analysis and categorization, using the QDA Miner program which reviewed and coded texts from the surveys and individual interviews, supplemented in turn, by field observation, analyzing the conceptual change, the theory-practice relationship and the correlation between the variables and categories established. Among the main results obtained, it should be noted that following the implementation of PBL in this Animal Physiology course, support for conceptual change was demonstrated and the formulated problem served as a connector between theory and practice. Moreover, there was a fusion of prior knowledge with newly acquired knowledge, meaningful learning, improvement in the level of conceptualization and an increase in the scientificness of definitions; it also led to problem-solving and overcoming epistemological obstacles such as multidisciplinarity and nonlinearity. As a result of this research, it is recommended that this method be evaluated in other topics related to Animal Physiology, in other sciences, in larger sample sizes, as well as to address the issue of evaluation applied directly to this method. Key words: Problem Based Learning (PBL), conceptual change, integration of theory and practice, significatif learning, animal physiology, thermoregulation, physiological stress.

  8. Caracterización del entorno del los blazares PG1553+113 y 3C66A con datos GEMINI-GMOS en las bandas g' e i'

    NASA Astrophysics Data System (ADS)

    Torres Zafra, J.; Cellone, S. A.; Andruchow, I.

    The blazars PG1553+113 and 3C66A have been recently detected at TeV energies -rays; however; an accurate modelling of their electromagnetic emission as well as -ray absorption by the extragalactic background light (EBL) are prevented by their lack of firm redshift determinations. This is due to the fact that; being objects of the BLLac subclass; their optical spectral have by definition very faint emission lines. In this paper the environment of both objects is photometrically analyzed; looking for overdensities that may trace galaxy clusters. Comparing magnitudes and colors of detected object to those of model galaxies allows us to provide a new constraint to the redshifts of both blazars. FULL TEXT IN SPANISH

  9. Descentralizacion de la educacion: Financiamiento basado en la demanda. Tendencias del Desarrollo. (Decentralization of Education: Demand-Side Financing. Directions in Development.)

    ERIC Educational Resources Information Center

    Patrinos, Harry Anthony; Ariasingam, David Lakshmanan

    Central government's supply-side expansions of schooling have not equally benefited all members of society, especially girls, indigenous peoples, tribal groups, disadvantaged minorities, and the poor. Public spending on education is often inefficient, higher education is subsidized at primary education's expense, and costs are becoming…

  10. Resumen cronoestratigráfico de las rocas ígneas de Costa Rica basado en dataciones radiométricas

    NASA Astrophysics Data System (ADS)

    Alvarado, G. E.; Kussmaul, S.; Chiesa, S.; Gillot, P.-Y.; Appel, H.; Wörner, G.; Rundle, C.

    1992-10-01

    Based on a recompilation of about 160 K-Ar and U-Th analyses of igneous rocks and their stratigraphic relationships, a synthesis of the magmatic evolution of Costa Rica is presented. The igneous rocks of Jurassic to Oligocene age belong principally to the tholeiitic series. Widespread calc-alkaline volcanism started in the late Miocene and culminated during the Pleistocene in the northern and central part of Costa Rica with the eruption of large volumes of andesitic to rhyolitic ignimbrites and the development of the stratovolcanoes of the Cordillera de Guanacaste and Cordillera Central; some of these volcanoes are still active. Alkaline rocks are subordinate and concentrated on the Caribbean side of Costa Rica. Plutonic intrusions, mainly of late Miocene age, are frequent in the southern part of Costa Rica. The histogram of the available data indicates some periods of more intensive volcanic activity.

  11. Grecia: Nivel IV. Basado en el curso de estudios sociales de Montgomery County Public Schools. (Greece. Level 6. Based on the Montgomery County Public Schools Social Studies Program).

    ERIC Educational Resources Information Center

    Maldonado, Marisol

    This curriculum unit, developed by the Montgomery County Public Schools, Maryland, was designed for use in an elementary level foreign language immersion program. It is geared toward the sixth grade social studies classroom. The unit includes instructional and performance objectives, necessary vocabulary lists, optional language structure…

  12. The Education of the Active Televiewer of School Age.

    ERIC Educational Resources Information Center

    Munoz, Patricio Calderon; Torres, Miguel Reyes

    In response to a series of problem symptoms related to the influence of television on students, a team of professors at the Universidad de Playa Ancha de Ciencias de la Educacion in Chile undertook a project designed to train television viewers to become critical viewers of the medium. Specific objectives of the project included: (1) to design a…

  13. [Theta/beta ratio (NEBA) in the diagnosis of attention deficit hyperactivity disorder].

    PubMed

    Delgado-Mejía, Iván D; Palencia-Avendaño, M Luisa; Mogollón-Rincón, Carolina; Etchepareborda, Máximo C

    2014-02-24

    Introduccion. En julio del año 2013, la Food and Drug Administration estadounidense aprobo el NEBA como el primer dispositivo para la evaluacion complementaria del trastorno por deficit de atencion/hiperactividad (TDAH), basado en el electroencefalograma cuantificado (EEGq) e incluyendo la relacion theta/beta estandarizada, cuyos resultados fueron consistentes con la evaluacion clinica, tanto medica como psicologica, y es una herramienta util para determinar si el TDAH es primario, secundario o comorbido a otro trastorno. Sin embargo, ninguna de las publicaciones, hasta la fecha, especifica si se trata de un cociente theta/beta total, o theta/beta-1 y theta/beta-2, como tampoco se aportan datos para discriminar entre subtipos diagnosticos del TDAH. Objetivo. Cuantificar los cocientes theta/beta, a traves del EEGq, en una muestra de pacientes rioplatenses con diagnostico principal confirmado de TDAH, para comparar el patron neurofisiologico segun el subtipo diagnostico. Pacientes y metodos. Muestra aleatoria estratificada de 62 sujetos de ambos sexos, de 8 a 17 años, distribuidos en dos grupos segun subtipo diagnostico, TDAH subtipo deficit de atencion (n = 31) y TDAH subtipo combinado (n = 31). Resultados. Se confirman cocientes altos theta/beta-1 y theta/beta-2 en la region Cz, mayores a los cocientes en las areas C3 y C4. Se encontraron diferencias moderadas y estadisticamente significativas entre los dos subtipos solo en la banda beta-1 en las regiones occipitales. El analisis de la coherencia interhemisferica sugiere una asociacion del pico de potencia cruzada con el subtipo diagnostico, que para el subtipo combinado es el pico mas rapido (10 Hz). No se encuentran diferencias importantes al analizar los espectros de fase, ni los cocientes theta/alfa. Conclusiones. Si bien la bibliografia cientifica, especificamente el sistema NEBA, plantea la importancia del cociente theta/beta en el diagnostico diferencial del TDAH de muestras controles y otros trastornos

  14. La Materia. Nivel II. Basado en el curso de estudios de Ciencia de Montgomery County Public Schools. (Matter. Level II. Based on the Montgomery County Public Schools Science Studies Program).

    ERIC Educational Resources Information Center

    Gerstman, M. Linda

    This curriculum unit is for use in an elementary school foreign language immersion program in Montgomery County, Maryland. The unit is geared toward the second grade science classroom. It includes instructional and performance objectives, vocabulary lists, optional language structure sections, illustrations, activities, evaluation suggestions, and…

  15. Seres Vivos. Nivel I. Basado en el curso de estudios de Ciencia de Montgomery County Public Schools. (Living Beings. Level 1. Based on the Montgomery County Public Schools Science Studies Program).

    ERIC Educational Resources Information Center

    Senger, Graciela

    This curriculum unit, developed by the Montgomery County Public Schools, Maryland, was designed for use in the elementary level foreign language immersion program. It is geared toward the first grade science classroom. The unit includes instructional and performance objectives, necessary vocabulary lists, optional language structure sections,…

  16. Enacting a People-Centred Curriculum in ELT with Teenage Learners (La vivencia de un currículo basado en los actores de la clase de inglés con adolescentes)

    ERIC Educational Resources Information Center

    Banegas, Darío Luis; Velázquez, Aurelia

    2014-01-01

    In this paper we reflect on the extent to which the learner-centred curriculum in English language teaching includes teachers and learners. We briefly describe the top-down nature of curriculum development in Argentina, then describe and discuss personal and collaborative explorations based on our identities as teachers of English in secondary…

  17. Task-Based Language Learning: Old Approach, New Style. A New Lesson to Learn (Aprendizaje basado en tareas: un antiguo enfoque, un nuevo estilo. Una nueva lección para aprender)

    ERIC Educational Resources Information Center

    Rodríguez-Bonces, Mónica; Rodríguez-Bonces, Jeisson

    2010-01-01

    This paper provides an overview of Task-Based Language Learning (TBL) and its use in the teaching and learning of foreign languages. It begins by defining the concept of TBL, followed by a presentation of its framework and implications, and finally, a lesson plan based on TBL. The article presents an additional stage to be considered when planning…

  18. Building ESP Content-Based Materials to Promote Strategic Reading (Diseño de materiales basados en contenidos para fomentar estrategias de lectura en un curso de inglés con propósitos específicos)

    ERIC Educational Resources Information Center

    Bautista Barón, Myriam Judith

    2013-01-01

    This article reports on an action research project that proposes to improve the reading comprehension and vocabulary of undergraduate students of English for Specific Purposes--explosives majors, at a police training institute in Colombia. I used the qualitative research method to explore and reflect upon the teaching-learning processes during…

  19. New Educational Environments Aimed at Developing Intercultural Understanding while Reinforcing the Use of English in Experience-Based Learning (Nuevos entornos educativos destinados a desarrollar la comprensión intercultural y a reforzar el uso del inglés mediante el aprendizaje basado en experiencias)

    ERIC Educational Resources Information Center

    Bruguier, Leonard R.; Greathouse Amador, Louise M.

    2012-01-01

    New learning environments with communication and information tools are increasingly accessible with technology playing a crucial role in expanding and reconceptualizing student learning experiences. This paper reviews the outcome of an innovative course offered by four universities in three countries: Canada, the United States, and Mexico. Course…

  20. "On Air": Participation in an Online Radio Show to Foster Speaking Confidence. A Cooperative Learning-Based Strategies Study ("Al aire": participación en un programa de radio en línea para fomentar la confianza al hablar. Un estudio basado en estrategias de aprendizaje cooperativo)

    ERIC Educational Resources Information Center

    Lemos Tello, Nubia Consuelo

    2012-01-01

    The daily observation of class sessions has enabled me to recognize that students possess a feeling of self-distrust in oral activities. For this reason, I designed a study carried out with a group of twelve eighth graders. This article illustrates an action research project conducted to enhance students' confidence when speaking on an online…

  1. Geomorphologic Indices for Transition from Subduction to Arc-Continent Collision in Sumba Island, Indonesia

    NASA Astrophysics Data System (ADS)

    Authemayou, C.; Delcaillau, B.; Brocard, G. Y.; Molliex, S.; Nexer, M.; Pedoja, K.

    2014-12-01

    The Sumba Island lies in a key area to study the eastern Indonesia geodynamics. It is located in the Sunda-Banda fore-arc in the area of transition from subduction of the Indian oceanic lithosphere (W) beneath the Sunda-Banda arc to arc-continent collision between the Australian continental margin and the Sunda-Banda arc (E). East of the Sumba Island, the western boundary of the Savu basin originated during Middle Miocene by the southeastward slab retreat below the Sunda-Banda arc (Rigg and Hall, 2001). Previous studies has detected a global uplift of the island accommodating the Australian plate - South West Banda Arc convergence (Fleury et al., 2009). This uplift is associated with northeastward tilting and gravitational collapse to the South. Analyses of various geomorphic markers (perched low relief landscapes, rockyshore platform, coral reef terraces, drainages) and of morphometric indices allowed us to localise new structures (faults and folds), to determine the chronology of their activation and to better constraint the uplift history of Sumba Island. These results aim to understand the evolution of the deformation in Sumba Island in regard with its geodynamic context from Middle Miocene to present-day.

  2. A helium isotope transect along the Indonesian archipelago

    NASA Astrophysics Data System (ADS)

    Hilton, D. R.; Craig, H.

    1989-12-01

    Helium isotope studies have identified the Banda arc section of the Indonesian archipelago as the only circum-Pacific volcanic arc with He-3/He-4 ratios significantly lower than the common ratio in midocean ridge basalts (MORBs). This paper reports He-3/He-4 measurements along a 1800-km section of the Sunda arc, a region of underthrust oceanic lithosphere, showing MORB-like ratios from western Java to a surprisingly sharp transition zone centered on Lomblen Island, where the low ratios of the Banda arc begin. The results confirm the prediction that Sunda arc volcanoes should have MORB-like He-3/He-4 ratios, with a well-defined transition to the much lower Banda arc ratios near Lewotolo volcano, and demonstrate a remarkable linkage of helium isotope variations with tectonic processes not readily discernible with trace elements or other isotopes.

  3. Facilitating disaster preparedness through local radio broadcasting.

    PubMed

    Romo-Murphy, Eila; James, Ross; Adams, Mike

    2011-10-01

    The 2008 Disaster Mitigation Preparedness (DMP) study took place in Aceh province, Indonesia. It sought to help develop radio programmes and messages to increase resilience to disasters. The role of radio was evaluated during and after the 2004 Asian tsunami disaster. The study team interviewed 984 tsunami survivors from nine sub-districts of Banda Aceh, and local nongovernmental organisations convened eight focus groups around the area of Aceh Besar. Six key informant interviews were held with government disaster management agencies. The DMP survey is the first of its kind to interview a representative random sample of Banda Aceh residents. It reveals the importance of community and social networks, during disaster situations, when essential communications are down. A disaster warning information system based on a multi-media approach needs to be developed. The wider community should be involved in the planning, education and training of Banda Aceh and Aceh Besar residents to facilitate appropriate personal and community survival strategies.

  4. Burbujas interestelares alrededor de estrellas masivas: observaciones en frecuencias de Radio

    NASA Astrophysics Data System (ADS)

    Cappa, C.

    Los vientos estelares de estrellas masivas interactúan con el medio interestelar circundante originando burbujas interestelares que pueden detectarse en diversas bandas del espectro electromagnético, incluyendo la banda de radio. En esta presentación se hace una puesta al día de los resultados obtenidos a partir de observaciones en el continuo de radio y en líneas espectrales en dirección de estas estructuras. Estas observaciones nos permiten estudiar el material ionizado, atómico y molecular asociado a las burbujas interestelares.

  5. Profile of Secondary School Students with High Mathematics Ability in Solving Shape and Space Problem

    ERIC Educational Resources Information Center

    Putra, Mulia; Novita, Rita

    2015-01-01

    This study aimed to describe the profile of secondary school students with high mathematics ability in solving shape and space problem in PISA (Program for International Student Assessment). It is a descriptive research with a qualitative approach, in which the subjects in this study were students of class VIII SMP N 1 Banda Aceh. The results show…

  6. Listening as Translation: Reflections on Professional Development Work in a Cross-Cultural Setting

    ERIC Educational Resources Information Center

    Schultz, Katherine; Smulyan, Lisa

    2007-01-01

    As part of a campus-wide response by the University of Pennsylvania to the large-scale disaster caused by the earthquake and tsunami in South Asia, a team of teacher educators and graduate students worked with teachers, teacher educators, and administrators in Banda Aceh, Indonesia during July of 2005 and 2006. Working in Indonesia highlighted for…

  7. Acetylcholine, Histamine, and Cognition: Two Sides of the Same Coin

    ERIC Educational Resources Information Center

    Blandina, Patrizio; Efoudebe, Marcel; Cenni, Gabriele; Mannaioni, Pierfrancesco; Passani, Maria Beatrice

    2004-01-01

    The forebrain cholinergic neurons are localized in the nucleus basalis magnocellularis (NBM), the major source of cholinergic innervation to the neocortex and to the amygdala, and in the medium septum-banda diagonalis complex, which provides cholinergic inputs to the hippocampus (Mesulam et al. 1983; Woolf et al. 1984; Nicoll 1985). Basic and…

  8. Seaweeds of the Snellius-II expedition. Chlorophyta: Dasycladales

    NASA Astrophysics Data System (ADS)

    Coppejans, E.; Van Reine, W. F. Prud'Homme

    A survey is given of algae collected during the Snellius-II Expedition (1984) in the Banda, Sawu and Flores Seas, in particular the genera Acetabularia, Bornetella, Cymopolia, Neomeris and Polyphysa ( Dasycladales). Their morphology and anatomy are discussed, biogeographical data are added and a comparison is made with the material from the earlier Siboga Expedition (1899-1900).

  9. The San Marcos Pueblo Archaeological Site: A Review and Update of Ongoing Work by the Summer of Applied Geophysical Experience (SAGE)

    NASA Astrophysics Data System (ADS)

    Poje, M. S. L.; Berry, K.; Brandt, T. W.; Irwin, T. C.; Creighton, A.; MacLennan, K. J.; Ferguson, J. F.; Pellerin, L.

    2014-12-01

    The San Marcos Pueblo, one of the largest and most important cities of the pre-European Southwest, has long been a place of curiosity for archaeologists and geophysicists alike. Despite numerous archaeological investigations, primarily test excavations and surface surveys carried out at San Marcos from the early 1900s to the present, the site retains pottery sherds scattered along the surface from when it was first occupied in the thirteenth century to its abandonment during the Pueblo Revolt of 1680. Geophysical investigations have identified locations of kivas (ceremonial pits), middens (trash heaps), room blocks and possible metallurgy activity in the area. The site is located south of Santa Fe, NM and to the east of the Cerrillos Hills, a source for lead ore and turquoise. The students of SAGE have studied the San Marcos Pueblo for the past 11 years, and produced a map of the northeastern portion of the Pueblo colloquially called 'El Mapa Grande.' Ground penetrating radar (GPR), magnetics, and electromagnetic (EM) data were acquired on 30mx30m grids and seismic refraction data on various profiles throughout El Mapa Grande. During the 2014 field season new GPR data were acquired on two grids, magnetics data on one, and multiple grids were resurveyed with magnetics and EM to enhance resolution. The most recent GPR data extend coverage of two large anomalies that are part of linear EW-trending structures previously identified and consistent with a possible block wall or midden. Low GPR scatter and circular magnetic lows define several kivas. A target area in the NE of El Mapa Grande was thought to be related to metallurgic activity. Analysis of previous seismic data did not resolve any subsurface features corresponding to a metallurgy operation, but detected the magnetically-chaotic Ancha formation. Comparison with magnetic profile data support the interpretation that this anomaly is caused by a sub-crop of the Ancha Formation.

  10. Magmatism in western Indonesia, the trapping of the Sumba Block and the gateways to the east of Sundaland

    NASA Astrophysics Data System (ADS)

    Soeria-Atmadja, R.; Suparka, S.; Abdullah, Chalid; Noeradi, Dardji; Sutanto

    1998-04-01

    The western Sulawesi magmatic belt and the Sunda-Banda arc define the eastern and south-eastern margins of Sundaland, which is part of the relatively stable Eurasian plate. The eastern margin is bounded by the Makassar Strait which separates western Sulawesi from Kalimantan. The initial opening of the Makassar Strait took place in the late Cretaceous-Early Tertiary leading to the opening of the Pacific-Indian Ocean gateway during Neogene time. Recent studies indicate similarities in the late Cretaceous-Paleogene stratigraphic sequence and calc-alkali magmatism between Sumba, south Sulawesi and south-east Kalimantan, suggesting a Sundaland origin for all of these areas. The southward migration of Sumba to the present frontal arc position of the Sunda-Banda arc has occurred since Late Cretaceous-Paleocene time.

  11. 2004 Indian Ocean tsunami flow velocity measurements from survivor videos

    NASA Astrophysics Data System (ADS)

    Fritz, Hermann M.; Borrero, Jose C.; Synolakis, Costas E.; Yoo, Jeseon

    2006-12-01

    The tsunami of 26th December 2004 severely affected Banda Aceh along the North tip of Sumatra (Indonesia) at a distance of 250 km from the epicenter of the magnitude 9.0 earthquake. This tsunami flow velocity analysis focused on two survivor videos recorded within Banda Aceh more than 3 km from the open ocean. The exact locations of the tsunami eyewitness video recordings were revisited by the survey team between February 22 and 25, 2005 to record camera calibration ground control points. The motion of the camera during the recordings was determined. The individual video images were rectified with a direct linear transformation (DLT) assuming a planar water surface at the level. Finally a cross-correlation based particle image velocimetry (PIV) analysis was applied to the rectified video images to determine instantaneous tsunami flow velocity fields. The measured tsunami flow velocities were within the range of 2 to 5 m/s.

  12. Estudio multifrecuencia del medio interestelar cercano a HD 192281

    NASA Astrophysics Data System (ADS)

    Arnal, E. M.; Cappa, C.; Cichowolski, S.; Pineault, S.; St-Louis, N.

    Una de las causas que modifica la estructura y dinámica del medio interestelar es la acción que los vientos de las estrellas de gran masa ejercen sobre el mismo. En este trabajo, mediante el uso de datos interferométricos obtenidos en la banda de radio en la transición de 21-cm del Hidrógeno neutro y de imágenes de la emisión de continuo en las bandas de 408 y 1420 MHz, de imágenes HIRES del satélite IRAS en 60 y 100 micrones, y de observaciones de continuo obtenidas con radiotelescopios de disco simple en 2695, 4850 y 8350 MHz se ha realizado un estudio multifrecuencia de los efectos que los vientos estelares de HD 192281, una estrella de tipo espectral O5 Vn((f))p, han tenido sobre el medio interestelar que rodea a la misma.

  13. Evidence for the Jurassic arc volcanism of the Lolotoi complex, Timor: Tectonic implications

    NASA Astrophysics Data System (ADS)

    Park, Seung-Ik; Kwon, Sanghoon; Kim, Sung Won

    2014-12-01

    We report the first sensitive high-resolution ion microprobe (SHRIMP) U-Pb zircon ages with geochemical data from metavolcanic rocks in the Lolotoi complex, Timor. The zircon U-Pb ages of two andesitic metavolcanic rocks yield a permissible range of the Middle Jurassic extrusion from 177 Ma to 174 Ma. The geochemical data indicate that the origins of the basaltic and andesitic metavolcanic rocks are products of prolonged oceanic crust and arc magmatism, respectively. They are originated from partial melting of lherzolites, providing an insight into the tectonic evolution of the forearc basements of the Banda volcanic arc. Thus, parts of the Banda forearc basement are pieces of allochthonous oceanic basalts and Jurassic arc-related andesites accreted to the Sundaland during the closure of Mesotethys, and are incorporated later into the Great Indonesian Volcanic Arc system along the southeastern margin of the Sundaland.

  14. Management of hospitals in Aceh during the tsunami.

    PubMed

    Kartowisastro, Hermansyur

    2005-01-01

    On December 26th, 2004, Aceh and its vicinity was hit by two natural forces consecutively, an earthquake and a tsunami. Hundreds of thousands of people perished, leaving the remaining of about the same number to become refugees. The writer was assigned by the Ministry of Health to Aceh on duty on the second and third week after the catastrophe, to help the management of Zainoel Abidin General Hospital in Banda Aceh, the province's biggest hospital, revive its operation. PMID:16300161

  15. Distribución en gran escala de los cúmulos globulares en Fornax

    NASA Astrophysics Data System (ADS)

    Ostrov, P. G.

    Para analizar los cúmulos globulares azules y rojos de NGC 1399 asociados con NGC 1399 en particular, o si los cúmulos azules representaban un sistema asociado con el cúmulo de Fornax en general, se obtuvieron imágenes CCD de gran formato con el telescopio de 4m del CTIO, en las bandas C y T1. Se describe el método empleado y lo encontrado.

  16. Life After the Tsunami, a Motivation to Learn about Earth Hazards

    NASA Astrophysics Data System (ADS)

    Kerlow, I.; Sieh, K.; Rubin, C. M.

    2014-12-01

    Banda Aceh: Life After the Tsunami is a documentary feature film that explores the impact of tsunamis in the Banda Aceh communities of today and of centuries ago. The film uses the results of paleotsunami research conducted in the area to explain the dynamics of natural hazards within a humanistic framework. The film also presents testimonies of local survivors of the 2004 Indian Ocean tsunami to showcase the direct relationship that exists between scientific knowledge and survival rates. The proposed session focuses on how to use stories about the human experiences to motivate general audiences to learn about Earth science and natural hazards. It will also summarize some of the development and production challenges faced by the interdisciplinary team, especially in terms of presenting deep science in a format that is easy to understand by a general audience. The film is three years in the making and is anchored by several interconnected topics: 1. Testimonies dealing with tales of survival and human experiences during, right after, and since the tsunami.2. Cross-reference of social history with tectonics and tsunami activity in the Acehnese and West Sumatran regions of Indonesia.3. Scientific facts about paleotsunami research in the region, including general and easy-to-understand information about the Sumatran Plate Boundary, Sumatran subduction zone, and the Great Sumatran fault. The film is scheduled to be released on the 10th anniversary of the 2004 Indian Ocean Tsunami. Banda Aceh: Life After the Tsunami (working title) is produced by the Earth Observatory of Singapore (EOS) in partnership with the International Center for Aceh and Indian Ocean Studies (ICAIOS) at Syiah Kuala University, in Banda Aceh, Indonesia.

  17. Subduction in eastern Indonesia: how many slabs?

    NASA Astrophysics Data System (ADS)

    Milsom, John

    2001-08-01

    Seismicity associated with arc-continent collision in eastern Indonesia testifies to past north-directed subduction of Indian Ocean lithosphere beneath the Banda Sea. The complex patterns of deep seismicity have been cited as evidence for simultaneous south-directed subduction at the northern margin of the sea but this interpretation has not been universally accepted. Recently available recomputations of hypocentre locations have provided increased resolution of eastern Indonesian Wadati-Benioff Zones (WBZs). Shallow to intermediate depth seismic activity around the Banda Arc appears to support models involving subduction of two separate and distinct lithospheric slabs, but between 150 and 500 km the WBZ has a continuous 'shoehorn' shape. This shape confirms the presence of subducted lithosphere beneath Seram, in the north, as well as beneath Timor, in the south, is incompatible with independent subduction of two unconnected plates and implies rapid eastwards retreat of the subduction trace across a now vanished northern spur of the Indian Ocean. This 'roll-back' is unlikely to have been driven by local gravitational forces alone and may have been sustained by injection behind the Banda slab of asthenospheric material escaping from the Molucca Sea arc-arc collision.

  18. Base de linhas moleculares para síntese espectral estelar

    NASA Astrophysics Data System (ADS)

    Milone, A.; Sanzovo, G.

    2003-08-01

    A análise das abundâncias quí micas fotosféricas em estrelas do tipo solar ou tardia, através do cálculo teórico de seus espectros, emprega a espectroscopia de alta resolução e necessita de uma base representativa de linhas atômicas e moleculares com suas respectivas constantes bem determinadas. Nesse trabalho, utilizamos como ponto de partida as extensas listas de linhas espectrais de sistemas eletrônicos de algumas moléculas diatômicas compiladas por Kurucz para a construção de uma base de linhas moleculares para a sí ntese espectral estelar. Revisamos as determinações dos fatores rotacionais de Honl-London das forças de oscilador das linhas moleculares, para cada banda vibracional de alguns sistemas eletrônicos, seguindo a regra usual de normalização. Usamos as forças de oscilador eletrônicas da literatura. Os fatores vibracionais de Franck-Condon de cada banda foram especialmente recalculados empregando-se novas constantes moleculares. Reproduzimos, com êxito, as absorções espectrais de determinadas bandas eletrônicas-vibracionais das espécies moleculares C12C12, C12N14 e Mg24H em espectros de estrelas de referência como o Sol e Arcturus.

  19. Transcurrent reactivation of Australia's western passive margin: An example of intraplate deformation from the central Indo-Australian plate

    NASA Astrophysics Data System (ADS)

    Hengesh, J. V.; Whitney, B. B.

    2016-05-01

    Australia's northwestern passive margin intersects the eastern termination of the Java trench segment of the Sunda arc subduction zone and the western termination of Timor trough along the Banda arc tectonic collision zone. Differential relative motion between the Sunda arc subduction zone and the Banda arc collision zone has reactivated the former rifted margin of northwestern Australia evidenced by Pliocene to Quaternary age deformation along a 1400 km long offshore fault system. The fault system has higher rates of seismicity than the adjacent nonextended crustal terranes, has produced the largest historical earthquake in Australia (1941 ML 7.3 Meeberrie event), and is dominated by focal mechanism solutions consistent with dextral motion along northeast trending fault planes. The faults crosscut late Miocene unconformities that are eroded across middle Miocene inversion structures suggesting multiple phases of Neogene and younger fault reactivation. Onset of deformation is consistent with the timing of the collision of the Scott Plateau part of the passive continental margin with the former Banda trench between 3.0 Ma and present. The range of estimated maximum horizontal slip rates across the zone is ~1.4 to 2.6 mm yr-1, at the threshold of geodetically detectable motion, yet significant with respect to an intraplate tectonic setting. The folding and faulting along this part of the continental margin provides an example of intraplate deformation resulting from kinematic transitions along a distant plate boundary and demonstrates the presence of a youthful evolving intraplate fault system within the Indo-Australian plate.

  20. Mapping the edge of the Cerros del Rio volcanic field, New Mexico: a piece of the puzzle to understanding a potential geothermal resource

    NASA Astrophysics Data System (ADS)

    Pellerin, L.; Gallegos, M.; Goebel, M.; Murphy, B. S.; Smith, J.; Soto, D.; Swiatlowski, J.; Volk, C.; Welch, M.; Feucht, D. W.; Hollingshaus, B.; Bedrosian, P. A.; McPhee, D. K.

    2012-12-01

    The Cerros del Rio volcanic field located west of Santa Fe, New Mexico spans the southwestern part of the Espanola Basin with the Rio Grande to the west. Underlying the volcanics are the Santa Fe Group sediments, which contain the Ancha Formation, an important aquifer in the region. High temperature gradients in water wells reveal a potential geothermal prospect. In 2012 the Summer of Applied Geophysical Experience (SAGE) program acquired transient electromagnetic (TEM), audiomagnetotelluric (AMT), gravity and ground magnetic data to determine the buried eastern margin of the volcanic field and the connectivity related to the underlying sediments. The roughly EW 5-km long transect was sited from USGS aeromagnetic data to cross the boundary of the Cerros del Rio volcanic field. TEM data collected at ten stations, at 200-400 m spacing, along the transect employed an in-loop configuration with a square 100 m x 100 m transmitter loop and both a Zonge receiver coil and a 5 m square receiver loop. The 5 m loop allowed for the recovery of early-time data that was saturated when using the Zonge coil. AMT data were acquired at eight stations, at 400-500 m spacing, using the Geometric Stratagem system recording from 92 kHz to 10 Hz; a horizontal magnetic dipole transmitter was used to augment low signal strength at around 1 kHz. Gravity data along the profile were acquired using CG-3 and CG-5 Scintrex gravimeters with a station interval >250 m. Magnetic data were acquired with a Geometrics Cesium vapor G-858 magnetometer for about 3500 m along the profile at a 0.5 second sampling rate. Two volcanic flows interbedded with Ancha Formation and overlying Santa Fe Group sediments were identified in both the TEM and AMT modeling. High surface resistivity zones (>300 ohm-m) with depths ranging from ~100 to 300 m define the volcanic flows and correspond to high densities (2.3 to 2.55 g/cm3), while low resistivity zones (<30 ohm-m) correspond to lower densities (~2.1 g/cm3). High

  1. National uranium resource evaluation: Mesa quaddrangle, Arizona

    SciTech Connect

    Luning, R.H.; Thiede, D.S.; O'Neill, A.J.; Nystrom, R.J.; White, D.L.

    1982-06-01

    The Mesa Quadrangle (2/sup 0/), Arizona, was evaluated to a depth of 1500 meters to identify geologic environments and delineate surface and subsurface areas favorable for the occurrence of uranium deposits. The criteria used to define uranium favorability were developed during the National Uranium Resource Evaluation program. Surface and subsurface studies were augmented by aerial radiometric surveys and hydrogeochemical and stream-sediment reconnaisance studies. The results of the investigations identified three favorable areas: older Precambrian quartz monzonite near Horseshoe Dam; the gray unit of the Dripping Spring quartzite of Precambrian age in the Sierra Ancha, Salt River Canyon, and Mescal Mountain regions; and Tertiary lake beds near Cave Creek, Horseshoe Dam, and northeastern Tonto Basin. Unfavorable environments include nearly all older Precambrian crystalline and metamorphic rocks, most younger Precambrian igneous and sedimentary rocks, parts of the Paleozoic section, igneous intrusives of Laramide age. Tertiary volcanic rocks, and late Tertiary sedimentary rocks. The eastern third of the quadrangle remains unevaluated because access was prohibited or could not be obtained in time. Environments were unevaluated in older Precambrian volcanic, sedimentary, and metamorphic rocks; the Naco and Supai Formations; Cretaceous sedimentary rocks; and many Tertiary sedimentary rocks in intermontane basins and within the southwestern portion of the quadrangle because of time constraints, land access restrictions, and sparsity of subsurface data.

  2. Modern sand petrofacies in the Tonto and Salt River basins, central Arizona: Applying multivariate statistics to petrographic compositional analysis

    SciTech Connect

    Miksa, E.J. . Dept. of Geosciences); Heidke, J. )

    1993-04-01

    The Salt River and its tributary Tonto Creek occupy a large basin between the Mazatzal and Sierra Ancha Ranges. Over 200 sediment samples were collected from the Salt River, Tonto Creek, and their tributaries in order to identify discrete modern sand composition zones. The motivation for this study was to aid identification of archeological ceramic production locations. Most prehistoric ceramic production takes place within 1 km of raw material source areas. Identification of unique sand temper sources thereby aids in locating production areas and trade routes. Sediment samples were sieved and washed so that only the sand fraction remained. Samples were mounted in epoxy, thin-sectioned, and stained for K and Ca. Thin-sections were counted to 400 points using the Gazzi-Dickinson technique. Twenty-six grain types were identified, with special care being taken to distinguish among different rock fragments. Samples were divided into 15 likely petrofacies based on geologic maps and composition. Correspondence analysis was used with each grain type considered separately to further refine the petrofacies boundaries, resulting in 20 spatially and compositionally discrete groups. Discriminant analysis was used to test the possibility of separating samples from different petrofacies. For this test, grain types were grouped into categories (i.e. all metamorphic grains, all feldspars). Discrimination among the 20 petrofacies was found to be better than 75%.

  3. The Malaysian Orthopaedic Association humanitarian mission to Indonesia and Sri Lanka.

    PubMed

    Sharaf, I; Saw, A; Hyzan, Y; Sivananthan, K S

    2005-07-01

    The tsunami which occurred off the west coast of North Sumatra on December 26, 2004 devastated the coastal areas of North Sumatra, South-West Thailand, South-East India and Sri Lanka killing more than a quarter of a million people. The destruction was enormous with many coastal villages destroyed. The other countries affected were Malaysia, Myanmar, Maldives, Bangladesh, Somalia, Kenya, Tanzania and the Seychelles. In January 2005, volunteers went in weekly rotation to Banda Aceh in collaboration with Global Peace Mission. These were Dr Hyzan Yusof, Dr Suryasmi Duski, Dr Sharaf Ibrahim, Dr Saw Aik, Dr Kamariah Nor and Dr Nor Azlin. In Banda Aceh, the surgical procedures that we could do were limited to external fixation of open fractures and debriding infected wounds at the Indonesian Red Crescent field hospital. In February, a team comprising Dato Dr K S Sivananthan, Dr T Kumar and Dr S Vasan spent a week in Sri Lanka. In Sri Lanka, Dato Sivananthan and his team were able to perform elective orthopaedic operations in Dr Poonambalam Memorial Hospital. We appealed for national and international aid and received support from local hospitals and the orthopaedic industry. International aid bound for Banda Aceh arrived in Kuala Lumpur from the Philippine Orthopaedic Association, the Chiba Children's Hospital in Japan and the Chinese Orthopaedic Association. The COA donated 1.5 tons of orthopaedic equipments. A special handing over ceremony from the COA to the Indonesian Orthopaedic Association was held in Putrajaya in March. Malaysia Airlines flew in the donated equipment to Kuala Lumpur while the onward flight to Aceh was provided by the Royal Malaysian Air Force. In April, Dr Saw Aik and Dr Yong Su Mei joined the Tsu-Chi International Medical Association for volunteer services on Batam Island, Indonesia. The MOA acknowledges the many individuals and organizations, both governmental and non-governmental, for their contributions in the humanitarian efforts.

  4. Structural expression of forearc crust uplift due to subducting asperity

    NASA Astrophysics Data System (ADS)

    Fleury, Jean-Marc; Pubellier, Manuel; de Urreiztieta, Marc

    2009-12-01

    New structural observations and mapping of reefal terraces, carried out both on the field and on satellite remote sensing data, indicate that Sumba Island is presently undergoing a large amount of extension, associated with a significant regional uplift. This crustal uplift may have been created by a major thrust emerging in the South of the island. The uplift, which partly accommodated the Australian plate-South West Banda Arc convergence, is associated with the general northeastward tilt of the island. The consequent anomalous positive topography along the southern coast of the island is being compensated by significant tectonic erosion along large-scale curvilinear normal faults in the southeastern half of the island. The most important expression of this gravitational collapse is located at the receding side of an advancing circular dome, showing striking similarities with accretionary wedges being affected by seamount subduction. The part of the forearc basin known as the Savu Basin is moderately deformed (mostly in its central part) and appears to act as a rigid buttress in the convergence between the Banda Arc and the Australian plate. As a result the convergence appears to be transferred northward within the actively-shortening back-arc domain, which goes from the north of the Flores Island to the southwest of the Timor block. The convergent plate boundary shows a transition between a stable domain (West of Sumba) and a tectonized domain (East of Sumba), the latter coinciding with the subduction of the outer Australian passive margin. The subduction of the ocean-continent boundary of the Austral-Indian plate below the Banda arc since the Lower Pliocene may have incorporated some crustal fragments in the plunging Benioff zone. Most likely, the integration of the stretched continental lithosphere in the subduction zone caused the uplift the entire forearc domain, exhibiting inherited structures of the upper plate.

  5. Assessment of health-related needs after tsunami and earthquake--three districts, Aceh Province, Indonesia, July-August 2005.

    PubMed

    2006-02-01

    On December 26, 2004, an earthquake measuring 9.2 on the Richter scale off the northwest coast of the island of Sumatra, Indonesia, produced a tsunami that caused the deaths of an estimated 230,000 persons in India, Indonesia, the Maldives, Somalia, Sri Lanka, and Thailand. The majority of casualties were in Aceh Province (population 4.5 million) in northern Sumatra, Indonesia, where an estimated 130,000 persons died. In addition, 500,000 persons were displaced from their homes, and 37,000 remain unaccounted for in the province. In the Aceh Province districts of Banda Aceh and Aceh Besar, an estimated 90,000 persons died; approximately 75% of health workers in Banda Aceh either died or were displaced from their homes. On March 28, 2005, a second major earthquake, measuring 8.7 on the Richter scale, caused large-scale damage to the islands of Simeulue and Nias off the western Sumatra coast; approximately 300 persons died, and thousands were displaced. The international community responded to these events with the largest relief measures ever undertaken for a natural disaster. To determine the health and nutrition status of the affected populations and to evaluate the effectiveness of relief interventions 7 months after the tsunami and 3 months after the second earthquake, Cooperative for Assistance and Relief Everywhere, Inc. (CARE) International Indonesia and CDC conducted surveys in three districts of Aceh Province (Aceh Besar, Banda Aceh, and Simeulue). This report summarizes the results of those surveys, which identified routine vaccinations and provision of toilets or latrines as particular areas for improvement and revealed no significant difference in health indicators between internally displaced persons (IDPs) and nondisplaced populations. The relief response in Aceh Province should target areas needing improvement with programs that serve both IDPs and nondisplaced persons, as measures are implemented to rebuild the public health infrastructure.

  6. Species profiles: Life histories and environmental requirements of coastal fishes and invertebrates (Pacific Northwest)--ghost and blue mud shrimp

    USGS Publications Warehouse

    Hornig, S.; Sterling, A.; Smith, S.

    1989-01-01

    Geographic range: The ghost shrimp is found in intertidal areas along the west coast of North America from Mutiny Bay, Alaska, to the mouth of the Tijuana River, San Diego County, California; MacGinitie (1934) and Ricketts and Calvin (1968) reported finding specimens as far south as El Estuario de Punto Banda, Baja California Norte, Mexico. The blue mud shrimp is found from southeastern Alaska to San Quentin Bay (Bahia de San Quentin) in Baja California Norte. The general distribution of the two species in the Pacific Northwest is identical (Figure 3).

  7. Earthquakes, November-December 1992

    USGS Publications Warehouse

    Person, W.J.

    1993-01-01

    There were two major earthquakes (7.0≤M<8.0) during the last two months of the year, a magntidue 7.5 earthquake on December 12 in the Flores region, Indonesia, and a magnitude 7.0 earthquake on December 20 in the Banda Sea. Earthquakes 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 earthquake caused slight damage at Big Bear in southern California. 

  8. L'ôle de Kur: géologie du flanc oriental du bassin de Weber (Indonésie orientale)

    NASA Astrophysics Data System (ADS)

    Honthaas, Christian; Villeneuve, Michel; Réhault, Jean-Pierre; Bellon, Hervé; Cornée, Jean-Jacques; Saint-Marc, Pierre; Butterlin, Jacques; Gravelle, Michel; Burhanuddin, Safri

    1997-12-01

    New biostratigraphical, geochronological and geochemical data from Kur island and two nearby dredgings allow us to show unknown events on the eastern margin of the Weber basin: an Early Oligocene magmatic arc; a tectono-metamorphic event between 24 and 17 Ma; and an Early Pliocene deformation, related to the collision between the Australian plate and the Banda arc. The Weber basin was created during Pleistocene with an uplift of its eastern margin. These events are briefly replaced within the geodynamic context of the Eastern Indonesia.

  9. Observaciones del CH interestelar y el continuo en 3,3 GHz

    NASA Astrophysics Data System (ADS)

    Olano, C. A.; Combi, J. A.; Pöppel, W.; Benaglia, P.; Sanz, A. J.; Bava, J. A.

    Se informa sobre el proyecto que se lleva a cabo en el IAR con el propósito de observar las líneas hiperfinas del estado fundamental del CH y el continuo en la banda de 3,3 GHz. El nuevo receptor construído en nuestro laboratorio para tal fin se instaló sobre uno de los radiotelescopios, funcionando conjuntamente con los sistemas de procesamiento actuales del IAR. Los resultados de las primeras observaciones, realizadas tanto en las líneas espectrales como en el continuo sobre fuentes conocidas, fueron satisfactorios.

  10. La Función de Luminosidad de las poblaciones de cúmulos globulares alrededor de NGC 1399

    NASA Astrophysics Data System (ADS)

    Ostrov, P. G.; Forte, J. C.; Geisler, D.

    Mediante el empleo de una técnica especial para filtrar el pattern de fringing, se ha obtenido una función de luminosidad de los cúmulos globulares de NGC 1399 superando por ~ 1 mag el turn-over en la banda T1 del sistema de Washington. El análisis de los resultados de la fotometría multibanda (C, M, T1) permite determinar que las mitades mas brillantes de las funciones de luminosidad de las dos principales poblaciones de cúmulos globulares asociadas con esta galaxia son similares.

  11. Seismic response to slab rupture and variation in lithospheric structure beneath the Savu Sea, Indonesia

    NASA Astrophysics Data System (ADS)

    Ely, Kim S.; Sandiford, Mike

    2010-03-01

    Variations in seismic moment release and stress state across the transition from subduction of oceanic crust to arc-continent collision in the Banda Arc are constrained by focal mechanism solutions from the CMT earthquake catalogue. In particular the slab under the western Savu Sea is unusual in that intermediate depth (70-300 km) events indicate that at this depth range the slab is largely in down-dip compression. This contrasts with the intermediate depth, down-dip tension that typifies the Sunda slab to the west and the far eastern Banda slab to the east. Down-dip compression beneath the Savu Sea reflects subduction of transitional crust of the Scott Plateau, more buoyant than the Indian Ocean crust subducting further west. In this region, enhanced magma flux is indicated by unusually narrow volcano spacing in the overlying arc, and suggests that down-dip compression reflects not only more buoyant transitional crust but also a reduction in slab-wedge coupling induced by enhanced magma flux. East of the Savu Sea, the near complete absence of intermediate depth seismicity is attributed to a slab window that has opened where Australian continental crust has collided with the arc. Differences in seismic moment release around this slab window indicate asymmetric rupture, propagating to the east at a much faster rate than to the west.

  12. Fotometria de grupos compactos de galáxias no infravermelho próximo

    NASA Astrophysics Data System (ADS)

    Brasileiro, F.; Mendes de Oliveira, C.

    2003-08-01

    Apresentamos medidas nas bandas J, H e K de cerca de 90 galáxias em 34 grupos compactos. Através da combinação dos novos dados, com dados obtidos na literatura para a banda B, investigamos como as luminosidades, cores, tamanhos e massas das galáxias em grupos compactos foram afetadas por processos dinâmicos, e como essas diferem de galáxias em ambientes menos densos. Uma comparação dos novos valores obtidos com aqueles listados no catálogo 2MASS, mostram que para 50 galáxias estudadas em comum, as diferenças nas magnitudes J, H e K estão dentro dos erros fotométricos. Através da construção dos diagramas de cor (J-H x H-K e B-H x J-K), percebemos que as galáxias em grupos compactos ocupam posições no diagrama diferentes das posições de galáxias em campo ou em aglomerados, sendo mais parecidas com as posições ocupadas por galáxias HII, ou com excesso de poeira, acreditamos que tal deslocamento é derivado do aumento da taxa de formação estelar.

  13. Estudio multifrecuencia del medio interestelar cercano a HD 192281

    NASA Astrophysics Data System (ADS)

    Arnal, E. M.; Cappa, C. E.; Cichowolski, S.; Pineault, S.; St-Louis, N.

    Una de las causas que modifica la estructura y dinámica del medio interestelar es la acción que los vientos de las estrellas de gran masa ejercen sobre el mismo. En este trabajo, mediante el uso de datos interferométricos obtenidos en la banda de radio en la transición de λ˜21-cm del hidrógeno neutro y de imágenes de la emisión de continuo en las bandas de 408 y 1420 MHz, de imágenes HIRES del satélite IRAS en 60 y 100μm, y de observaciones de continuo obtenidas con radiotelescopios de disco simple en 2695, 4850 y 8350 MHz se ha realizado un estudio multifrecuencia de los efectos que los vientos estelares de HD 192281, una estrella de tipo espectral O5,Vn((f))p, han tenido sobre el medio interestelar que rodea a la misma.

  14. New Insights into the Active Tectonics of Eastern Indonesia from GPS Measurements

    NASA Astrophysics Data System (ADS)

    Susilo, S.; Koulali Idrissi, A.; McClusky, S.; Meilano, I.; Cummins, P. R.; Tregoning, P.; Syafii, A.

    2014-12-01

    The Indonesian archipelago encompasses a wide range of tectonic environments, including island arc volcanism, subduction zones, and arc-continent collision. Many of the details of this tectonic activity are still poorly understood, especially where the Australian continent collides with Indonesia, separating the Sunda Arc in west from that at the Banda Arc in the east. While it seems clear that the Australian plate is subducted under both the Sunda and Banda Arcs, it is not clear what happens along the 1000 km -long stretch in between. The question of just where the plate motion is accommodated is of major importance to assessments of earthquake and tsunami hazard in the region. To help resolve these questions the Geospatial Information Agency of Indonesia has collaborated with the Australian National University and the Bandung Institute of Technology in a GPS campaign spanning much of eastern Indonesia, from Lombok in the west to Alor in the east. We have combined these data with those from previous campaigns, resulting in over 27 campaign and 18 continuous GPS sites being used in the analysis. The improvement in site density allowed us to develop of a more complete description of tectonic activity in this region than has been obtained in previous studies. Our preliminary results suggests that there is a relatively simple transition from subduction at the Java Trench off east Java, to a partitioned convergence along both the Timor Trough and the Flores Thrust in the Nusa Tenggara region.

  15. Participation in the 1996 Arlindo Cruise to the Indonesian Seas

    NASA Technical Reports Server (NTRS)

    Marra, John

    1997-01-01

    The objective of Arlindo-Productivity is to understand the factors responsible for regional differences in the response of phytoplankton and zooplankton to the SE and NW Monsoons in Indonesia. The hypothesis is that an interplay between circulation and shoaling of the nutricline, as a response to the monsoons, regulates productivity in the Indonesian Seas. My o@jective for the cruise in 1996 was to continue our collaboration with Indonesian scientists by conducting a set of hydrographic, primary production and spectral irradiance observations in the Indonesian Seas. This grant paid for shipping, travel and incidental costs associated with participation in the cruise in December, 1996. Ship costs were borne by the Indonesian Institute of Sciences as part of the collaborative effort. A plan for Arlindo in 1996 was agreed upon in March, 1996, by Indonesian scientists together with Arnold Gordon. The plan called for a 20-day physical oceanography and mooring cruise in November, 1996, followed by a 5-day bio-optical cruise. The bio-optical cruise departed from, and returned to, Ambon, and sampled in the Banda Sea. We completed a series of chlorophyll analyses, both a sampling of surface variability and depth profiles in the Banda Sea. We also completed three MER profiles for depth profiles of spectral irradiance. These data have a useful by-product in that they can be used for vicarious calibration of the OCTS sensor aboard the ADEOS satellite. As such, the data has been transmitted to NASDA in Japan for their use.

  16. Sea Surface Temperature Coupling to Madden-Julian Oscillations over the Indonesian Maritime Continent

    NASA Astrophysics Data System (ADS)

    Napitu, A. M.; Gordon, A. L.; Pujiana, K.

    2014-12-01

    The intraseasonal SST characteristics within the Indonesian Seas and their responses to the Madden-Julian Oscillations [MJO] are examined through analyses of observed and reanalysis datasets. Intraseasonal variation accounts for about 30% of SST variability, with the strongest signature is observed in Banda and Timor seas. The MJO signature in SST is evident in the form of energy peak at 35-45 days, amplification during the Northwest Monsoon (boreal winter), and eastward propagation. SST responds to sea-air heat flux associated with MJO with net heat flux into the ocean (atmosphere) characterizing the suppressed (active) phase of MJO. The influence of MJO on Banda Sea SST is greatest during La Niña periods, which are favorable for deeper thermocline conditions, which diminish the role of ocean processes driving vertical heat transfer between subsurface and surface layers. Diminished influence of ocean processes results in dominance of surface heat fluxes associated with MJO in governing intraseasonal SST variability. During El Niño, the role of ocean processes is favorable to mediate heat transfer between lower and upper layer of the ocean surface as thermocline is shallower. The ocean component heat fluxes then compete with MJO forced heat fluxes in governing SST variability as indicated by less pronounced eastward propagation.

  17. Past dynamics of the Australian monsoon: precession, phase and links to the global monsoon concept

    NASA Astrophysics Data System (ADS)

    Beaufort, L.; van der Kaars, S.; Bassinot, F. C.; Moron, V.

    2010-10-01

    Past variations in the dynamics of the Australian monsoon have been estimated from multi-proxy analysis of a core retrieved in the Eastern Banda Sea. Records of coccolith and pollen assemblages, spanning the last 150 000 years, allow reconstruction of past primary production in the Banda Sea, summer moisture availability, and the length of the dry season in northern Australia and southeastern Indonesia. The amount of moisture available during the summer monsoon follows typical glacial/interglacial dynamics with a broad asymmetrical 100-kyr cycle. Primary production and length of the dry season appear to be closely related, given that they follow the precessional cycle with the same phase. This indicates their independence from ice-volume variations. The present inter-annual variability of both parameters is related to El Niño Southern Oscillation (ENSO), which modulates the Australian Winter Monsoon (AWM). The precessional pattern observed in the past dynamics of the AWM is found in ENSO and monsoon records of other regions. A marked shift in the monsoon intensity occurring during the mid Holocene during a period of constant ice volume, suggests that low latitude climatic variation precedes increases in global ice volume. This precessional pattern suggests that a common forcing mechanism underlies low latitude climate dynamics, acting specifically and synchronously on the different monsoon systems.

  18. Past dynamics of the Australian monsoon: precession, phase and links to the global monsoon

    NASA Astrophysics Data System (ADS)

    Beaufort, L.; van der Kaars, S.; Bassinot, F. C.; Moron, V.

    2010-06-01

    Past variations in the dynamics of the Australian monsoon have been estimated from multi-proxy analysis of a core retrieved in the Eastern Banda Sea. Records of coccolith and pollen assemblages, spanning the last 150,000 years, allow reconstruction of past primary production in the Banda Sea, summer moisture availability, and the length of the dry season in Northern Australia and Southeastern Indonesia. The amount of moisture available during the summer monsoon follows typical glacial/interglacial dynamics with a broad asymmetrical 100-kyr cycle. Primary production and length of the dry season appear to be closely related, given that they follow the precessional cycle with the same phase (August insolation). This indicates their independence from ice-volume variations. The present inter-annual variability of both parameters is related to El Niño Southern Oscillation (ENSO), which modulates the Australian Winter Monsoon (AWM). The precessional pattern observed in the past dynamics of the AWM is found in ENSO and monsoon records of other regions. A marked shift in the monsoon intensity occurring during the mid Holocene during a period of constant ice volume, suggest that low latitude climatic variation precedes global ice volume. This precessional pattern suggests that a common forcing mechanism underlies low latitude climate dynamics, acting specifically and synchronically on the different monsoon systems.

  19. El espectro de KX TrA entre 1990 y 1996

    NASA Astrophysics Data System (ADS)

    Brandi, E.; García, L.; Ferrer, O.; Barbá, R.

    La estrella simbiótica KX TrA = He2-177 fue observada espectroscópicamente con el telescopio de 2.15 m del CASLEO entre los años 1990 y 1996, utilizándose resoluciones intermedia y alta. El rango espectral estudiado se extiende desde 4400 Åa 7200 Å. La historia fotométrica de KX TrA presenta explosiones del mismo tipo que las mostradas por la nova lenta RR Tel y su espectro de alta excitación, muy rico en líneas de emisión, es también similar al de RR Tel. Por lo tanto, es importante analizar la evolución espectral de KX TrA en el tiempo, prestando especial atención a los posibles cambios en los niveles de excitación. Las emisiones presentes corresponden a transiciones permitidas y prohibidas con un amplio rango de ionización, incluyéndose las anchas e intensas líneas originadas por scattering Raman de O VI en λλ 6825 y 7082 Å. En el período cubierto por nuestras observaciones se estudia la variación de la intensidad relativa de las emisiones, el comportamiento de las velocidades radiales y los cambios de perfiles de las líneas, especialmente en Hα y Hβ. El contínuo de la región roja observada indica un tipo espectral no más tardío que M3 para la componente gigante fría del sistema.

  20. Patterns of deformation, exhumation and uplift across the Island of Timor: insights into the processes that control the early stages of orogenesis (Invited)

    NASA Astrophysics Data System (ADS)

    McQuarrie, N.; Tate, G. W.; Van Hinsbergen, D. J.; Harris, R. A.

    2013-12-01

    On the island of Timor, arc-continent collision between the Banda volcanic arc and the Australian continent since the late Miocene has uplifted a mountain range containing both deeply exhumed metamorphic rocks and deepwater synorogenic basins. These varied lithologies are separated by a few tens of kilometers, and provide us with an opportunity to examine the spatial patterns of differential uplift and exhumation and its links to the geometry and magnitude of deformation in an orogen that is still in its infancy. New mapping in Timor has provided a detailed view of how the Australian continental slope and shelf rocks are being structurally repeated below overriding Banda Arc material. In East Timor, a window though the Banda terrane shows Permian and Triassic rocks that are repeated by four NNE-striking thrust faults with ~3 km spacing and 50-75 km along-strike extent. The strike of these faults is rotated 50-60 degrees compared to structures to the east and west of this main window. In addition, mapped fold axes are shown to cut across and warp fault traces. These map patterns indicate that the duplex has been both refolded and tilted since its initial formation. In West Timor, Permian through Triassic stratigraphy is faulted and folded into an antiformal stack with 5 exposed thrusts repeating an ~ 3 km thick section. Both south of and adjacent to these structural highs are 10-20 km wide piggyback basins of deepwater, synorogenic marine limestones and clays that coarsen upward into turbidites. Deposition of these units initiated at 5.5 Ma at lower bathyal depths. Synorogenic deposition directly over the Bobonaro mélange, which acts as the décollement between the overthrust Banda Arc rocks and the structurally repeated Australian margin rocks, requires the removal of both Banda arc material and the Cretaceous and younger Kolbano sequence before deposition. These basins record rapid surface uplift to upper bathyal depths from 3.5-3 Ma with continual uplift to

  1. Re-evaluation of the Cablac Limestone at its type area, East Timor: Revision of the Miocene stratigraphy of Timor

    NASA Astrophysics Data System (ADS)

    Haig, David W.; McCartain, Eujay W.; Keep, Myra; Barber, Logan

    2008-08-01

    The Cablac Limestone, widely recorded in Timor, has its type area on Cablac Mountain where it was regarded as a Lower Miocene shallow-marine carbonate-platform succession. The Bahaman-like facies placed in the Cablac Limestone are now known to belong to the Upper Triassic-Lower Jurassic rather than the Lower Miocene. On the northern slopes of Cablac Mountain, a crush breccia, formerly regarded as the basal conglomerate of the formation, is now considered to have developed along a high-angle fault separating Banda Terrane units of Asian affinity from an overthrust limestone stack containing units belonging to the Gondwana and Australian-Margin Megasequences. The Cablac breccia includes rock fragments that were probably derived locally from these tectonostratigraphic units after terrane emplacement and overthrusting. Clasts include peloid and oolitic limestones of the Upper Triassic-Lower Jurassic derived from the Gondwana Megasequence, deep-water carbonate pelagites of the Cretaceous and Paleogene derived from the Australian-Margin Megasequence, Upper Oligocene-Lower Miocene (Te Letter Stage) shallow-water limestone derived from the Banda Terrane, and a younger Neogene calcarenite containing clasts of mixed tectonostratigraphic affinity. There is no evidence for significant sedimentary or tectonic transport of clasts that form the breccia. The clast types and the present understanding of the geological history of Timor suggest that the crush breccia formed late in the Plio-Pleistocene uplift history of Timor. It is not the basal conglomerate of the Cablac Limestone. However, the clasts of an Upper Oligocene-Lower Miocene limestone found in the breccia suggest that a shallow-marine limestone unit of this age either outcrops in the region and has not been detected in the field, or has been eroded completely during late Neogene uplift. The clasts are similar in age and lithology to an Upper Oligocene-Lower Miocene formation that unconformably overlies a metamorphic

  2. Nurture Versus Nature: Accounting for the Differences Between the Taiwan and Timor active arc-continent collisions

    NASA Astrophysics Data System (ADS)

    Harris, R. A.

    2011-12-01

    The active Banda arc/continent collision of the Timor region provides many important contrasts to what is observed in Taiwan, which is mostly a function of differences in the nature of the subducting plate. One of the most important differences is the thermal state of the respective continental margins: 30 Ma China passive margin versus 160 Ma NW Australian continental margin. The subduction of the cold and strong NW Australian passive margin beneath the Banda trench provides many new constraints for resolving longstanding issues about the formative stages of collision and accretion of continental crust. Some of these issues include evidence for slab rollback and subduction erosion, deep continental subduction, emplacement or demise of forearc basement, relative amounts of uplift from crustal vs. lithospheric processes, influence of inherited structure, partitioning of strain away from the thrust front, extent of mélange development, metamorphic conditions and exhumation mechanisms, continental contamination and accretion of volcanic arcs, does the slab tear, and does subduction polarity reverse? Most of these issues link to the profound control of lower plate crustal heterogeneity, thermal state and inherited structure. The thermomechanical characteristics of subducting an old continental margin allow for extensive underthrusting of lower plate cover units beneath the forearc and emplacement and uplift of extensive nappes of forearc basement. It also promotes subduction of continental crust to deep enough levels to experience high pressure metamorphism (not found in Taiwan) and extensive contamination of the volcanic arc. Seismic tomography confirms subduction of continental lithosphere beneath the Banda Arc to at least 400 km with no evidence for slab tear. Slab rollback during this process results in massive subduction erosion and extension of the upper plate. Other differences in the nature of the subducting plates in Taiwan in Timor are differences in the

  3. Como Lo Hago Yo: Anomalías del Tubo Neural en Guatemala — Mielomeningocele Unidad de Espina Bífida e Hidrocefalia

    PubMed Central

    Manucci, Graciela; von Quednow, Enzo

    2014-01-01

    En Guatemala nacen por añ 786 niños con defectos de tubo neural. Operamos 65 a 70 niños con mielomenigocele por año. Tenemos equipo multidisciplinario. Recomendamos parto por cesárea. Infección antes de la cirugía es un problema mayor. Derivación tardía es un problema. Disecamos la plaqueta con la técnica clásica. Suturamos la plaqueta para restituir la forma de la médula. Corpectomía en casos de cifósis. Hidrocefalía: Operamos el 80% de los niños. Chiari II: Operamos basados en los síntomas, primero nos aseguramos que la válvula funciona bien. Médula anclada: Operamos basados en los síntomas. PMID:24791216

  4. Sintetizadores de síntesis digital directa

    NASA Astrophysics Data System (ADS)

    Olalde, J. C.; Perilli, D.; Larrarte, J. J.

    Se describen las características e implementación de sintetizadores de alta resolución en frecuencia, <= 2 mHz, tiempos de conmutación rápidos, submicrosegundo, con posibilidad de control de fase basados en la técnica de síntesis digital directa. La implementación se realiza a partir del circuito integrado AD7008, que incluye un oscilador controlado numéricamente y un conversor analógico digital, y en el trabajo se dan pautas para la especificación de los filtros de reconstrucción. El instrumento implementado posee un módulo basado en un microcontrolador INTEL 8752 el cual provee la posibilidad de monitoreo, indicación visual y control en forma local a partir de un teclado; y remoto a partir de un ``host" con interfases RS232 y RS 485.

  5. [Non-speech oral motor treatment efficacy for children with developmental speech sound disorders].

    PubMed

    Ygual-Fernandez, A; Cervera-Merida, J F

    2016-01-01

    Introduccion. En el tratamiento logopedico de las dificultades de habla se practican dos enfoques metodologicos antagonicos: los no verbales, basados en ejercicios de motricidad oral (EMO), y los verbales, que se basan en tareas de procesamiento de habla con silabas, fonemas y palabras. En España, los programas de EMO se llaman 'programas de praxias', estan muy difundidos y son apreciados por los logopedas. Objetivo. Revisar los estudios sobre la eficacia de los tratamientos basados en EMO aplicados a niños con trastornos de habla y los argumentos teoricos que podrian justificar o no su utilidad. Desarrollo. Durante las ultimas decadas se han acumulado pruebas sobre la falta de eficacia de este enfoque en el tratamiento de los trastornos evolutivos del habla y en las dificultades de pronunciacion de poblaciones sin alteracion neurologica de la funcion motriz. La American Speech-Language-Hearing Association ha desaconsejado su uso atendiendo a los principios de practica basada en la evidencia. Los conocimientos acumulados sobre el control motor demuestran que el patron de movilidad y su correspondiente organizacion cerebral son diferentes en el habla y en otras funciones no verbales ligadas a la alimentacion y la respiracion. Conclusiones. Ni los estudios sobre su eficacia ni los argumentos a partir de estudios del control motor aconsejan el uso de los programas basados en EMO para el tratamiento de las dificultades de pronunciacion en niños con trastornos evolutivos del lenguaje.

  6. Down-depth Seismicity Gaps and the Shape of the Seismic Zone along the entire Indonesian arc from Relocated Hypocenters

    NASA Astrophysics Data System (ADS)

    Das, S.

    2005-05-01

    Using thousands of handpicked P, S, pP, sP, PcP, and ScP phases from digitally recorded seismograms, together with International Seismological Centre reported phases, we obtain improved hypocentral locations for ~2600 earthquakes deeper than 50 km with mb > ~5.0 earthquakes, for the period 1962 to September 1996, along the Indonesian subduction zone. The seismicity distribution is found to be very non-uniform both along the arc and in depth. Gaps in the relocated hypocenters exist along depth in most places of the arc, with its upper edge varying from 100-450 km depth and its lower edge from 350-670 km in different portions of the arc. The relocated hypocenters show that (1) a portion of the Indonesian arc between ~110°E and 123°E longitude, and deeper than ~500 km, is dipping southward at an angle of ~75°, that is, in a direction opposite to the upper part of the north dipping slab, suggesting southward lateral flow in the mantle, relative to the plate motion vector here. (2) East of about 108°E, the seismic zone is wider near 670 km than near the 500 km depth. (3) The seismic zone between 129--131°E in the 100--200 km depth range is the widest along the arc both in strike and downdip. This region, near the highest arc curvature, has the highest seismic activity, and is the only part of the arc with earthquakes continuously occurring from the surface down to below 600 km. (4) The very deep earthquakes under Sulawesi are shown to be part of the west-southwest dipping Seram slab. (5) In the westernmost part of the Banda arc, the slab is under downdip tension in the 50-250 km depth range, while the deepest portion of the slab in this region is under compression. From 128-131°E the slab between 100--200 km depth is under mainly horizontal compression. Our study supports the "two-slab" model for the Banda arc. 3-D computer animations of the subduction zone will be presented. Das, S. (2004) Seismicity Gaps and the Shape of the Seismic Zone in the Banda Sea Region

  7. Link between the northward extension of Great Sumatra Fault and continental rifting in the Andaman Sea: new results from seismic reflection studies

    NASA Astrophysics Data System (ADS)

    Singh, S. C.; Moeremans, R. E.; McArdle, J.; Johansen, K.

    2012-12-01

    The Great Sumatra Fault (GSF) traverses the main land Sumatra from Sunda Strait in the southeast to Banda Aceh in the northwest for about 1900 km, and defines the present day plate boundary between the Sunda Plate in the north and Burmese Sliver Plate in the south. It is formed due to the oblique subduction of the Indo-Australian Plate beneath the Sunda Plate. It has been well studied on land but is poorly studied north of Banda Aceh in the Andaman Sea. Its study is further complicated by the presence of volcanic arc in its vicinity and its interaction with the West Andaman Fault (WAF) further north. Here we present deep seismic reflection images along the northward extension of the GSF over 700 km until it joins the Andaman Spreading Centre and interpret these images in the light of earthquake, gravity and bathymetry data. We find that the GSF has two strands between Banda Aceh and Nicobar Island: a transpression in the south and a deep narrow active rift basin in the north dotted with volcanoes in the center, suggesting that the volcanic arc is coincident with the rifting. Further north of Nicobar Island, an active strike-slip fault cuts through a deep rifted basin until its intersection with Andaman Sea Spreading Centre. The volcanic arc lies just east of the basin. The western margin of this basin seems to be a rifted continental margin, tilted westward flooring the Andaman-Nicobar forearc basin, which was once a part of Malaya Peninsula, suggesting that a significant parts of the Andaman-Nicobar forearc system is underlain by the Sunda continental crust. The Andaman-Nicobar forearc basin is bounded in the west by backthrusts, similar to the West Andaman and Mentawai faults bounding the Aceh and Mentawai forearc basins in the south. The cluster of seismicity after the 2004 great Andaman-Sumatra earthquake just north of Nicobar Island coincides with the intersection of two NW-SE and N-S trending strike-slip fault systems. Some of hypocentre of these earthquakes

  8. Quaternary Deformation of Sumba, Indonesia: Evidence from Carbonate Terraces

    NASA Astrophysics Data System (ADS)

    Dahlquist, M. P.; West, A. J.; Dolan, J. F.

    2014-12-01

    The Banda Arc of Indonesia remains one of the least understood tectonic domains on the modern Earth. The island of Sumba, located approximately 50 km south of Flores and 120 km north of the Java Trench, northwest of where it transitions into the Timor Trough, lies in a region of tectonic transition and potentially offers insights into regional dynamics. The Banda Arc is volcanically active, but Sumba itself is not volcanic. The northern coast of Sumba is covered in Quaternary coral terraces, with the rest of the island's surface geology composed of Mio-pliocene carbonates and uplifted Late Cretaceous-Oligocene forearc basin and volcanic rocks. The purpose of this study is to remotely map the topographic expression of the coral terraces and use the information gained to better understand deformation on Sumba since their deposition. The ages of the coral terraces, of which many platforms are exposed over significant areas of the island, have been constrained at Cape Luandi in north central Sumba, but uplift rates calculated from those ages may not be representative of the island as a whole. The lateral continuity of these dated terraces can help constrain the extent to which uplift of Sumba is spatially variable. Analysis of the terraces using SRTM digital elevation data with ArcGIS software makes it possible to trace the same terrace platforms over large distances, and shows that the north central part of the island has experienced the most uplift since the deposition of the terraces, forming an anticline with the east limb dipping more steeply than the west. The terraces are not well preserved on the southern half of the island. Exposure of older rocks and lack of terrace preservation, as well as a south-skewed drainage divide suggests the southern half of the island experiences greater exhumation, but this could be driven by climate or other factors and does not necessarily indicate more rapid uplift. Study of Quaternary deformation of Sumba can offer greater

  9. Inelastic yielding and forebulge shape across a modern foreland basin: North West Shelf of Australia, Timor Sea

    NASA Astrophysics Data System (ADS)

    Lorenzo, Juan M.; O'Brien, Geoffrey W.; Stewart, Jonathan; Tandon, Kush

    The Timor Trough is a modern ‘underfilled’ foreland basin created by partial subduction of the outer north west continental shelf of Australia beneath Timor Island in the Outer Banda Arc of eastern Indonesia during the Cenozoic. A change of the effective elastic thickness (EET) of the continental foreland lithosphere from ˜80±20 km to ˜25 km over a distance of ˜300 km explains (1) the high curvature (˜10-7 m-1) on the outer Trough wall, (2) the low shelf forebulge (˜200 m) as measured along a reference base Pliocene unconformity, and (3) observed gravity. An inelastically yielding quartzite-quartz-diorite-dunite continental rheology can explain the EET gradient. New, shallow crustal (<8 km), seismic reflection images indicate that Jurassic basement normal faults are reactivated during bending of the foreland.

  10. Postcollision extension in arc-continent collision zones, eastern Indonesia

    NASA Astrophysics Data System (ADS)

    Charlton, T. R.

    1991-01-01

    Postcollisional extension superimposed on arc-continent collision complexes is a common feature in the orogenic belts of eastern Indonesia. In the southern Banda arc, the arc-continent collision event is essentially a Pliocene and younger feature, but already an element of extension is being superimposed on the compressional structures of the collision complex. It is thus likely that the extension commences within a very short period (<5 m.y.) after the initiation of collision-related compressional deformation. A similar history of fold-belt development immediately followed by extension can be inferred for the Lengguru fold belt and the adjacent Wandamen-Wondiwoi terranes of Irian Jaya and for the Gulf of Bone in Sulawesi. It is suggested that the extension results from decoupling of the subducting oceanic lithosphere from the unsubductable continental lithosphere and that the superimposition of extension is a virtually unavoidable consequence of the arc-continent collision.

  11. The rise and fall of an arc-continent collisional orogen: insights from synorogenic sediments in Timor Leste

    NASA Astrophysics Data System (ADS)

    Duffy, B. G.; Quigley, M.; Nguyen, N.; Shulmeister, J.

    2011-12-01

    The island of Timor consists in part of synorogenic, late Miocene to Pleistocene mid-bathyal marine sequences that record structural, sedimentological, and palynological aspects of the collision between the northern Australian continental shelf and the Banda arc. Structural analysis of these sediments in the Viqueque, Laleia and Marobo Basins of Timor Leste reveals that the post-collisional phase is dominated by extensional and strike slip deformation related to the interplay between topographic and buoyancy forces and a dynamically evolving tectonic stress field. Sedimentological and palynological data combined with U-Pb dating of detrital corals provide temporal constraints on the topographic evolution and aerial emergence of the source region. Rapid Pliocene to Holocene uplift is driven primarily by the regional buoyant rebound of crustal lithosphere in response to slab delamination, rather than by crustal thickening alone.

  12. Estudio de la galaxia peculiar NGC 1487

    NASA Astrophysics Data System (ADS)

    Agüero, E. L.; Paolantonio, S.; Gunthardt, G.

    La galaxia peculiar NGC 1487, cuya morfología sugiere un evento de ``merging" o interacción próxima, es estudiada en base a material observacional espectroscópico y fotométrico obtenido en el CASLEO. Mediante técnicas espectrofotométricas standards se determinan las principales características espectrales, los mecanismos de excitación actuantes, las condiciones físicas y las velocidades radiales de las estructuras conspicuas de la galaxia. Por otra parte, usando imágenes directas en las bandas B, V, R e I, se obtienen distribuciones detalladas de los colores B-V, V-R y R-I y detalles de su morfología.

  13. Preliminary study on detection sediment contamination in soil affected by the Indian Ocean giant tsunami 2004 in Aceh, Indonesia using laser-induced breakdown spectroscopy (LIBS)

    NASA Astrophysics Data System (ADS)

    Idris, Nasrullah; Ramli, Muliadi; Hedwig, Rinda; Lie, Zener Sukra; Kurniawan, Koo Hendrik

    2016-03-01

    This work is intended to asses the capability of LIBS for the detection of the tsunami sediment contamination in soil. LIBS apparatus used in this work consist of a laser system and an optical multichannel analyzer (OMA) system. The soil sample was collected from in Banda Aceh City, Aceh, Indonesia, the most affected region by the giant Indian Ocean tsunami 2004. The laser beam was focused onto surface of the soil pellet using a focusing lens to produce luminous plasma. The experiment was conducted under air as surrounding gas at 1 atmosphere. The emission spectral lines from the plasma were detected by the OMA system. It was found that metal including heavy metals can surely be detected, thus implying the potent of LIBS technique as a fast screening tools of tsunami sediment contamination.

  14. Tsunami Research driven by Survivor Observations: Sumatra 2004, Tohoku 2011 and the Lituya Bay Landslide (Plinius Medal Lecture)

    NASA Astrophysics Data System (ADS)

    Fritz, Hermann M.

    2014-05-01

    The 10th anniversary of the 2004 Indian Ocean tsunami recalls the advent of tsunami video recordings by eyewitnesses. The tsunami of December 26, 2004 severely affected Banda Aceh along the North tip of Sumatra (Indonesia) at a distance of 250 km from the epicenter of the Magnitude 9.0 earthquake. The tsunami flow velocity analysis focused on two survivor videos recorded within Banda Aceh more than 3km from the open ocean. The exact locations of the tsunami eyewitness video recordings were revisited to record camera calibration ground control points. The motion of the camera during the recordings was determined. The individual video images were rectified with a direct linear transformation (DLT). Finally a cross-correlation based particle image velocimetry (PIV) analysis was applied to the rectified video images to determine instantaneous tsunami flow velocity fields. The measured overland tsunami flow velocities were within the range of 2 to 5 m/s in downtown Banda Aceh, Indonesia. The March 11, 2011, magnitude Mw 9.0 earthquake off the coast of Japan caused catastrophic damage and loss of life. Fortunately many survivors at evacuation sites recorded countless tsunami videos with unprecedented spatial and temporal coverage. Numerous tsunami reconnaissance trips were conducted in Japan. This report focuses on the surveys at selected tsunami eyewitness video recording locations along Japan's Sanriku coast and the subsequent tsunami video image analysis. Locations with high quality survivor videos were visited, eyewitnesses interviewed and detailed site topography scanned with a terrestrial laser scanner (TLS). The analysis of the tsunami videos followed the four step procedure developed for the analysis of 2004 Indian Ocean tsunami videos at Banda Aceh. Tsunami currents up to 11 m/s were measured in Kesennuma Bay making navigation impossible. Further tsunami height and runup hydrographs are derived from the videos to discuss the complex effects of coastal structures

  15. Fotometría de grupos compactos de galaxias: Shakhbazian 37, 45, 166, 331 y 362

    NASA Astrophysics Data System (ADS)

    Campos, J. M.; Calderón, J. H.; Gimeno, N. G.; Díaz, R. J.

    Continuando con la fotometría CCD de Grupos de Galaxias Compactos de Shakhbazyan (SCGG) en este trabajo se presentan nuevos resultados preliminares sobre los grupos Shakbazyan 37, 45, 166, 331 y 362. EL objeto del proyecto es contribuir al estudio de las propiedades físicas de tales grupos y contribuir a las bases de datos para mejora de las estadísticas. Los datos fueron adquiridos con el Telescopio JKT del Observatorio Norte Europeo. El análisis de las imágenes en las bandas I y B como del índice de color B-I permitió reidentificar las galaxias catalogadas, resultando las mismas muy enrojecidas y verificando que predominan las galaxias tempranas, resultados consistentes con los obtenidos para otros grupos y por otros autores.

  16. Modelling the Shallow Water Equations in Curvilinear Coordinates with Physical Application

    SciTech Connect

    Wingenter, Suzanne

    2005-01-12

    The goal of this project is to provide the capability for simulating fluid flow on complicated geometries, such as in the Bahia de Todos Santos. The Bahia de Todos Santos is a bay situated in the northwest corner of Mexico, off the coast of Ensenada and south of San Diego, California, USA. Figure 1.1 shows the Bahia de Todos Santos. It is part of an image taken from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensors on the Aqua and Terra satellites in late June and early July 2003 [8]. Roughly 200 square kilometers in size, the bay also contains two islands off the peninsula of Punta Banda. Characteristics of flow in this bay are driven by the moon tide (M2) and wind forcing [9].

  17. Volcano hazard mitigation program in Indonesia

    USGS Publications Warehouse

    Sudradjat, A.

    1990-01-01

    Volcanological investigations in Indonesia were started in the 18th century, when Valentijn in 1726 prepared a chronological report of the eruption of Banda Api volcno, Maluku. Modern and intensive volcanological studies did not begin until the catastrophic eruption of Kelut volcano, East Java, in 1919. The eruption took 5,011 lives and destroyed thousands of acres of coffee plantation. An eruption lahar generated by the crater lake water mixed with volcanic eruptions products was the cause of death for a high number of victims. An effort to mitigate the danger from volcanic eruption was first initiated in 1921 by constructing a tunnel to drain the crater lake water of Kelut volcano. At the same time a Volcanological Survey was established by the government with the responsibility of seeking every means for minimizing the hazard caused by volcanic eruption. 

  18. Seismicity studies at Moluccas area based on the result of hypocenter relocation using HypoDD

    SciTech Connect

    Utama, Muhammad Reza July; Nugraha, Andri Dian; Puspito, Nanang T.

    2015-04-24

    The precise hypocenter was determined location using double difference method around subduction zone in Moluccas area eastern part of Indonesia. The initial hypocenter location from MCGA data catalogue of 1,945 earthquake events. Basically the principle of double-difference algorithm assumes if the distance between two earthquake hypocenter distribution is very small compared to the distance between the station to the earthquake source, the ray path can be considered close to both earthquakes. The results show the initial earthquakes with a certain depth (fix depth 10 km) relocated and can be interpreted more reliable in term of seismicity and geological setting. The relocation of the intra slab earthquakes beneath Banda Arc are also clearly observed down to depth of about 400 km. The precise relocated hypocenter will give invaluable seismicity information for other seismological and tectonic studies especially for seismic hazard analysis in this region.

  19. The role of the New Guinea cross-equatorial flow in the interannual variability of the western North Pacific summer monsoon

    NASA Astrophysics Data System (ADS)

    Lin, Yu-Wei; LinHo; Chou, Chia

    2014-04-01

    The western North Pacific (WNP) monsoon trough from 1958 to 2001 shows a binary-like feature in August and September, with more than half being either an imposing presence or a total absence. One of the major moisture sources maintaining the WNP monsoon trough is the low-level moisture advection laterally driven by the low-level cross-equatorial flow that originates from the Banda Sea and Solomon Sea. By decomposing contributions to the cross-equatorial flow based on the method proposed by Back and Bretherton in 2009, the boundary-layer pressure gradient in the Maritime Continent plays a major role. This pressure gradient is further found to be associated with the densely packed sea surface temperature (SST) gradient near the equator around New Guinea, which is well correlated with the SST anomalies in the equatorial eastern Pacific, a concurrent El Niño/Southern Oscillation (ENSO) condition.

  20. Geological evolution and analysis of confirmed or suspected gas hydrate localities

    SciTech Connect

    Finley, P.D.; Krason, J.

    1989-10-01

    Geological factors controlling the formation, stability, and distribution of gas hydrates in the Timor Trough region were investigated by basin analysis. Geological, geophysical, and geochemical data from the region were assembled and evaluated to determine the relationships of geological environments and gas hydrates. The Timor Trough is located between the Indonesian island of Timor and the northwest margin of Australia. The floor of the Timor Trough is 1800 m to 3400 m deep and ranges in width from 3 to 20 km. The trough extends for about 600 km. The Timor Trough is part of the Banda Arc system; it is bounded to the west by the Java Trench and the Aru Basin to the east. 36 refs., 26 figs., 2 tabs.

  1. Mud volcanoes, shale diapirs, wrench faults, and melanges in accretionary complexes, eastern Indonesia

    SciTech Connect

    Barber, A.J.; Tjokrosapoetro, S.; Charlton, T.R.

    1986-11-01

    In Timor, eastern Indonesia, where the northern margin of the Australian continent is colliding with the Banda Arc, Australian continental margin sediments are being incorporated into an imbricate wedge, which passes northward into a foreland fold and thrust belt. Field mapping in Timor has shown that scale clays, containing irregularly shaped or phacoidal blocks (up to several meters long) and composed of a wide range of lithologies derived from local stratigraphic units, occur in three environments: along wrench faults, as crosscutting shale diapirs, and associated with mud volcanoes. A model is proposed linking these phenomena. Shales become overpressured as a result of overthrusting; this overpressure is released along vertical wrench faults, which cut through the overthrust units; overpressured shales containing blocks of consolidated units rise along the fault zones as shale diapirs; and escaping water, oil, and gas construct mud volcanoes at the surface. 6 figures, 1 table.

  2. Classification of earthquake site effects by shallow reflection seismics using a shear-wave land-streamer system

    NASA Astrophysics Data System (ADS)

    Polom, U.; Arsyad, I.; Wiyono, S.; Krawczyk, C. M.

    2007-12-01

    Touched in the SW by the Great Sumatra Fault, the densely populated delta of the Krueng Aceh River consists mainly of young alluvial sediments of clay, sand and gravel with partially high organic content. The depth of this sediment body and its internal structure are widely unknown. Whereas traditional timber constructed buildings are mostly unaffected by strong earthquakes, the change to concrete building techniques added a significant new and locally unknown seismic risk in this region. The classification of earthquake site effects in the city of Banda Aceh and the surrounding region of Aceh Besar was the aim of a high-resolution shear-wave reflection seismic survey in the Indonesian province Nanggroe Aceh Darussalam. In cooperation with the Government of Indonesia and local counterparts, this was part of the Project "Management of Georisk" of the Federal Institute for Geosciences and Natural Resources. Using shear-wave reflection seismics in combination with a land streamer has proven to be an enormously useful method in the sedimentary regions of the Aceh province with an easy and fast recording operation. In addition, the specialized seismic system accounts for compacted soil surfaces which allows a wide range of applications within cities, industrial sites, paved roads and also on small dirt roads. Using a vibrator seismic source, this technique was applied successfully also in areas of high building density in the city of Banda Aceh or in the surrounding mostly agricultural environment. Combined with standard geoengineering investigations like cone penetrometer tests, it was possible to evaluate the soil stiffness in populated urban areas down to 100 m depth in terms of the IBC2003. This is important for the exploration of new areas for save building foundation and groundwater aquifer detection in the tsunami-flooded region.

  3. Aplicación de la metodología Molecular de Orbitales de Defecto Cuántico (MQDO) al cálculo de intensidades vibrónicas y vidas medias de niveles vibracionales

    NASA Astrophysics Data System (ADS)

    María Velasco Sanz, Ana

    Desde que se formuló, en 1996, la metodología Molecular de Orbitales de Defecto Cuántico (MQDO) [1], se han obtenido datos de calidad relativos a intensidades de bandas electrónicas que implican estados Rydberg para una gran variedad de sistemas moleculares [2]. Animados por los buenos resultados obtenidos, recientemente hemos abordado el estudio de transiciones vibrónicas, es decir aquellas que ocurren entre estados vibracionales que pertenecen a distintos estados Rydberg electrónicos. Como prototipo adecuado para nuestros propósitos hemos elegido la molécula de NO, importante en la química de la atmósfera, y para la cual existen en la bibliografía datos experimentales de calidad suficiente para contrastar la validez de nuestros resultados. En concreto, hemos calculado las fuerzas de oscilador y coeficientes de Einstein para transiciones electrónicas y vibrónicas de las principales bandas del NO, al igual que vidas medias radiativas de niveles vibracionales de dicha molécula. Las propiedades estudiadas son esenciales para la comprensión de los aspectos teóricos de los procesos físicos básicos relativos a la dispersión electrónica en moléculas heteronucleares con capas abiertas. Además, valores fiables de probabilidades de transición moleculares tienen importantes aplicaciones en Astrofísica, en la modelización de procesos fotodinámicos moleculares, etc., al igual que para evaluar más profundamente la validez de nuestra metodología teórica.

  4. Fotometria WHBY |o lll|/HB de Regiones H 11 Y la HISTORIA de la Formacion ESTELAR Reciente EN la PEQUENA NUBE de Magallanes

    NASA Astrophysics Data System (ADS)

    Copetti, M. V. F.; Dottori, H. A.

    1987-05-01

    El ancho equivalente WHβ de la linea de Hβ en emisión y la razón [0 III]/Hβ del par λλ4959, 50 7 A del [0111], fueron medidos en 23 regiones HII de la Peque˜a Nube de Magallanes, por medio de la fotometría fotoeléctrica a través de un sistema de tres filtros interferenciales: dos Hβ , con bandas pasantes de 100 y 30 A, y un [0111] centrado en 5000 A y con banda pasante de 50 A. Las observaciones fueron realizadas con los telescopios de 1.60-m y 0.60-m del Laboratorio Nacional de Astrofísica, Brasópolis, Brasil. Fueron escogidos diafragmas suficientemente grandes para captar la radiación integrada de cada región HII. Las medidas fueron calibradas por comparación a un conjunto de nebulosas planetarias con flujos absolutos bien definidos. A través de la comparación entre los datos observacionales y modelos evolutivos de WHβ y [0 III] /Hβ (Copetti et al.1986', Astr. and Ap., 156, 111), las edades de las regiones HIl fueron estimadas. Basada en la distribución espacial de las edades de regiones HIl, la historia de la formación estelar reciente en la Pequeña Nube de Magallanes es analizada. La similitud de las medidas de WH&beta y [OIII]/WHβ entre las regiones H II observadas sugiere que hubo una explosión de formación estelar a 4±1 x106 años en la Pequeña Nube de Magallanes. (Parcialmente financiado por CNPq).

  5. Flyway-scale variation in plasma triglyceride levels as an index of refueling rate in spring-migrating western sandpipers (Calidris mauri)

    USGS Publications Warehouse

    Williams, T.D.; Warnock, N.; Takekawa, J.Y.; Bishop, M.A.

    2007-01-01

    We combined radiotelemetry, plasma metabolite analyses, and macro-invertebrate prey sampling to investigate variation in putative fattening rates (estimated as plasma triglyceride levels) at the flyway scale in Western Sandpipers (Calidris mauri) migrating between Punta Banda, Mexico (31??N), and Hartney Bay, Alaska (60??N), a distance of 4,240 km. Birds were caught at a wintering site (San Francisco Bay) and eight stopover sites along this Pacific Flyway. Body mass was higher in females than in males at six sites, but variation was not correlated with latitude for either sex, and the relationship of change in mass by date within sites was uninformative with regard to possible latitudinal variation in fattening rates. At San Francisco Bay, triglyceride levels were higher in the spring than in the winter. Mean plasma triglyceride varied among stopover sites, and there was a significant linear trend of increasing triglyceride levels with latitude as birds migrated north. At San Francisco Bay, length of stay was negatively related to triglyceride levels. However, plasma triglyceride levels at wintering or initial stopover sites (San Francisco and Punta Banda) did not predict individual variation in subsequent rates of travel during migration. We found no significant relationship between triglyceride levels and prey biomass at different stopover sites, which suggests that the latitudinal pattern is not explained by latitudinal changes in food availability. Rather, we suggest that differences in physiology of migratory birds at southern versus northern stopover sites or behavioral differences may allow birds to sustain higher fattening rates closer to the breeding grounds. ?? The American Ornithologists' Union, 2007.

  6. World Encircling Tectonic Vortex Street - Geostreams Revisited: The Southern Ring Current EM Plasma-Tectonic Coupling in the Western Pacific Rim

    NASA Astrophysics Data System (ADS)

    Leybourne, Bruce; Smoot, Christian; Longhinos, Biju

    2014-05-01

    Interplanetary Magnetic Field (IMF) coupling to south polar magnetic ring currents transfers induction energy to the Southern Geostream ringing Antarctica and underlying its encircling mid-ocean ridge structure. Magnetic reconnection between the southward interplanetary magnetic field and the magnetic field of the earth is the primary energy transfer mechanism between the solar wind and the magnetosphere. Induced telluric currents focused within joule spikes along Geostreams heat the southern Pacific. Alignment of the Australian Antarctic Discordance to other tectonic vortexes along the Western Pacific Rim, provide electrical connections to Earths core that modulate global telluric currents. The Banda Sea Triple Junction, a mantle vortex north of Australia, and the Lake Baikal Continental Rift vortex in the northern hemisphere modulate atmospheric Jetstream patterns gravitationally linked to internal density oscillations induced by these telluric currents. These telluric currents are driven by solar magnetic power, rotation and orbital dynamics. A solar rotation 40 day power spectrum in polarity controls north-south migration of earthquakes along the Western Pacific Rim and manifest as the Madden Julian Oscillation a well-documented climate cycle. Solar plasma turbulence cycles related to Hale flares trigger El Nino Southern Oscillations (ENSO's), while solar magnetic field strength frequencies dominate global warming and cooling trends indexed to the Pacific Decadal Oscillation. These Pacific climate anomalies are solar-electro-tectonically modulated via coupling to tropical geostream vortex streets. Particularly the section along the Central Pacific Megatrend connecting the Banda Sea Triple Junction (up welling mantle vortex) north of Australia with the Easter Island & Juan Fernandez twin rotating micro-plates (twin down welling mantle vortexes) along the East Pacific Rise modulating ENSO. Solar eruptions also enhance the equatorial ring current located

  7. GNSS Tsunami Warning System Augmentation for the Indo-Pacific Region

    NASA Astrophysics Data System (ADS)

    LaBrecque, J. L.

    2015-12-01

    The years since the devastating Banda Aceh Earthquake of December, 2004 have repeatedly inflicted the terrible loss of life and economic disruption from large earthquakes and resulting tsunamis upon Indo-Pacific coastal populations. The hardest hit populations are those closest to the earthquake source, a scenario for which most Indo-Pacific nations lack an adequate early warning system. Following the Banda Aceh Earthquake, GNSS based techniques were developed to provide accurate, timely, estimates of ground displacements, the modeling and monitoring of tsunami propagation. Major investments are also being made to deploy and upgrade existing GNSS constellations (GPS, GLONASS, Beidou, Galileo, GZSS, and IRNSS) by the end of this decade. There have also been significant investments in multi-GNSS ground networks and analysis centers that often provide measurements in real time. These multi-national investments now present the possibility for significant improvements to the Indo-Pacific region's tsunami warning. The development of GNSS based tsunami warning integrated with existing seismic based tsunami warning systems will provide a robust, accurate, timely, and cost effective network to provide effective warning for the Indo-Pacific coastal communities. The UN General Assembly has called for the sharing of geodetic data for the mitigation of natural hazards while the IUGG and IGS recommend the implementation of a GNSS based augmentation to the Tsunami Early Warning System. The same GNSS ground networks and constellations that support the Tsunami Early Warning network also provide Positioning, Navigation, and Timing and other benefits to these communities thereby insuring a sustainable and reliable capability.

  8. Modeling the effect of forest restoration scenarios on runoff through a reanalysis of historical experimental watershed data

    NASA Astrophysics Data System (ADS)

    O'Donnell, F. C.; Springer, A. E.; Masek Lopez, S.; Sanchez Meador, A.

    2013-12-01

    Since the settlement of the American Southwest, the ponderosa pine and mixed conifer forests of the Arizona highlands have increased in density due to fire suppression, recovery from logging, and livestock grazing. The landscape-scale Collaborative Forest Restoration Program project known as the Four Forest Restoration Initiative (4FRI) has been proposed to reduce forest density and restore a more natural fire cycle over large areas of the region. Expected benefits include a reduced risk of high-intensity wildfire, improved wildlife habitat, increased forest resiliency to drought and infestation, improved wildlife habitat, and increased water yield. There is considerable interest in restoration effects on water yield because the forests contribute a large portion of the runoff to the Salt River, which supplies water to the Phoenix metropolitan area. While empirical data on the effects of restoration on streamflow are limited, paired watershed studies conducted in the 1950's-80's at a number of historic research sites in the region provide robust datasets that tested how a range of silvicultural techniques influence runoff. The study sites included the Beaver Creek Experimental Watershed, Workman Creek in the Sierra Ancha Experimental Forest, and two sites in the White Mountains of eastern Arizona. We synthesized the data from these studies to develop an improved regression model that predicts annual runoff increase following a forest thinning based on basal area, time since treatment, climate, and physical characteristics of the watershed. We used the model to predict the increase in runoff due to forest thinning for a small watershed that is part of the proposed treatment area from 2014 to 2050. We considered three management scenarios: no thinning, the proposed 4FRI thinning prescription, and a more intense thinning that reduces basal area to pre-settlement conditions. Our model is based on trajectories of forest recovery dynamics for each scenario produced by

  9. Physical Properties of the SKYLAB North Polar Coronal Hole with an Extended Base and its MHD Self-Consistent Modelling

    NASA Astrophysics Data System (ADS)

    Bravo, S.; Ocania, G.

    1991-04-01

    RESUMEN Con base en las observaciones del Skylab del Sol en rayos X que permitieron r la forma de la frontera del hoyo coronal del polo norte y en las observaciones de l 'z que permitieron derivar un perfil de densidad para el flujo de viento solar (IC ese hoyo, Murno yjackson (1977) concluyeron que se requiere una adici6n t l clc energfa al flujo hasta al menos 5 R8. En este trabajo, recalculamos los perfiles de y de temperatura para el mismo hoyo pero considerando una frontera Cs mas ancha en la base, de acuerdo con las observaciones del coron6metro-K del IIAO, los espectroheliogramas en EUV del OSO-7 y las fotografias de la corona solar cerca de los 4 E)()O A. Se tomaron tambien las incertidumbres en el perfil de densidad electr6nica inl & a las observaciones de luz blanca y se consideraron diversos valores posibles dCl fl 'jo (lC masa 1 UA. Encontramos que las diferencias introducidas no son suficientes par clcsc' la necesidad de una energetizaci6n extensa del viento solar, pero una dC las s posibles muestra una concordancia muy buena con el modelado MHD (l( l flujo con el unico t6rmino adicional de la fuerza de Lorentz en la ecuaci6n de # (). ABSTRACT Based on the near to the Sun boundary of the Skylab north polar coroi ' l estimated from the AS & E X-ray photographs and on the density profile fi-C)I white light data, Munro and Jackson (1977) concluded that substantial energy the solar wind flux is required up to at least 5 Rs. In this paper we recalculate `eloci y and temperature profiles for the same hole but considering a different bo ' ry for flux tube which is larger at its base, according to the HAO K- obser"' (i()I0 , the OSO-7 EUV spectroheliograms and pictures of the solar 4500 A. è take into account the uncertainties inherent in the white light observations () electron density profile and consider different possible values of the solar I .' fltix at 1 AU. We that the differences introduced are not sufficient to discard ii y of an extended

  10. Hydrochemical controls on aragonite versus calcite precipitation in cave dripwaters

    NASA Astrophysics Data System (ADS)

    Rossi, Carlos; Lozano, Rafael P.

    2016-11-01

    Despite the paleoclimatic relevance of primary calcite to aragonite transitions in stalagmites, the relative role of fluid Mg/Ca ratio, supersaturation and CO32- concentration in controlling such transitions is still incompletely understood. Accordingly, we have monitored the hydrochemistry of 50 drips and 8 pools that are currently precipitating calcite and/or aragonite in El Soplao and Torca Ancha Caves (N. Spain), investigating the mineralogy and geochemistry of the CaCO3 precipitates on the corresponding natural speleothem surfaces. The data reveal that, apart from possible substrate effects, dripwater Mg/Ca is the only obvious control on CaCO3 polymorphism in the studied stalagmites and pools, where calcite- and aragonite-precipitating dripwaters are separated by an initial (i.e. at stalactite tips) Mg/Ca threshold at ≈1.1 mol/mol. Within the analyzed ranges of pH (8.2-8.6), CO32- concentration (1-6 mg/L), supersaturation (SIaragonite: 0.08-1.08; SIcalcite: 0.23-1.24), drip rate (0.2-81 drops/min) and dissolved Zn (6-90 μg/L), we observe no unequivocal influence of these parameters on CaCO3 mineralogy. Despite the almost complete overlapping supersaturations of calcite- and aragonite-precipitating waters, the latter are on average less supersaturated because the waters having Mg/Ca above ∼1.1 have mostly achieved such high ratios by previously precipitating calcite. Both calcite and aragonite precipitated at or near oxygen isotopic equilibrium, and Mg incorporation into calcite was consistent with literature-based predictions, indicating that in the studied cases CaCO3 precipitation was not significantly influenced by strong kinetic effects. In the studied cases, the calcites that precipitate at ∼11 °C from dripwaters with initial Mg/Ca approaching ∼1.1 incorporate ∼5 mol% MgCO3, close to the published value above which calcite solubility exceeds aragonite solubility, suggesting that aragonite precipitation in high-relative-humidity caves is

  11. Abundancias químicas de ψ Octantis

    NASA Astrophysics Data System (ADS)

    Medina, M. C.; Pintado, O. I.

    Se determinan las abundancias químicas de ψ Oct usando espectros obtenidos con EBASIM en CASLEO. Los valores iniciales de temperatura efectiva y gravedad superficial se calculan con la fotometría uvbyβ. Esta estrella fue estudiada por Pintado y Adelman (1996) usando espectros REOSC y Adelman y otros (1993), este último basado en espectros echelle obtenidos con el Telescopio Anglo Australiano. Comparamos nuestros resultados con los de los trabajos anteriormente mencionados, pudiéndose realizar una evaluación de la calidad de los espectros EBASIM.

  12. Hydrogeology of the Mogollon Highlands, central Arizona

    USGS Publications Warehouse

    Parker, John T.C.; Steinkampf, William C.; Flynn, Marilyn E.

    2005-01-01

    The Mogollon Highlands, 4,855 square miles of rugged, mountainous terrain at the southern edge of the Colorado Plateau in central Arizona, is characterized by a bedrock-dominated hydrologic system that results in an incompletely integrated regional ground-water system, flashy streamflow, and various local water-bearing zones that are sensitive to drought. Increased demand on the water resources of the area as a result of recreational activities and population growth have made necessary an increased understanding of the hydrogeology of the region. The U.S. Geological Survey conducted a study of the geology and hydrology of the region in cooperation with the Arizona Department of Water Resources under the auspices of the Arizona Rural Watershed Initiative, a program launched in 1998 to assist rural areas in dealing with water-resources issues. The study involved the analysis of geologic maps, surface-water and ground-water flow, and water and rock chemical data and spatial relationships to characterize the hydrogeologic framework. The study area includes the southwestern corner of the Colorado Plateau and the Mogollon Rim, which is the eroded edge of the plateau. A 3,000- to 4,000-foot sequence of early to late Paleozoic sedimentary rocks forms the generally south-facing scarp of the Mogollon Rim. The area adjacent to the edge of the Mogollon Rim is an erosional landscape of rolling, step-like terrain exposing Proterozoic metamorphic and granitic rocks. Farther south, the Sierra Ancha and Mazatzal Mountain ranges, which are composed of various Proterozoic rocks, flank an alluvial basin filled with late Cenozoic sediments and volcanic flows. Eight streams with perennial to intermittent to ephemeral flow drain upland regions of the Mogollon Rim and flow into the Salt River on the southern boundary or the Verde River on the western boundary. Ground-water flow paths generally are controlled by large-scale fracture systems or by karst features in carbonate rocks. Stream

  13. Communicating Tsunami Preparedness Through the Lessons Learned by Survivors

    NASA Astrophysics Data System (ADS)

    Kerlow, I.

    2015-12-01

    Often times science communication is reactive and it minimizes the perceptions of the general public. The Tsunami of New Dreams is a film with the testimonies of survivors of the 2004 Indian Ocean tsunami in Banda Aceh and Aceh Besar in West Sumatra, Indonesia. Production of the film spanned over five years and dozens of interviews, and is based on a unique geographic, demographic and experiential sampling of the local population. This documentary feature film underscores the importance of Earth science and science communication in building sustainable communities. The film is a lesson in survival and sustainability, and it provides a simple but powerful testimony of what to do and what not to do before and during a tsunami. The film also highlights the direct relationship that exists between disaster survival rates and the knowledge of basic Earth science and preparedness facts. We hope that the human stories presented in the film will serve as a strong motivator for general audiences to learn about natural hazards, preparedness, and Earth science. These engaging narratives can touch the minds and hearts of general audiences much faster than technical lectures in a classroom. Some of the testimonies are happy and others are sad, but they all present the wide range of beliefs that influenced the outcomes of the natural disaster. The interviews with survivors are complemented with unique archival footage of the tsunami and unique footage of daily life in Aceh. Hand-drawn illustrations are used to recreate what survivors did immediately after the earthquake, and during the extreme moments when they faced the tsunami waves. Animated visuals, maps and diagrams enhance the understanding of earthquake and tsunami dynamics. The film is a production of the Earth Observatory of Singapore (EOS) in collaboration with the International Center for Aceh and Indian Ocean Studies (ICAIOS) in Banda Aceh, Indonesia. The film is scheduled for release in late 2015. This is a unique

  14. Observações simultâneas no óptico e infravermelho próximo dos BL Lacs PKS 2005-489 e PKS 2155-304 em diversas escalas de tempo

    NASA Astrophysics Data System (ADS)

    Dominici, T. P.; Abraham, Z.; Galo, A. L.

    2003-08-01

    A existência de variações rápidas de brilho em alguns blazares é um fenômeno bem comprovado, mas até agora não sabemos ao certo quais são os mecanismos físicos envolvidos. A maior dificuldade é a ausência de observações multibanda simultâneas que poderiam fornecer vínculos aos modelos. Buscando colaborar com a discussão estudamos o comportamento de dois BL Lacs, PKS 2005-489 e PKS 2155-304, em relação à variabilidade em diversas escalas de tempo, de poucos minutos até vários meses, com observações simultâneas em seis bandas espectrais (óptico e infravermelho próximo). Para tanto dois telescópios do LNA foram utilizados em conjunto nas campanhas observacionais realizadas em 2001 e 2002, cujos resultados são apresentados aqui. As duas fontes apresentaram características bastante diferentes, inclusive em relação à existência de variabilidade nos índices espectrais. Particularmente, registramos a primeira detecção de variações em escalas de tempo da ordem de poucos minutos em PKS 2005-489, com evidências da presença de um atraso entre as curvas de luz nas bandas V e R e a variação em R ocorrendo antes (o contrário do esperado no modelo de shock-in-jet). Em PKS 2155-304 detectamos pela primeira vez variabilidade em escalas de tempo de poucos minutos no infravermelho em um AGN. As observações indicam que as variações de brilho em blazares são o resultado da ação de mais de um fenômeno, especialmente em escalas de tempo muito curtas. Alguns cenários físicos são sugeridos para explicar os resultados observacionais.

  15. In-Situ Estimates of tidal mixing in the Indonesian archipelago from multidisciplinary data

    NASA Astrophysics Data System (ADS)

    Koch-Larrouy, Ariane; Atmadipoera, Agus; van Beek, Pieter; Madec, Gurvan; Aucan, Jerome; Lyard, Florent; Grelet, Jacques; Souhaut, Marc

    2015-04-01

    The Indonesian Mixing program (INDOMIX) was designed to quantify the very strong mixing that transforms Pacific waters into homohaline Indonesian Waters in the Indonesian archipelago. The turbulent dissipation rates and associated mixing were estimated and analyzed using a multidisciplinary approach that combines physical and geochemical observations: 1) direct measurements of the dissipation using a microstructure profiler, 2) use of density-based fine-scale methods, and 3) study of the vertical distribution of natural radionuclides (radium isotopes and actinium-227). Data were collected at five contrasting stations within the Indonesian archipelago. Strong instabilities, inversions of the density profiles and a very strong water mass transformation were observed. A wide range of values is obtained for dissipation within [10-10, 10-4] W.kg-1 with spots of higher dissipation in the ocean interior correlated with a strong internal tide signal. Both Fine-scale and micro-scale methods allow us to identify very strong dissipation energy levels above the straits, ranging within [10-7, 10-4] W.kg-1, in contrast to lower values at stations far from generation sites. However, the dissipation in the interior water column for the station located in the center of Halmahera [10-9, 10-8] W.kg-1 is stronger than for the Banda station [10-11, 10-10] W.kg-1, which is further away from generation sites. The three approaches agree relatively well and provide Kz values ranging between 5 10-4 and 5 10-1 m2.s-1, except in the Banda Sea where values are similar to the ones found in the open ocean (10-6 m2.s-1). Kz values mainly increase toward the bottom, where stratification decreases. Surface mixing, at the base of the mixed layer is found to be still very strong with values within [10-4, 10-3 m2.s-1]. These results confirm the results of modelling studies, in which hypothesis of intensified subsurface mixing were made, a mixing that strongly modifies the whole tropical mean state and

  16. Pliocene obducted, rotated and migrated ultramafic rocks and obduction-induced anatectic granite, SW Seram and Ambon, Eastern Indonesia

    NASA Astrophysics Data System (ADS)

    Linthout, Kees; Helmers, Hendrik

    Geochemistry, petrography and thermobarometry of the ultramafic and associated rocks of SW Seram and Ambon indicate that they were obducted as weakly depleted oceanic lithosphere which was formed about 10 Ma prior to obduction. Occurrences of cordierite-bearing granite are closely associated with the ultramafic rocks. Petrography and geochemical analysis based on major, RE and other trace elements, indicate that the granite is of the S-type, containing a significant restite component; a VAG signal is interpreted as inherited from the partly melted and included Palaeozoic metasediments. The granite magma was formed as a consequence of the obduction of very hot mantle peridotite inflicting high-grade metamorphism and partial anatexis on the Palaeozoic continental substratum. The oldest age in the literature for cordierite-bearing dacite, connected to this partial anatexis, sets the minimum age of the obduction event at 4.4 Ma. The obduction took place at the eastern end of the Banda Arc, near the NE margin of the Weber Deep, where SW Seram must have been at that time. The ophiolite as part of the Buru-Seram Microplate, rotated and migrated about 400 km westward to its present position. Since the Early Pliocene, the rate of upheaval in Kaibobo (SW Seram) has averaged about 260 cm Ka -1, but may well have been over 1000 cm Ka -1 in the early period immediately after the formation of the granite melt. As the average uplift rate over the same period for Central Seram was previously estimated at 110 cm Ka -1, strongly differential upheaval prevailed in Seram in the Early Pliocene. It is postulated that young oceanic lithosphere has been created by transtensional pull-apart in the easternmost part of the Banda Sea Plate due to oblique convergence of the northward moving Australian Plate, of which fragments gradually became incorporated in the regime of the westbound SW Pacific Plates. Obduction was effected during the strong Pliocene rotation of the Buru-Seram Microplate

  17. Urban shear-wave reflection seismics: Reconstruction support by combined shallow seismic and engineering geology investigations

    NASA Astrophysics Data System (ADS)

    Polom, U.; Guenther, A.; Arsyad, I.; Wiyono, P.; Krawczyk, C. M.

    2009-12-01

    After the big 2004 Sumatra-Andaman earthquake, the massive reconstruction activities in the Aceh province (Northern Sumatra) were promoted by the Republic of Indonesia and the Federal Ministry of Economic Cooperation and Development. The aims of the project MANGEONAD (Management of Georisk Nanggroe Aceh Darussalam). are to establish geoscientific on the ground support for a sustainable development and management of save building constructions, lifelines, infrastructure and also natural resources. Therefore, shallow shear-wave reflection seismics was applied in close combination to engineering geology investigations in the period between 2005-2009 since depth and internal structure of the Krueng Aceh River delta (mainly young alluvial sediments) were widely unknown. Due to the requirements in the densely populated Banda Aceh region, lacking also traffic infrastructure, a small and lightweight engineering seismic setup of high mobility and high subsurface resolution capability was chosen. The S-wave land streamer system with 48 channels was applied successfully together with the ELVIS vibratory source using S- and P-waves on paved roads within the city of Banda Aceh. The performance of the S-wave system enabled the detailed seismic investigation of the shallow subsurface down to 50-150 m depth generating shaking frequencies between 20 Hz to 200 Hz. This also provides depth information extending the maximum depths of boreholes and Standard Penetrometer Testings (SPT), which could only be applied to max. 20 m depth. To integrate the results gained from all three methods, and further to provide a fast statistical analysis tool for engineering use, the Information System Engineering Geology (ISEG, BGR) was developed. This geospatial information tool includes the seismic data, all borehole information, geotechnical SPT and laboratory results from samples available in the investigation area. Thereby, the geotechnical 3D analysis of the subsurface units is enabled. The

  18. Geochemical and tectonic relationships in the east Indonesian arc-continent collision region: Implications for the subduction of the Australian passive margin

    NASA Astrophysics Data System (ADS)

    van Bergen, M. J.; Vroon, P. Z.; Hoogewerff, J. A.

    1993-07-01

    Van Bergen, M.J., Vroon, P.Z. and Hoogewerff, J.A., 1993. Geochemical and tectonic relationships in the east Indonesian arc-continent collision region: implications for the subduction of the Australian passive margin. In: M.J.R. Wortel, U. Hansen and R. Sabadini (Editors), Relationships between Mantle Processes and Geological Processes at or near The Earth's Surface. Tectonophysics, 223: 97-116. Variations in the isotopic signatures of volcanics along the East Sunda Banda Arc reflect changes in the nature and amount of sedimentary material supplied by the northeast Indian Ocean floor and the adjacent Australian passive continental margin, which form the two major domains of the Indian Ocean plate that approach the arc system. A compilation of isotopic data for 200-500-km-long arc sectors shows that the trend in magmatic signatures follows distinct subduction/collision stages reached by the corresponding oceanic and continental-margin sections entering the trench system. Maximum amounts of magma source contamination are inferred for volcanics near an extinct sector north of Timor, where the Australian continent started to collide with the arc first. Pb-Nd isotopic source mixing models point to contamination by sediments with variations in composition, similar to observed along-arc changes in sediments entering the trench. The results indicate an increasing contribution of subducted continental material in the direction of the collision region. Mass-balance calculations, considering the magmatic output and minimum input of subducted continental material required to generate the composition of the volcanic arc in the collision region, are difficult to reconcile with subduction of ocean-floor sediments alone. Thicknesses of sediments presently covering oceanic crust near the margin are close to calculated thicknesses of the sediments fluxed into the trench and magmatically returned to the arc crust, but cannot account for the additional volumes of material accreted on

  19. Geologic Map of the Albuquerque 30' x 60' Quadrangle, North-Central New Mexico

    USGS Publications Warehouse

    Williams, Paul L.; Cole, James C.

    2007-01-01

    local folding and uplift within the complex rift seems to have occurred in the late Miocene, accompanied by erosion and recycling of earlier rift-fill sediments. This deformation may reflect clockwise reorientation of the primary extension direction to its Pliocene and current east-west alignment. Late Miocene and early Pliocene uplift and erosion were widespread in the region, as indicated by channeled and local angular unconformities at the bases of all Pliocene units, especially prominent along basin margins. These Pliocene fluvial and alluvial deposits (Ceja and Ancha Formations and Tuerto Gravel) and the upper part of the Cochiti Formation are all conspicuously coarser grained than the Miocene beds they cover, particularly near source areas along the margins of the rift. These observations together indicate that the regional streams flowed at much greater discharge than the Miocene streams and that the Pliocene onset of cooler, wetter climate worldwide was the most likely cause. Despite these higher discharge conditions, it appears there was no Pliocene trunk stream through the rift valley because the youngest Pliocene beds in the basin center are largely fine grained sand, pebbly sand, and sandy silt. No Pliocene cobble-gravel deposits, or thick crossbed sets indicative of major stream discharge, have been documented in the basin center. Considerable evidence indicates significant erosion began in late Pliocene time, coincident with and following eruption of abundant basalt from several local centers at about 2.7-2.6 Ma. The onset of central valley erosion marks the initiation of the first through-flowing, high-energy trunk stream (the 'ancestral' Rio Grande), which most likely was caused by integration of drainage southward through the Socorro region. No upper Pliocene fluvial deposits have been identified in the valley center; rather, a significant unconformity separates beds with medial (or earliest late) Blancan fauna (older than about 2.2 Ma) from

  20. [How do the obese persons perceive their overall health?].

    PubMed

    Ríos-Martínez, Blanca P; Rangel-Rodríguez, Gabriela; Pedraza-Moctezuma, Luis G

    2013-01-01

    Objetivo: conocer cómo la persona con obesidad percibe su salud en diferentes áreas de su vida. Métodos: a 224 pacientes con obesidad, se les aplicó el cuestionario SF-36, el cual mide funcionamiento social y físico, salud mental y física, dolor corporal, limitaciones de roles debido a problemas físicos o emocionales, vitalidad y salud general. Se analizaron las diferencias entre los sexos, el tratamiento y el grado de obesidad. Se realizó análisis descriptivo y se aplicó t de Student, Anova y prueba de Tukey Resultados: Las mujeres tuvieron peor funcionamiento social y emocional que los hombres; en cuanto al tipo de tratamiento, los pacientes con derivación gástrica indicaron mayor cansancio que aquellos con banda gástrica y los que tuvieron obesidad mórbida mostraron menor funcionamiento físico, mayor dolor y peor salud general que quienes tenían obesidad. Conclusiones: la mayoría de los pacientes analizados tendió a sentirse cansada, exhausta y con la sensación de que su salud ha sido y seguirá deteriorándose.

  1. Temporal Change of the Earth's Inner Core Boundary beneath North Pacific and Eurasia

    NASA Astrophysics Data System (ADS)

    Yao, J.; Wen, L.

    2015-12-01

    It has been shown that, based on the analysis of changes of seismic compressional waves that are refracted (PKIKP) and reflected (PKiKP) off the inner core, the Earth's inner core surface exhibits temporal change beneath Africa, but no discernible change beneath South America. The temporal change of inner core surface occurs in localized regions, and is episodic, rapidly migrating and alternately enlarged and shrunk in a time scale of years. To better understand the nature of temporal change of inner core boundary, we expand the study of temporal change to the inner core surface beneath North Pacific and Eurasia, using doublets occurring in Kuril Islands and Banda Sea between 1990 and 2015. The doublets are within 1 km of separation of depth and horizontal distance. Seismograms recorded at stations in America and Africa for these doublets show clear PKIKP and PKiKP phases sampling the inner core surface beneath North Pacific and Eurasia. No discernible temporal change of PKiKP or PKIKP is observed in those seismic observations. Superimposed PKiKP-PKIKP waveforms of the doublets also show excellent agreements in both absolute arrival time and differential travel time of the two phases. These observations indicate that the inner core surface beneath Eurasia and North Pacific does not experience any detectable temporal change. In this presentation, we will further summarize the results of temporal change of inner core surface reported so far.

  2. An economical non-destructive method for estimating eelgrass, Zostera marina (Potamogetonaceae) leaf growth rates: formal development and use in northwestern Baja California.

    PubMed

    Solana-Arellano, Elena; Echavarria-Heras, Héctor; Franco-Vizcaíno, Ernesto

    2008-09-01

    Seagrass beds provide much of the primary production in estuaries; host many fishes and fish larvae, and abate erosion. The present study presents original analytical methods for estimating mean leaf-growth rates of eelgrass (Zostera marina). The method was calibrated by using data collected in a Z. marina meadow at Punta Banda estuary in Baja California, Mexico. The analytical assessments were based on measurements of leaf length and standard regression procedures. We present a detailed explanation of the formal procedures involved in the derivation of these analytical methods. The measured daily leaf-growth rate was 10.9 mm d(-1) leaf(-1). The corresponding value projected by our method was 10.2 mm d(-1) leaf(-). The associated standard errors were of 0.53 and 0.56 mm d(-1) leaf(-1) respectively. The method was validated by projecting leaf-growth rates from an independent data set, which gave consistent results. The use of the method to obtain the mean leaf growth rate of a transplanted plot is also illustrated. Comparison of our leaf-growth data with previously reported assessments show the significant forcing of sea-surface temperature on eelgrass leaf dynamics. The formal constructs provided here are of general scope and can be applied to equivalent eelgrass data sets in a straightforward manner. PMID:19419023

  3. A geometria do campo magnético na região da nuvem Lupus 1

    NASA Astrophysics Data System (ADS)

    Alves, F. P.; Franco, G. A. P.

    2003-08-01

    Apresentaremos os resultados de uma investigação polarimétrica na região de formação estelar junto à nuvem escura Lupus 1. Esse estudo baseia-se em polarimétria CCD obtida na banda R, e cobre Lupus 1, bem como a área vizinha a essa nuvem contendo a cavidade em 100 mm IRAS. Os dados observacionais foram coletados com o telescópio IAG de 60 cm do Observatório do Pico dos Dias (LNA/MCT - Brasópolis - MG). Nossa primeira análise mostra que uma variação da orientação do campo magnético através da região pode produzir padrões complexos de polarização cuja geometria do campo não pode ser facilmente determinada. Os padrões de polarização são inconsistentes com um campo magnético estritamente uniforme e unidimensional em larga escala. Comparação com a emissão em 100 mm mostra que localmente os vetores de polarização exibem um forte alinhamento com a orientação dos padrões observados em infravermelho.

  4. En la búsqueda de características en eyecciones coronales de masa que discriminen entre dos paradigmas físicos en modelos de ECMs

    NASA Astrophysics Data System (ADS)

    Paissan, G.; Stenborg, G.; Rovira, M.

    Se conocen tres diferentes fenómenos de gran escala que ocurren en la atmósfera solar, denominados eyecciones coronales de masa (ECMs), protuberancias eruptivas y grandes fulguraciones de dos bandas. Estos fenómenos están estrechamente relacionados y podrían ser distintas manifestaciones de un único proceso físico. Las ECMs son definidas como eyecciones de gran escala de masa y flujo magnético desde la baja corona al espacio interplanetario. Desde su descubrimiento en los '70, muchos modelos han sido propuestos para explicar su origen y evolución. La explicación física de las ECMs es un tema de debate intenso. No obstante, los modelos pueden sintetizarse en dos grandes grupos: 1) los modelos de inyección de flujo y 2) los modelos de almacenamiento y liberación. En este trabajo, se presentan los estudios realizados con una serie de eventos observados con el coronógrafo MICA (Mirror Coronograph for Argentina), el telescopio en H-alfa HASTA (H-alpha Solar Telescope for Argentina) y los coronógrafos C2 y C3 de la sonda SOHO (Solar and Heliospheric Observatory). Los eventos que pudieron ser identificados como ECMs son contrastados dentro del esquema de los dos paradigmas teóricos propuestos.

  5. Australia and Indonesia in collision: geochemical sources of magmatism

    NASA Astrophysics Data System (ADS)

    Elburg, M. A.; Foden, J. D.; van Bergen, M. J.; Zulkarnain, I.

    2005-01-01

    The islands of Alor, Lirang, Wetar and Romang are located in the extinct section of the Sunda-Banda arc, where the collision with the Australian continent has brought subduction to a halt. Intrusive and extrusive igneous samples show a wide range of Sr, Nd and Pb isotopic characteristics. Samples from the northeast coast of Alor extend the trend of increasing 206Pb/ 204Pb ratios along the arc in an easterly direction, with values as high as 19.6. Samples from Alor's south coast, Lirang, Wetar and Romang have appreciably lower 206Pb/ 204Pb ratios (≤19.1), and 143Nd/ 144Nd ratios down to 0.5119. The Pb isotope data are interpreted as reflecting mixing between two internally variable end members within the subducting Australian continent, either the upper and lower crust, or two upper crustal end members of different ages. These melts may come up virtually unmodified, giving rise to the felsic, low 143Nd/ 144Nd samples, or may interact with the mantle, of which the partial melts and the fractionation products thereof give rise to basalts to rhyodacites with more intermediate Nd isotopic characteristics. Mixing modelling of the latter samples' isotopic ratios constrains the amount of crustal material that has been added to the mantle wedge to reach up to 9%. The isotopic and trace element heterogeneity in the samples studied is likely to reflect inhomogeneity of the crustal sources contributing to magmatism.

  6. The evolution of Sumba Island (Indonesia) revisited in the light of new data on the geochronology and geochemistry of the magmatic rocks

    NASA Astrophysics Data System (ADS)

    Abdullah, C. I.; Rampnoux, J.-P.; Bellon, H.; Maury, R. C.; Soeria-Atmadja, R.

    2000-04-01

    The island of Sumba, presently located in the southern row of islands of the Eastern Nusa Tenggara province of Eastern Indonesia, has a unique position, being part of the Sunda-Banda magmatic arc and subduction system. It represents a continental crustal fragment located at the boundary between the Sunda oceanic subduction system and the Australian arc-continent collision system, separating the Savu Basin from the Lombok Basin. New data on magmatic rocks collected from Sumba are presented in this paper, including bulk rock major and trace element chemistry, petrography and whole rock and mineral 40K- 40Ar ages. Three distinct calc-alkaline magmatic episodes have been recorded during Cretaceous-Paleogene, all of them characterized by similar rock assemblages (i.e. pyroclastic rocks, basaltic-andesitic lava flows and granodioritic intrusions). They are: (i) the Santonian-Campanian episode (86-77 Ma) represented by volcanic and plutonic rock exposures in the Masu Complex in Eastern Sumba; (ii) the Maastrichtian-Thanetian episode (71-56 Ma) represented by the volcanic and plutonic units of Sendikari Bay, Tengairi Bay and the Tanadaro Complex in Central Sumba; and (iii) the Lutetian-Rupelian episode (42-31 Ma) of which the products are exposed at Lamboya and Jawila in the western part of Sumba. No Neogene magmatic activity has been recorded.

  7. Sequences and clusterings of significant volcanic eruptions in convergent plate margins during 1900 1980

    NASA Astrophysics Data System (ADS)

    Papadopoulos, G. A.

    1987-07-01

    Magmatic eruptions which lasted at least 15 days and had a Volcanic Explosivity Index ⩾ 1, are defined as significant volcanic eruptions. Data concerning significant eruptions which occurred from 1900 to 1980 show that in seventeen regions of plate convergence which were examined there is a similar time-evolution pattern of the volcanism, namely, periods of frequent volcanic activity with significant eruptions in at least one volcano (usually lasting less than 15 years) alternating with intervals of quiescence lasting from 4.5 to 20 years. Empirical criteria have been applied to classify ordinary periods, sequences, and clusterings of significant eruptions. Taking into account the date of the first eruption on all the volcanoes of a given period of frequent volcanic activity, then, in seven sequences or clusterings occurring in several regions, one may observe a systematic migration of the volcanism along the arc (e.g. in Lesser Sunda-Banda Sea Islands during 1963-1974). A clear positive correlation between the delay-time of the eruptions and the distance of the corresponding volcanoes from the first erupted volcano has been found. It is suggested that large-scale, long-term physical processes in the earth's interior may be responsible for the volcanic activity-volcanic quiescence pattern in plate convergence regions.

  8. Th isotope and U-series studies of subduction-related volcanic rocks

    NASA Astrophysics Data System (ADS)

    Gill, James B.; Williams, Ross W.

    1990-05-01

    The activities of 6-7 radionuclides measured by alpha spectrometry are reported for 35 samples of recent volcanic rocks from 24 volcanoes in 9 arcs. These include continental margins (Cascades, Alaska, Costa Rica), island arcs (the Sunda, Banda, and Sangihe arcs of Indonesia, Marianas, Japan, Aleutians, Antilles, Tonga), and a backarc basin (Lau Basin). Enrichment of 238U over 230Th is more common (over 2/5 of the samples) and greater (up to 59%) in these subduction-related volcanics than in those from other tectonic environments. 230Th /232Th ratios also extend to higher values, both in absolute numbers and relative to other isotope ratios. Enrichment of 210Po and 226Ra over 230Th is widespread and is more common and greater in island arcs than continental margins. The level of Po or Ra enrichment (50-300% in island arcs, 10-50% at continental margins) is similar to that in ocean island and ridge basalts and decreases with differentiation. The differences in Th-U systematics between subduction-related and other volcanic rocks are attributed to variations in the process of melt extraction, changes in bulk partition coefficients within the mantle wedge, or preferential addition of U from subducted lithosphere. Ra enrichments are attributed to partial melting processes which are similar to those at ocean ridges. Smaller excesses at continental margins are attributed either to slower ascent or to differences in the process of melt formation beneath continents.

  9. Isolated deep earthquakes and the fate of subduction in the mantle

    NASA Astrophysics Data System (ADS)

    Lundgren, Paul; Giardini, Domenico

    1994-08-01

    The locations of earthquakes with depth in the mantle provide direct evidence of the trajectory and state of stress of subducting lithosphere. The occurrence over the last decade of isolated large deep earthquakes outside the main Wadati-Benioff zones in the Kurile, Izu-Bonin, and Chile deep seismic areas (in addition to the observed flat distributions of deep seismicity beneath the Banda Sea and Fiji Plateau areas and the large number of deep earthquakes located away from the main slab in the Tonga arc) supports recent tomographic and other seismological studies, leading to a reconsideration of slabs as simple planar structures sinking undeformed into the lower mantle. The focal geometries of these isolated earthquakes, which often exhibit near vertical compressional stresses, are distinct from adjacent events in the main Wadati-Benioff zone. They are also different in orientation from events in the deflecting toe of the slab and from the stress orientation expected if the deflected slab acts as a stress guide. These isolated mantle earthquakes are interpreted to take place in subducted lithosphere that has deflected to a horizontal posture at the base of the upper mantle. Conversely, the deep seismicity in the adjacent Wadati-Benioff is associated with the deflection of the subducting lithosphere.

  10. Complex Proterozoic crustal assembly of southwestern North America in an arcuate subduction system:Tthe Black Canyon of the Gunnison, southwestern Colorado

    NASA Astrophysics Data System (ADS)

    Jessup, Micah J.; Kalstrom, Karl E.; Connelly, James; Williams, Michael; Livaccari, Richard; Tyson, Amanda; Rogers, Steven A.

    The dominant orogenic fabric in Proterozoic rocks of the southwestern U.S. includes a series of NE-striking shear zones that are commonly interpreted as suture zones across which blocks of juvenile crust were assembled to the southern margin of Laurentia. New structural and geochronological data from southwestern Colorado suggest that fabrics related to assembly of tectonostratigraphic terranes in this area strike northwest. The NW-striking foliations represent deformation at ca. 10-20 km paleodepths (ca. 1.77-1.71 Ga), and are parallel to magnetic anomalies and to gradients in mantle velocity structure. The agreement between these data sets suggests that the NW-striking structures are important at lithospheric scale, extend to >100 km depth, and may record assembly of southwestern Colorado across NW-striking tectonic boundaries. Geochronologic data indicate that northwest (central Colorado)—and northeast (Cheyenne belt)—striking boundaries developed simultaneously during accretion of southwestern Laurentia between ca. 1.78-1.73 Ga. We propose that the Yavapai province at ca. 1.75 Ga may have involved a complex arcuate subduction system, with multiple arcs, analogous to that of the modern Banda Sea, in the Indonesia region.

  11. A correlação índice espectral vs. luminosidade em QSOs e suas implicações

    NASA Astrophysics Data System (ADS)

    Garcia-Rissmann, A.

    2003-08-01

    Estudos de variabilidade de núcleos ativos já demonstraram ser comum o fato de seu contínuo óptico/UV tornar-se mais "duro" à medida que a luminosidade aumenta. Essa tendência ocorre tanto de forma individual quanto global, e pode ter implicações importantes (1) para estudos fotométricos de variabilidade conduzidos numa banda fixa no referencial do observador, comparando objetos a diferentes redshifts, e (2) no cálculo da correção K, com consequente impacto na determinação de massas de buracos negros e bojos de galáxias hospedeiras (através da relação de Magorrian). Confirmo aqui as correlações positivas entre o índice espectral e a luminosidade óptica, utilizando dados espectroscópicos de 11 QSOs monitorados no Brasil e no Chile, durante ~2 anos. O estudo é complementado com parâmetros extraídos de espectros e de dados fotométricos públicos de quasares. Destaco ainda as diferenças observadas em tais correlações para objetos do tipo radio-loud e radio-quiet. Este projeto é financiado pelo I. Milênio/CNPq.

  12. [Optic neuritis in childhood. A pediatric series, literature review and treatment approach].

    PubMed

    Lopez-Martin, D; Martinez-Anton, J

    2016-08-01

    Introduccion. En la edad pediatrica, la forma mas frecuente de neuritis optica se presenta generalmente despues de un cuadro infeccioso, con edema de papila, que suele ser bilateral y tiene buen pronostico. La conversion a esclerosis multiple es infrecuente. Objetivo. Presentar las caracteristicas clinicas y de laboratorio de una serie pediatrica de neuritis optica. Pacientes y metodos. Se analiza una serie de 17 casos de neuritis optica en niños y jovenes de 4 a 14 años, referidos entre los años 2000 y 2015. Resultados. La edad mediana de la serie fue de 11 años. Predominaron los pacientes de sexo femenino y el antecedente infeccioso fue poco frecuente; en cinco pacientes, la afectacion fue bilateral, y cuatro casos se presentaron como neuritis optica retrobulbar. La resonancia magnetica mostro hiperintensidad en T2 en los nervios opticos afectados en cinco pacientes. El estudio del liquido cefalorraquideo y bandas oligoclonales fue normal en todos los casos. Los pacientes, tratados con metilprednisolona intravenosa, tuvieron buena recuperacion. Solo en tres casos se comprobo una evolucion posterior a esclerosis multiple. Conclusiones. En esta serie, los casos que evolucionaron a esclerosis multiple no mostraron diferencias clinicas, aunque si presentaron mayor cantidad de lesiones hiperintensas en la resonancia magnetica. Este hecho, descrito en trabajos previos, apoya nuestro esquema diagnostico y terapeutico en un intento por acercarnos al manejo optimo de esta patologia.

  13. Ice clouds optical properties in the Far Infrared from the ECOWAR-COBRA Experiment

    NASA Astrophysics Data System (ADS)

    Rizzi, Rolando; Tosi, Ennio

    ECOWAR-COBRA (Earth COoling by WAter vapouR emission -Campagna di Osservazioni della Banda Rotazionale del vapor d'Acqua) field campaign took place in Italy from 3 to 17 March 2007 with the main goal of studying the scarcely sensed atmospheric emission occurring beyond 17 microns. Instrumentation involved in the campaign included two different Fourier Transforms Spectrometers (FTS) : REFIR-PAD (at Testa Grigia Station, 3500 m a.s.l.) and FTIR-ABB (at Cervinia Station, 1990 m a.s.l.). In this work cloudy sky data have been ana-lyzed. A cloud properties retrieval methodology (RT-RET), based on high spectral resolution measurements in the atmospheric window (800-1000 cm-1), is applied to both FTS sensors. Cloud properties determined from the infrared retrievals are compared with those obtained from Raman lidar taken by the BASIL Lidar system that was operating at Cervinia station. Cloud microphysical and optical properties retrieved by RT-RET are used to perform forward simulations over the entire FTSs measurements spectral interval. Results are compared to FTS data to test the ability of single scattering ice crystals models to reproduce cloudy sky radiances in the Far Infra-Red (FIR) part of the spectrum. New methods to retrieve cloud optical and microphysical properties exploiting high spectral resolution FIR measurements are also investigated.

  14. Irregular topography at the Earth's inner core boundary.

    PubMed

    Dai, Zhiyang; Wang, Wei; Wen, Lianxing

    2012-05-15

    Compressional seismic wave reflected off the Earth's inner core boundary (ICB) from earthquakes occurring in the Banda Sea and recorded at the Hi-net stations in Japan exhibits significant variations in travel time (from -2 to 2.5 s) and amplitude (with a factor of more than 4) across the seismic array. Such variations indicate that Earth's ICB is irregular, with a combination of at least two scales of topography: a height variation of 14 km changing within a lateral distance of no more than 6 km, and a height variation of 4-8 km with a lateral length scale of 2-4 km. The characteristics of the ICB topography indicate that small-scale variations of temperature and/or core composition exist near the ICB, and/or the ICB topographic surface is being deformed by small-scale forces out of its thermocompositional equilibrium position and is metastable.

  15. The "other" side of labor reform: accounts of incarceration and resistance in the Straits Settlements penal system, 1825-1873.

    PubMed

    Pieris, Anoma

    2011-01-01

    The rhetoric surrounding the transportation of prisoners to the Straits Settlements and the reformative capacity of the penal labor regime assumed a uniform subject, an impoverished criminal, who could be disciplined and accordingly civilized through labor. Stamford Raffles, as lieutenant governor of Benkulen, believed that upon realizing the advantages of the new colony, criminals would willingly become settlers. These two colonial prerogatives of labor and population categorized transportees into laboring classes where their exploitation supposedly brought mutual benefit. The colonized was collectively homogenized as a class of laborers and evidence to the contrary, of politically challenging and resistant individuals was suppressed. This paper focuses on two prisoners who were incriminated during the anti-colonial rebellions of the mid-nineteenth century and were transported to the Straits Settlements. Nihal Singh, a political prisoner from Lahore, was incarcerated in isolation to prevent his martyrdom and denied the supposed benefits of labor reform. Conversely, Tikiri Banda Dunuwille, a lawyer from Ceylon was sent to labor in Melaka as a form of humiliation. Tikiri’s many schemes to evade labor damned him in the eyes of the authorities. The personal histories of these two individuals expose how colonial penal policy recognized and manipulated individual differences during a time of rising anti-colonial sentiment. The experiences of these prisoners, the response of their communities and the voices of their descendents offer us a very different entry point into colonial penal history.

  16. Seismicity of the Earth 1900-2012 Java and vicinity

    USGS Publications Warehouse

    Jones, Eric S.; Hayes, Gavin P.; Bernardino, Melissa; Dannemann, Fransiska K.; Furlong, Kevin P.; Benz, Harley M.; Villaseñor, Antonio

    2014-01-01

    The Sunda convergent margin extends for 5,600 km from the Bay of Bengal and the Andaman Sea, both located northwest of the map area, towards the island of Sumba in the southeast, and then continues eastward as the Banda arc system. This tectonically active margin is a result of the India and Australia plates converging with and subducting beneath the Sunda plate at a rate of approximately 50 to 70 mm/yr. The main physiographic feature associated with this convergent margin is the Sunda-Java Trench, which stretches for 3,000 km parallel to the Java and Sumatra land masses and terminates at 120° E. The convergence of the Indo-Australia and Sunda plates produces two active volcanic arcs: Sunda, which extends from 105 to 122° E and Banda, which extends from 122 to 128° E. The Sunda arc results solely from relatively simple oceanic plate subduction, while the Banda arc represents the transition from oceanic subduction to continental collision, where a complex, broad deforming zone is found. Based on modern activity, the Banda arc can be divided into three distinct zones: an inactive section, the Wetar Zone, bound by two active segments, the Flores Zone in the west and the Damar Zone in the east. The lack of volcanism in the Wetar Zone is attributed to the collision of Australia with the Sunda plate. The absence of gap in volcanic activity is underlain by a gap in intermediate depth seismicity, which is in contrast to nearly continuous, deep seismicity below all three sections of the arc. The Flores Zone is characterized by down-dip compression in the subducted slab at intermediate depths and late Quaternary uplift of the forearc. These unusual features, along with GPS data interpretations indicate that the Flores Zone marks the transition between subduction of oceanic crust in the west and the collision of continental crust in the east. The Java section of the Sunda arc is considered relatively aseismic historically when compared to the highly seismically active

  17. Contribuições para o projeto da câmara infravermelha Spartan do telescópio SOAR

    NASA Astrophysics Data System (ADS)

    Laporte, R.; Jablonski, F.; Loh, E.

    2003-08-01

    Como parte de uma colaboração entre a Divisão de Astrofísica do INPE, IAG-USP, Instituto do Milênio MEGALIT e a Michigan State University, trabalhamos durante um ano junto ao grupo do Dr. Edwin Loh (MSU) no projeto e detalhamento de diversos subsistemas para a câmara infravermelho Spartan do telescópio SOAR. Trata-se de um imageador para as bandas J, H e K que explora todo o potencial, em termos de qualidade de imagem e campo de visada, fornecido pelo sistema de óptica adaptativa de primeira ordem do telescópio SOAR. Projetamos soluções detalhadas para os subsistemas de rodas de filtros/grismas/máscaras de Lyot; subsistema de compactação do mosaico de detectores em duas versões distintas; subsistema de alimentação de Nitrogênio líquido. Mantivemos sempre uma supervisão geral sobre todas as partes restantes e os respectivos envelopes volumétricos produzindo soluções para a integração de todos os componentes. Neste trabalho, ilustramos as principais contribuições e fornecemos um resumo do estado atual do instrumento.

  18. Seismicity of the Earth 1900-2012 Java and vicinity

    USGS Publications Warehouse

    Jones, Eric S.; Hayes, Gavin P.; Bernardino, Melissa; Dannemann, Fransiska K.; Furlong, Kevin P.; Benz, Harley M.; Villaseñor, Antonio

    2014-01-01

    The Sunda convergent margin extends for 5,600 km from the Bay of Bengal and the Andaman Sea, both located northwest of the map area, towards the island of Sumba in the southeast, and then continues eastward as the Banda arc system. This tectonically active margin is a result of the India and Australia plates converging with and subducting beneath the Sunda plate at a rate of approximately 50 to 70 mm/yr. The main physiographic feature associated with this convergent margin is the Sunda-Java Trench, which stretches for 3,000 km parallel to the Java and Sumatra land masses and terminates at 120° E. The convergence of the Indo-Australia and Sunda plates produces two active volcanic arcs: Sunda, which extends from 105 to 122° E and Banda, which extends from 122 to 128° E. The Sunda arc results solely from relatively simple oceanic plate subduction, while the Banda arc represents the transition from oceanic subduction to continental collision, where a complex, broad deforming zone is found. Based on modern activity, the Banda arc can be divided into three distinct zones: an inactive section, the Wetar Zone, bound by two active segments, the Flores Zone in the west and the Damar Zone in the east. The lack of volcanism in the Wetar Zone is attributed to the collision of Australia with the Sunda plate. The absence of gap in volcanic activity is underlain by a gap in intermediate depth seismicity, which is in contrast to nearly continuous, deep seismicity below all three sections of the arc. The Flores Zone is characterized by down-dip compression in the subducted slab at intermediate depths and late Quaternary uplift of the forearc. These unusual features, along with GPS data interpretations indicate that the Flores Zone marks the transition between subduction of oceanic crust in the west and the collision of continental crust in the east. The Java section of the Sunda arc is considered relatively aseismic historically when compared to the highly seismically active

  19. Uranium-series ages of marine terraces, La Paz Peninsula, Baja California Sur, Mexico

    USGS Publications Warehouse

    Sirkin, L.; Szabo, B. J.; Padilla, G.A.; Pedrin, S.A.; Diaz, E.R.

    1990-01-01

    Uranium-series dating of coral samples from raised marine terrace deposits between 1.5 and 10 m above sea level in the La Paz Peninsula area, Baja California Sur, yielded ages between 123 ka and 138 ka that are in agreement with previously reported results. The stratigraphy and ages of marine units near the El Coyote Arroyo indicate the presence of two high stands of the sea during the last interglacial or oxygen isotope substage 5e at about 140 ka and 123 ka. Accepting 5 m for the sea level during the last interglacial transgression, we calculate average uplift rates for the marine terraces of about ???70 mm/ka and 40 mm/ka. These slow rates of uplift indicate a relative stability of the La Paz peninsula area for the past 140 000 years. In contrast, areas of Baja California affected by major faultf experienced higher rates of uplift. Rockwell et al. (1987) reported vertical uplift rates of 180 to 300 mm/ka at Punta Banda within the Aqua Blanea fault zone in northern Baja California. ?? 1990 Springer-Verlag.

  20. Polarización lineal en estrellas simbióticas

    NASA Astrophysics Data System (ADS)

    Brandi, E.; García, L. G.; Ferrer, O. E.

    Se presenta un estudio de polarización lineal en las bandas UBVRI de un grupo de estrellas simbióticas, a fin de analizar el comportamiento del grado de polarización y del ángulo de posición en función de la longitud de onda. En aquellos sistemas observados repetidas veces, se analizan además variaciones temporales en los parámetros de polarización. En base a este comportamiento se determina si la polarización observada es puramente interestelar o si existe una contribución de polarización, intrínseca al objeto. La muestra de objetos estudiados presenta ciertas características comunes, es decir, son sistemas simbióticos tipo D, cuyas respectivas componentes gigantes son variables tipo Mira y además presentan nebulosas ionizadas extendidas con morfología y dimensiones conocidas. Esto es de importancia ya que el conocimiento de la estructura del gas extendido permite interpretar la geometría de scattering que produce la polarización observada. Las observaciones fueron realizadas con el Fotopolarímetro de Torino adosado al telescopio de 2.15 m del CASLEO.

  1. Design analysis of vertical wind turbine with airfoil variation

    NASA Astrophysics Data System (ADS)

    Maulana, Muhammad Ilham; Qaedy, T. Masykur Al; Nawawi, Muhammad

    2016-03-01

    With an ever increasing electrical energy crisis occurring in the Banda Aceh City, it will be important to investigate alternative methods of generating power in ways different than fossil fuels. In fact, one of the biggest sources of energy in Aceh is wind energy. It can be harnessed not only by big corporations but also by individuals using Vertical Axis Wind Turbines (VAWT). This paper presents a three-dimensional CFD analysis of the influence of airfoil design on performance of a Darrieus-type vertical-axis wind turbine (VAWT). The main objective of this paper is to develop an airfoil design for NACA 63-series vertical axis wind turbine, for average wind velocity 2,5 m/s. To utilize both lift and drag force, some of designs of airfoil are analyzed using a commercial computational fluid dynamics solver such us Fluent. Simulation is performed for this airfoil at different angles of attach rearranging from -12°, -8°, -4°, 0°, 4°, 8°, and 12°. The analysis showed that the significant enhancement in value of lift coefficient for airfoil NACA 63-series is occurred for NACA 63-412.

  2. Oceanwide gravity anomalies from Geos-3, Seasat and Geosat altimeter data

    NASA Technical Reports Server (NTRS)

    Rapp, Richard H.; Basic, Tomislav

    1992-01-01

    Three kinds of satellite altimeter data have been combined, along with 5 x 5 arcmin bathymetric data, to calculate a 0.125 deg ocean wide gridded set of 2.3 x 10 exp 6 free-air gravity anomalies. The procedure used was least squares collocation that yields the predicted anomaly and standard deviation. The value of including the bathymetric data was shown in a test around the Dowd Seamount where the root mean square (rms) difference between ship gravity measurements decreased from +/- 40 mgal to +/- 20 mgal when the bathymetry was included. Comparisons between the predicted anomalies and ship gravity data is described in three cases. In the Banda Sea the rms differences were +/- 20 mgal for two lines. In the South Atlantic rms differences over lines of 2000 km in length were +/- 7 mgal. For cruise data in the Antarctica region the discrepancies were +/- 12 mgal. Comparisons of anomalies derived from the Geosat geodetic mission data by Marks and McAdoo (1992) with ship dta gave differences of +/- 6 mgal showing the value of the much denser Geosat geodetic mission altimeter data.

  3. Tectonic development of the Indonesian archipelago and its bearing on the occurrence of hydrocarbons

    SciTech Connect

    Simanjuntak, T.O. )

    1994-07-01

    The present geological and tectonic configuration of the Indonesian archipelago may represent a typical triple junction plate convergence, which has developed since Neogene times due to the northward-moving Indo-Australian plate, the westward-moving Pacific plate, and the south-southeastward-moving Eurasian Craton. The occurrence of a number of microcontinents in eastern Indonesia makes the geology and tectonics of the region more complex. The archipelago is one of the most complicated regions from the plate tectonics point of view. The geological evolution of the Indonesian archipelago is recorded by the occurrence of both tectonic convergence and tectonic divergence. Various types of plate convergences include a Cordilleran type subduction, which has been reoccurring since Paleozoic until present times in western Indonesia; a Neogene Tethyan type collision in the Banda region; and a double-arc collision in northern Maluku, central Indonesia. Tectonic divergence, which was preceded by rifting due to thermal doming and magma rise in the northern margins of the Australian Craton and followed by the detachment and west-northwestward displacement of continental fragments in Mesozoic, gave rise to the development of the microcontinents in eastern Indonesia.

  4. Nuevas observaciones de 3C10 con el VLA*: estudio de la expansión

    NASA Astrophysics Data System (ADS)

    Reynoso, E. M.; Moffett, D. A.:; Dubner, G. M.; Giacani, E. B.; Reynolds, S. P.; Goss, W. M.; Dickel, J.

    Se presentan nuevos resultados sobre la expansión del remanente de la supernova de Tycho a lo largo de un intervalo de 10.9 años, comparando nuevas observaciones tomadas con el VLA a 1375 y 1635 MHz durante 1994 y 1995, con observaciones previas realizadas entre 1983 y 1984 (Dickel y col. ~1991 AJ 101, 2151), usando las mismas configuraciones, anchos de banda, calibradores y tiempos de integración. El coeficiente de expansión se calcula para sectores radiales de 4o de ancho cada uno, ajustando la correlación cruzada de las derivadas de los perfiles promedio para cada época. A partir de la expansión medida, se estima el índice (parámetro de expansión) de la ley potencial R∝ tm como m≡ d ln R/d ln t . Este valor se compara con coeficientes teóricos para diferentes fases evolutivas de remanentes de supernova.

  5. An economical non-destructive method for estimating eelgrass, Zostera marina (Potamogetonaceae) leaf growth rates: formal development and use in northwestern Baja California.

    PubMed

    Solana-Arellano, Elena; Echavarria-Heras, Héctor; Franco-Vizcaíno, Ernesto

    2008-09-01

    Seagrass beds provide much of the primary production in estuaries; host many fishes and fish larvae, and abate erosion. The present study presents original analytical methods for estimating mean leaf-growth rates of eelgrass (Zostera marina). The method was calibrated by using data collected in a Z. marina meadow at Punta Banda estuary in Baja California, Mexico. The analytical assessments were based on measurements of leaf length and standard regression procedures. We present a detailed explanation of the formal procedures involved in the derivation of these analytical methods. The measured daily leaf-growth rate was 10.9 mm d(-1) leaf(-1). The corresponding value projected by our method was 10.2 mm d(-1) leaf(-). The associated standard errors were of 0.53 and 0.56 mm d(-1) leaf(-1) respectively. The method was validated by projecting leaf-growth rates from an independent data set, which gave consistent results. The use of the method to obtain the mean leaf growth rate of a transplanted plot is also illustrated. Comparison of our leaf-growth data with previously reported assessments show the significant forcing of sea-surface temperature on eelgrass leaf dynamics. The formal constructs provided here are of general scope and can be applied to equivalent eelgrass data sets in a straightforward manner.

  6. Rebuilt risk: involuntary return, voluntary migration, and socioeconomic segregation in post-tsunami Aceh

    NASA Astrophysics Data System (ADS)

    McCaughey, Jamie; Daly, Patrick; Mundzir, Ibnu; Mahdi, Saiful; Patt, Anthony

    2016-04-01

    In light of growing coastal populations and rising relative sea levels, understanding the consequences of infrequent, high-impact coastal hazards for human migration is a key ingredient for meeting the challenges of sustainable development. Using new quantitative and qualitative evidence from 1160 households and 121 village leaders, we examine longer-term migration in the city of Banda Aceh, Indonesia, following the devastating 2004 tsunami and an international aid response that offered most survivors only resettlement back in the tsunami-affected area. While many survivors wanted to return, some preferred to relocate further from the coast but did not have the chance to do so. Since that time, selective out-migration by those with the means and socioeconomic sorting of newcomers have led to a new socioeconomic segregation of the tsunami-affected parts of the city. More broadly, these findings suggest that short-distance socioeconomic sorting into and out from vulnerable areas may be an important migratory response to a newly recognized risk.

  7. [Effect of alcohol on electrical organisation in the brain during a visuospatial working memory task and its relationship with the menstrual cycle].

    PubMed

    Sanz-Martin, Araceli; Hernández-González, Marisela; Guevara, Miguel Ángel; Santana, Gloria; Gumá-Díaz, Emilio

    2014-02-01

    Introduccion. El metabolismo del alcohol y el desempeño de muchas funciones cognitivas pueden variar a lo largo del ciclo menstrual. Tanto la ingestion de alcohol como las variaciones hormonales durante el ciclo menstrual se asocian con cambios caracteristicos en la actividad electroencefalografica. Objetivo. Determinar si la actividad electroencefalografica durante una tarea de memoria de trabajo es afectada por el consumo agudo de alcohol, y si dicha actividad varia en funcion del ciclo menstrual. Sujetos y metodos. Muestra de 24 mujeres que ingirieron alcohol o placebo durante las fases folicular y lutea temprana. Se registro el electroencefalograma durante la ejecucion de una tarea de memoria de trabajo visuoespacial. Resultados. Aunque el alcohol no deterioro el rendimiento de la tarea de memoria de trabajo, si produjo en el electroencefalograma una disminucion de la potencia relativa de theta y una menor correlacion frontoparietal derecha en las bandas theta y alfa2. Unicamente las mujeres alcoholizadas en la fase folicular presentaron una mayor potencia relativa de alfa1, que podria indicar menor nivel de alertamiento y atencion. Conclusiones. Estos resultados contribuyen a una mejor comprension de los mecanismos cerebrales que subyacen a los cambios cognitivos con el alcohol y su relacion con el ciclo menstrual.

  8. Cool Indonesian throughflow as a consequence of restricted surface layer flow.

    PubMed

    Gordon, Arnold L; Susanto, R Dwi; Vranes, Kevin

    2003-10-23

    Approximately 10 million m3 x s(-1) of water flow from the Pacific Ocean into the Indian Ocean through the Indonesian seas. Within the Makassar Strait, the primary pathway of the flow, the Indonesian throughflow is far cooler than estimated earlier, as pointed out recently on the basis of ocean current and temperature measurements. Here we analyse ocean current and stratification data along with satellite-derived wind measurements, and find that during the boreal winter monsoon, the wind drives buoyant, low-salinity Java Sea surface water into the southern Makassar Strait, creating a northward pressure gradient in the surface layer of the strait. This surface layer 'freshwater plug' inhibits the warm surface water from the Pacific Ocean from flowing southward into the Indian Ocean, leading to a cooler Indian Ocean sea surface, which in turn may weaken the Asian monsoon. The summer wind reversal eliminates the obstructing pressure gradient, by transferring more-saline Banda Sea surface water into the southern Makassar Strait. The coupling of the southeast Asian freshwater budget to the Pacific and Indian Ocean surface temperatures by the proposed mechanism may represent an important negative feedback within the climate system. PMID:14574409

  9. Surface water processes in the Indonesian throughflow as documented by a high-resolution coral Δ14C record

    NASA Astrophysics Data System (ADS)

    Fallon, Stewart J.; Guilderson, Thomas P.

    2008-09-01

    To explore the seasonal to decadal variability in surface water masses that contribute to the Indonesian throughflow, we have generated a 115-year bimonthly coral-based radiocarbon time series from a coral in the Makassar Straits. In the pre-bomb (pre-1955) era from 1890 to 1954, the radiocarbon time series occasionally displays a small seasonal signal (10-15‰). After 1954 the radiocarbon record increases rapidly, in response to the increased atmospheric 14C content caused by nuclear weapons testing. From 1957 to 1986 the record displays clear seasonal variability from 15 to 60‰ and the post-bomb peak (163 per mil) occurred in 1974. The seasonal cycle of radiocarbon can be attributed to variations of surface waters passing through the South Makassar Strait. Southern Makassar is under the influence of the Northwest Monsoon, which is responsible for the high austral summer radiocarbon (North Pacific waters) and the Southeast Monsoon that flushes back a mixture of low (South Pacific and upwelling altered) radiocarbon water from the Banda Sea. The coral record also shows a significant 14C peak in 1955 due to the bomb-14C water advected into this region from nuclear weapons tests in the Marshall Islands in 1954.

  10. Analysis of spatiotemporal variation in b-value for the Sunda arc using high precision earthquake location

    NASA Astrophysics Data System (ADS)

    Nugraha, Andri Dian; Shiddiqi, Hasbi Ash; Widiyantoro, Sri; Sutiyono, Handayani, Titi

    2016-05-01

    The Sunda arc is one of the most active tectonic regions, which has a complex tectonic setting due to different tectonic regimes and subduction geometry along this arc. We analyzed variation in b-value for this region in order to obtain better information regarding the state of stress in this region. For the first step, we relocated earthquake hypocenters taken from the BMKG catalog for the period 2009 - 2015 by employing a teleseismic double-difference (DD) relocation method and using a 3D velocity model. There are 10,440 earthquakes that were successfully relocated with greatly reduced residual errors. Based on its tectonic feature and earthquake distribution, we divided the study area into 8 regions, i.e. northern Sumatra, central Sumatra, southern Sumatra, Sunda strait, western Java, eastern Java, lesser Sunda islands, and Sunda-Banda transition zone. For b-value analysis we combined the BMKG catalog with the International Seismological Centre (ISC) catalog from 2006 to 2009 to obtain a longer time period. We analyzed the spatial variation in b-value for western sunda arc and found a low b-value that matches well with earthquake locations.

  11. Estudio teórico de la desorción de Na y K de SiO2 estimulada por la acción de fotones o electrones

    NASA Astrophysics Data System (ADS)

    Domínguez Ariza, D.; López, N.; Illas, F.; Pacchioni, G.; Madey, T. E.

    Se ha estudiado el mecanismo de generación de sodio y potasio atómico a partir de muestras de SiO2 utilizando cálculos basados tanto en la teoría del funcional de la densidad como en métodos post-Hartree Fock, así como en el método de cluster para modelar el sólido. Como consecuencia del estudio se han propuesto distintos caminos posibles para la desorción, estimulada por la acción de fotones o electrones, de sodio y potasio desde el óxido de silicio, proporcionando por lo tanto una explicación a la atmósfera tenue de sodio y potasio de La Luna.

  12. Evolución estelar en sistemas binarios

    NASA Astrophysics Data System (ADS)

    De Vito, M. A.; Benvenuto, O.

    Definición y clasificación de sistemas binarios; descripción del comportamiento del sistema frente a la variación de su masa; binarias de rayos X; transferencia de masa en sistemas binarios masivos aplicado al posible esclarecimiento del progenitor azul de la supernova SN 1987A; comentario acerca de la evolución de enanas blancas de helio de baja masa y su conexión con los sistemas binarios; reseña del trabajo de Kippenhahn y Weigert sobre el cual está basado el código evolutivo desarrollado en la FCAG por el Dr. Benvenuto y sobre el cual se trabajará para poder incluir la evolución de una estrella con pérdida de masa perteneciente a un sistema binario.

  13. Primeros resultados sobre el estudio de oscilaciones no radiales

    NASA Astrophysics Data System (ADS)

    Córsico, A.; Benvenuto, O. G.

    En el Observatorio de La Plata se ha comenzado a elaborar un código de pulsaciones el cual resuelve el problema de las oscilaciones no radiales en el caso adiabático. Dicho código está basado en la técnica de diferencias finitas ampliamente usado en cálculos de estructura y evolución estelar. En este trabajo se presentan los primeros resultados encontrados aplicando el código mencionado al caso de una polítropa de índice n=3. Se presentan los valores de las autofrecuencias y las autofunciones para diferentes modos de pulsación de dicha configuración politrópica. En un futuro próximo, se aplicará este programa al estudio de las pulsaciones no radiales de estrellas enanas blancas.

  14. The last interglacial period on the Pacific Coast of North America: Timing and paleoclimate

    USGS Publications Warehouse

    Muhs, D.R.; Simmons, K.R.; Kennedy, G.L.; Rockwell, T.K.

    2002-01-01

    New, high-precision U-series ages of solitary corals (Balanophyllia elegans) coupled with molluscan faunal data from marine terraces on the Pacific Coast of North America yield information about the timing and warmth of the last interglacial sea-level highstand. Balanophyllia elegans takes up U in isotopic equilibrium with seawater during growth and shortly after death. Corals from the second terrace on San Clemente Island (offshore southern California), the third terrace on Punta Banda (on the Pacific Coast of northern Baja California), and the Discovery Point Formation on Isla de Guadalupe (in the Pacific Ocean offshore Baja California) date to the peak of the last interglacial period and have U-series ages ranging from ca. 123 to 114 ka. The first terrace on Punta Banda has corals with ages ranging from ca. 83 to 80 ka, which corresponds to a sea-level highstand formed in the late last interglacial period. U-series analyses of corals from the Cayucos terrace (central California) and the Nestor terrace at Point Loma (southern California) show that these fossils have evidence of open-system history, similar to what has been reported by other workers for the same localities. Nevertheless, a model of continuous, secondary U and Th uptake shows that two ages of corals are likely present at these localities, representing the ca. 105 and ca. 120 ka sea-level highstands reported elsewhere. U-series ages of last interglacial corals from the Pacific Coast overlap with, but are on average younger than the ages of corals from Barbados, the Bahamas, and Hawaii. This age difference is explained by the nature of the geomorphic response to sea-level change: fringing or barrier reefs on low-latitude coastlines have an accretionary growth style that keeps pace with rising sea level, whether on a tectonically rising or stable coastline. In contrast, midlatitude, high-energy coastlines are sites of platform cutting during the early part of a sea-level high stand and terrace

  15. Estimates of tidal mixing in the Indonesian archipelago from multidisciplinary INDOMIX in-situ data

    NASA Astrophysics Data System (ADS)

    Koch-Larrouy, Ariane; Atmadipoera, Agus; van Beek, Pieter; Madec, Gurvan; Aucan, Jérôme; Lyard, Florent; Grelet, Jacques; Souhaut, Marc

    2015-12-01

    The Indonesian Mixing program (INDOMIX) was designed to quantify the very strong mixing that transforms Pacific waters into isohaline Indonesian Waters in the Indonesian archipelago. The turbulent dissipation rates and associated mixing were estimated and analyzed using a multidisciplinary approach that combines physical and geochemical in-situ observations: (1) direct measurements of the dissipation using a microstructure profiler, (2) use of density-based fine-scale methods applied to CTD and XCTD data, and (3) study of the vertical distribution of natural radionuclides (radium isotopes and actinium-227). Data were collected at five contrasting stations within the Indonesian archipelago, found above energetic straits or in relatively quiescent large basins. Strong instabilities, inversions of the density profiles and a very strong water mass transformation were observed. A wide range of dissipation values were obtained (between [10-10, 10-4] W kg-1) with spots of higher dissipation in the ocean interior correlated with a strong internal tide signal. Both the fine-scale and micro-scale methods allow us to identify very strong energy dissipation levels above the straits, ranging between [10-7, 10-4] W kg-1, in contrast to lower values at stations further away from the generation sites. The dissipation for the station located in the center of the Halmahera Sea ([10-9, 10-8] W kg-1) is stronger than for the Banda station ([10-11, 10-10] W kg-1), which is even further away from the generation sites. The three approaches agree relatively well and provide vertical eddy diffusivities values ranging between 5×10-4 and 5×10-1 m2 s-1, except in the Banda Sea where values are similar to the ones found in the open ocean (10-6 m2 s-1). CTD and XCTD profilers (deployed between stations) give estimates of dissipation all along the transit. It is found that enhanced mixing occurs preferentially above rough topography, such as in the Ombai Strait, the Halmahera Sea's northern

  16. Mantle dynamics and slab rheology constrained by numerical modeling, structural and source seismology

    NASA Astrophysics Data System (ADS)

    Alpert, Lisa Ann

    , regional uplift patterns and magmatism have been used to infer the relationship between subducting slabs and surface processes. In Chapter 4, I develop three dimensional, thermochemical, dynamic subduction models guided by seismicity and geomorphology from the Banda arc to explore the fate of subducted slabs after continental collision. I confirm the importance of buoyancy contrasts in exerting a first order control on the generation of slab tears in the upper mantle. I find that rheology exerts a strong control on the timing of slab tearing while continental geomorphology may explain complex surface processes in regions of incipient continental collision. From my modeling, I infer that seismicity patterns beneath the Banda Arc represent a westward propagating slab tear in response to the collision of the buoyant Australian shelf, and an eastward propagating slab tear in response to the collision of the Scott Plateau to the west. Further utilization of surface observations along with continued advances in geodynamic modeling continue to bridge the gap between lithospheric and deeper mantle processes.

  17. Northwestern Australian Collision in the Timor Sea: Constraints From Flexurally-Induced Normal Faulting.

    NASA Astrophysics Data System (ADS)

    Londono, J.; Lorenzo, J.; O'Brien, G.

    2001-12-01

    Since latest Miocene to Early Pliocene partial subduction of the northwestern Australian continental margin beneath the Eurasian plate produced an early stage foreland basin in the Timor Sea. Pre-Miocene superimposed thin and thick skinned structural styles, are equally affected by the collision of the continental crust with the Banda Arc. Flexural extension due to the bending of the Australian plate resulted in the reactivation of numerous earlier normal faults. These reactivated structures document the oblique, rotational clockwise, southeastward nature of the convergence. Over 500 kilometers of 2D seismic data and well information record the geometry and character of the flexure-induced normal faults. Over 200 of these faults were studied. Earliest Pliocene fault slip decreases about 35 % from west to east from 11.95 ms (Approx. 30 m) on average in the south west (Vulcan basin area) to 7.86 ms (Approx. 19.5 m) in the north east (Sahul platform area). Conversely, late Pliocene fault slip increases about 28 % from 6.47 ms (Aprox. 17 m) on average in the south west (Vulcan basin area) to 8.3 ms (Approx. 21 m) in the north east (Sahul platform region). Rheologic analysis indicates that the Vulcan basin area has undergone more total deformation as indicated by the higher total offset of faulting within the sedimentary foreland sequence. However, since Late Pliocene the Sahul platform area has undergone about 10 % more deformation as indicated by the average slip in the flexural faults. Collision, then, probably occurs in a clockwise sense beginning south of Timor Island and continuing later toward the Tanimbar Island region in the north east. Tomographic images of the mantle in the area corroborate the enhanced amount of subduction of the southwestern region compare to the north east. Simple elastic models predict greater bending stresses toward the Timor trough. The expected increase in deformation toward the trough is manifested by an increase in fault density

  18. Tectonic History and Mantle Structure of the Sundaland and Indonesian Region

    NASA Astrophysics Data System (ADS)

    Hall, R.; Spakman, W.

    2012-12-01

    The heterogeneous Sundaland region was assembled by closure of Tethyan oceans and addition of continental fragments. Its Mesozoic and Cenozoic history is partly recorded in the mantle, and mantle structure from tomographic imaging can be interpreted using new plate tectonic reconstructions. Continental fragments of east Asian origin, ophiolites and deformed sediments were accreted to eastern Sundaland north of Borneo in the Cretaceous, and a wide zone from Sarawak northwards to South China probably represents subduction at the Pacific margin until about 90 Ma. Eastward rollback at this margin may have contributed to Cretaceous extension and thermal events in Indochina but it is difficult to identify a record of this subduction in the mantle. Continental blocks rifted from western Australia in the Late Jurassic-Early Cretaceous are in Borneo, Java and Sulawesi. West Burma was not one of them; it was already part of SE Asia by the Triassic. The Banda (SW Borneo) block was added to Sundaland at c.110 Ma, and at c.90 Ma the Woyla intra-oceanic arc and Argo (East Java-West Sulawesi) block collided with the Sundaland margin causing subduction to cease. A marked change in deep mantle structure at about 110°E reflects the different subduction histories north of India and Australia since 90 Ma. India and Australia were separated by a transform boundary that was leaky from 90 to 75 Ma and slightly convergent from 75 to 55 Ma. West of this I-A transform, ENE-striking high-velocity anomalies in the lower mantle are interpreted to mark subduction zones active as India moved rapidly north from 80 Ma, with north-directed subduction of Tethys, associated with collision of India with an intra-oceanic arc at c.55 Ma, west of Sumatra, before collision with Asia in the Eocene. In contrast, east of the I-A transform little or none of the Mesozoic history can be identified in the mantle. Between 90 and 45 Ma Australia separated very slowly from Antarctica and there was no significant

  19. Compilação de dados atômicos e moleculares do UV ao IV próximo para uso em síntese espectral

    NASA Astrophysics Data System (ADS)

    Coelho, P.; Barbuy, B.; Melendez, J.; Allen, D. M.; Castilho, B.

    2003-08-01

    Espectros sintéticos são utéis em uma grande variedade de aplicações, desde análise de abundâncias em espectros estelares de alta resolução ao estudo de populações estelares em espectros integrados. A confiabilidade de um espectro sintético depende do modelo de atmosfera adotado, do código de formação de linhas e da qualidade dos dados atômicos e moleculares que são determinantes no cálculo das opacidades da fotosfera. O nosso grupo no departamento de Astronomia no IAG tem utilizado espectros sintéticos há mais de 15 anos, em aplicações voltadas principalmente para a análise de abundâncias de estrelas G, K e M e populações estelares velhas. Ao longo desse tempo, as listas de linhas vieram sendo construídas e atualizadas continuamente, e alguns acréscimos recentes podem ser citados: Castilho (1999, átomos e moléculas no UV), Schiavon (1998, bandas moleculares de TiO) e Melendez (2001, átomos e moléculas no IV próximo). Com o intuito de calcular uma grade de espectros do UV ao IV próximo para uso no estudo de populações estelares velhas, se fazia necessário compilar e homogeneizar as diversas listas em apenas uma lista atômica e uma molecular. Nesse processo, a nova lista compilada foi correlacionada com outras bases de dados (NIST, Kurucz Database, O' Brian et al. 1991) para atualização dos parâmetros que caracterizam a transição atômica (comprimento de onda, log gf e potencial de excitação). Adicionalmente as constantes de interação C6 foram calculadas segundo a teoria de Anstee & O'Mara (1995) e artigos posteriores. As bandas moleculares de CH e CN foram recalculadas com o programa LIFBASE (Luque & Crosley 1999). Nesse poster estão detalhados os procedimentos citados acima, as comparações entre espectros calculados com as novas listas e espectros observados em alta resolução do Sol e de Arcturus, e uma análise do impacto decorrente da utilização de diferentes modelos de atmosfera no espectro sintético. Ao

  20. Redox-variability and controls in subduction zones from an iron-isotope perspective

    NASA Astrophysics Data System (ADS)

    Nebel, O.; Sossi, P. A.; Bénard, A.; Wille, M.; Vroon, P. Z.; Arculus, R. J.

    2015-12-01

    An ongoing controversy in mantle geochemistry concerns the oxidation state of the sources of island arc lavas (IAL). Three key factors control oxidation-reduction (redox) of IAL sources: (i) metasomatism of the mantle wedge by fluids and/or melts, liberated from the underlying subducted slab; (ii) the oxidation state of the wedge prior to melting and metasomatism; and (iii) the loss of melt from IAL sources. Subsequently, magmatic differentiation by fractional crystallisation, possible crustal contamination and degassing of melts en route to and at the surface can further modify the redox states of IAL. The remote nature of sub-arc processes and the complex interplay between them render direct investigations difficult. However, a possible gauge for redox-controlled, high-temperature pre-eruptive differentiation conditions is variations in stable Fe isotope compositions (expressed here as δ57Fe) in erupting IAL because Fe isotopes can preserve a record of sub-surface mass transfer reactions involving the major element Fe. Here we report Fe isotope compositions of bulk IAL along the active Banda arc, Indonesia, which is well known for a prominent subducted sediment input. In conjunction with other arc rocks, δ57Fe in erupted Banda IAL indicates that fractional crystallisation and possibly crustal contamination primarily control their Fe isotope signatures. When corrected for fractional crystallisation and filtered for contamination, arc magmas that had variable sediment melt contributions in their sources show no resolvable co-variation of δ57Fe with radiogenic isotope tracers. This indicates that crustal recycling in the form of subducted sediment does not alter the Fe isotope character of arc lavas, in agreement with mass balance estimates. Primitive sources of IAL, however, are clearly isotopically lighter than those sourced beneath mid-ocean ridges, indicating either preferential Fe3+-depletion in the mantle wedge by prior, δ57Fe-heavy melt extraction, and

  1. Timing the structural events in the Palaeoproterozoic Bolé-Nangodi belt terrane and adjacent Maluwe basin, West African craton, in central-west Ghana

    NASA Astrophysics Data System (ADS)

    de Kock, G. S.; Théveniaut, H.; Botha, P. M. W.; Gyapong, W.

    2012-04-01

    The Maluwe basin, north-adjacent to the Sunyani basin, is the northernmost of the northeast-trending Eburnean volcaniclastic depositories in Ghana. These basins are separated from one another by remnants of Eoeburnean crust, all formed during the evolution of an arc-backarc basins complex in a Palaeoproterozoic intraoceanic environment. The Bolé-Nangodi belt terrane to the northwest, of mostly Eoeburnean crust is fault bounded with the Maluwe basin along the northeast-trending Bolé-Navrongo fault zone. The stratigraphic sequence, which was the key to unravelling the structural evolution of the study area, was established by means of field observations aided by precision SHRIMP geochronology. The quartzitic, pelitic, quartzofeldspathic and granitic gneisses of the Eoeburnean crust (>2150 Ma) experienced complex metamorphic mineral growth and migmatitization, mostly under static crustal conditions and were subjected to several deformation episodes. The foliated mafic and metasedimentary enclaves within the Ifanteyire granite establish deformation to have taken place prior to ˜2195 Ma, while the tectonically emplaced Kuri amphibolites within the 2187-Ma gneissic Gondo granite indicate a stage of rifting followed by collision. Deformation of granite dykes in the Gondo granites at ˜2150 Ma concluded the development of the Eoeburnean orogenic cycle (DEE). The Sawla Suite, contemporaneous with the deposition of the Maluwe Group, intruded the tectonic exhumed Bolé-Nangodi terrane during extension between ˜2137 and 2125 Ma. The rifting separated the Abulembire fragment from the Bolé-Nangodi terrane. During subsequent northwestward subduction of young back-arc basin oceanic crust the volcaniclastic strata of the Maluwe Group and Sawla granitoids were deformed (DE1) under chlorite/sericite greenschist-grade conditions. The NE-trending folds had subhorizontal axes and subvertical axial planes. Simultaneous to the DE1 orogenesis the molasses of the Banda Group was

  2. The 339 Years of Living Dangerously in Indonesia: Earthquakes and Tsunamis in the Indonesian Region from 1538 to 1877

    NASA Astrophysics Data System (ADS)

    Harris, R. A.; Major, J.

    2013-05-01

    Using 339 years of Dutch records of geophysical events in Indonesia and tsunami modeling, we have identified previously unknown mega-thrust earthquake sources in eastern Indonesia that caused severe devastation in the past and are likely to reoccur in the near future. Indonesia has experienced some of the most extreme geohazards known (Toba, Krakatoa, Tambora, Indian Ocean tsunami). Although most of well known events occurred in western Indonesia, historical records reveal that eastern Indonesia is actually more hazardous. Strain rates in eastern Indonesia are twice those in Sumatra and tsunamis are much more frequent. Adding to the disaster potential in Indonesia is its rapid population growth and urbanization, especially in coastal regions. When the events documented in historical records reoccur in eastern Indonesia, as they have in western Indonesia, ten times more people and assets will be in harms way. Arthur Wichmann's Die Erdbeben Des Indischen Archipels [The Earthquakes of the Indian Archipelago] (1918) documents >100 destructive earthquakes and 68 tsunamis between 1600 and 1877. The largest and best documented are the events of 1629, 1674 and 1852 in the Banda Sea region, 1770 and 1859 in the Molucca Sea region, 1820 in Makassar, 1857 in Dili, Timor, 1815 in Bali and Lombak, 1699, 1771, 1780, 1815, 1848 and 1852 in Java and 1799, 1833 and 1861 in Sumatra. All of these events caused damage over a broad region notwithstanding high seismic attenuation rates, and are associated with years of temporal and spatial clustering of earthquakes. Several tsunami are recorded with run-up heights > 15 meters. Many islands were engulfed and coastal communities washed away. The earthquakes associated with these events were felt over a region as large as the 2011 Tohoku Earthquake in Japan and were followed by decades of aftershocks. Over the past 160 years no major shallow earthquakes have struck eastern Indonesia, which is characterized as an area incapable of mega

  3. Uranium-Series Ages of Marine Terrace Corals from the Pacific Coast of North America and Implications for Last-Interglacial Sea Level History

    USGS Publications Warehouse

    Muhs, D.R.; Kennedy, G.L.; Rockwell, T.K.

    1994-01-01

    Few of the marine terraces along the Pacific coast of North America have been dated using uranium-series techniques. Ten terrace sequences from southern Oregon to southern Baja California Sur have yielded fossil corals in quantities suitable for U-series dating by alpha spectrometry. U-series-dated terraces representing the ???80,000 yr sea-level high stand are identified in five areas (Bandon, Oregon; Point Arena, San Nicolas Island, and Point Loma, California; and Punta Banda, Baja California); terraces representing the ???125,000 yr sea-level high stand are identified in eight areas (Cayucos, San Luis Obispo Bay, San Nicolas Island, San Clemente Island, and Point Loma, California; Punta Bands and Isla Guadalupe, Baja California; and Cabo Pulmo, Baja California Sur). On San Nicolas Island, Point Loma, and Punta Bands, both the ???80,000 and the ???125,000 yr terraces are dated. Terraces that may represent the ???105,000 sea-level high stand are rarely preserved and none has yielded corals for U-series dating. Similarity of coral ages from midlatitude, erosional marine terraces with coral ages from emergent, constructional reefs on tropical coastlines suggests a common forcing mechanism, namely glacioeustatically controlled fluctuations in sea level superimposed on steady tectonic uplift. The low marine terrace dated at ???125,000 yr on Isla Guadalupe, Baja California, presumed to be tectonically stable, supports evidence from other localities for a +6-m sea level at that time. Data from the Pacific Coast and a compilation of data from other coasts indicate that sea levels at ???80,000 and ???105,000 yr may have been closer to present sea level (within a few meters) than previous studies have suggested.

  4. Significant Tsunami Events

    NASA Astrophysics Data System (ADS)

    Dunbar, P. K.; Furtney, M.; McLean, S. J.; Sweeney, A. D.

    2014-12-01

    Tsunamis have inflicted death and destruction on the coastlines of the world throughout history. The occurrence of tsunamis and the resulting effects have been collected and studied as far back as the second millennium B.C. The knowledge gained from cataloging and examining these events has led to significant changes in our understanding of tsunamis, tsunami sources, and methods to mitigate the effects of tsunamis. The most significant, not surprisingly, are often the most devastating, such as the 2011 Tohoku, Japan earthquake and tsunami. The goal of this poster is to give a brief overview of the occurrence of tsunamis and then focus specifically on several significant tsunamis. There are various criteria to determine the most significant tsunamis: the number of deaths, amount of damage, maximum runup height, had a major impact on tsunami science or policy, etc. As a result, descriptions will include some of the most costly (2011 Tohoku, Japan), the most deadly (2004 Sumatra, 1883 Krakatau), and the highest runup ever observed (1958 Lituya Bay, Alaska). The discovery of the Cascadia subduction zone as the source of the 1700 Japanese "Orphan" tsunami and a future tsunami threat to the U.S. northwest coast, contributed to the decision to form the U.S. National Tsunami Hazard Mitigation Program. The great Lisbon earthquake of 1755 marked the beginning of the modern era of seismology. Knowledge gained from the 1964 Alaska earthquake and tsunami helped confirm the theory of plate tectonics. The 1946 Alaska, 1952 Kuril Islands, 1960 Chile, 1964 Alaska, and the 2004 Banda Aceh, tsunamis all resulted in warning centers or systems being established.The data descriptions on this poster were extracted from NOAA's National Geophysical Data Center (NGDC) global historical tsunami database. Additional information about these tsunamis, as well as water level data can be found by accessing the NGDC website www.ngdc.noaa.gov/hazard/

  5. Insights on the Quaternary Tectonic Evolution of the SE Indonesia Arc-Continent Collision from the Study of Uplifted Coral Terraces on Sumba Island.

    NASA Astrophysics Data System (ADS)

    Leclerc, F.; Rigaud, S.; Chiang, H. W.; Djamil, Y. S.; Herdiyanti, T.; Johnny, J.; Ildefonso, S.; Meilano, I.; Bijaksana, S.; Abidin, H. Z.; Tapponnier, P.; Wang, X.

    2015-12-01

    Sumba Island is uniquely positioned within the Sunda-Banda forearc, at the transition between oceanic subduction and arc-continent collision. There, the convergence between the Sunda and Australian plates is accommodated along at least three major structures: the megathrust, the Savu backthrust located south of Sumba and the Flores backthrust located north of the volcanic arc. The incipient collision in the vicinity of Sumba is responsible for coastal vertical movements. Quaternary reefal deposits form spectacular uplifted flights of terraces, which directly overlie Mid Miocene - Early Pliocene deep carbonate and volcaniclastic rocks at elevations exceeding 500m. Although aerial fossil reefs extensively rim the northern and eastern coasts of Sumba, studies have been limited to Cape Laundi where an uplift rate of 0.2-0.5 m/kyr is estimated for the last 400 kyr, partly on the basis of alpha-spectrometric U/Th dating. At the island scale, the relief morphology and the hydrographic network point to a N-S asymmetry, indicating a general tilt toward the north. A subducting seafloor asperity and south-dipping normal faults have been postulated to generate this asymmetry. However as the pattern and kinematics of the deformation remain partially determined, structures and processes capable of driving such deformation and accommodating the nascent collision may be undisclosed. New topographic data coupled with field observations and coral mass-spectrometric U/Th dating allow investigating the morphology, stratigraphy and age of the fossil reef terraces at the island scale. Tectonic structures disrupting the topography are identified and their activities are relatively dated with respect to fossil reef terraces. The deformation pattern of Sumba is characterized, especially in Cape Laundi where the uplift rate is re-evaluated. Through a multi-disciplinary study, we intend to reconstruct the tectonic evolution of Sumba island and, at a larger scale, of the collision in SE

  6. Utilization of formal health services for children aged 1–5 in Aceh after the 2004 tsunami: Which children did not receive the health care they needed? Implications for other natural disaster relief efforts

    PubMed Central

    Rassekh, Bahie Mary; Santosham, Mathuram

    2014-01-01

    Aceh, Indonesia, was the hardest-hit area in the December 26, 2004 Indian Ocean earthquake and tsunami, with more than 500,000 people displaced, 120,000 people dead, and total damages and losses estimated at $4.5 billion. The relief effort following the tsunami was also immense, with billions of dollars of aid pledged to this province alone. Since then, there have been several natural disasters, including Typhoon Haiyan, which have caused great loss of life and displacement and for which these results are applicable. This study aimed to determine and assess utilization patterns of health services for children under the age of five with diarrhea, cough and difficulty breathing, fever, or skin disease and to identify determinants of formal and non-formal healthcare usage. A household survey of 1439 households was administered to caretakers of children aged 1–5 years. A sample of clusters within Banda Aceh and Aceh Besar were selected and those caretakers within the cluster who fit the inclusion criteria were interviewed. In the two weeks prior to the survey, 78.3% of respondents utilized formal health services as the first line of care for their child's illness episode. Factors significantly associated with decreased formal healthcare usage for the sick children were if the children were living in a displaced household, if the children's mother or father were not living, and if the children's caretaker was not the mother. Although utilization of formal health services for children was quite high after the tsunami, there were certain children who received significantly less care, including those who were displaced, those who were being cared for by someone other than their mother, and those for whom one or both parents had died. Among the recommendations are suggestions to target these children to ensure that they receive the health care they need. PMID:25750772

  7. An evaluation of public, private, and mobile health clinic usage for children under age 5 in Aceh after the tsunami: implications for future disasters

    PubMed Central

    Rassekh, Bahie Mary; Shu, Winnie; Santosham, Mathuram; Burnham, Gilbert; Doocy, Shannon

    2014-01-01

    Background: Aceh, Indonesia, was the hardest-hit area in the 26 December 2004 Indian Ocean earthquake and tsunami, with more than 500,000 people displaced, 120,000 people dead, and total damages and losses estimated at $4.5 billion. The relief effort following the tsunami was also immense. Objectives: This study aimed to determine and assess utilization patterns of formal public versus private and mobile health services for children under age 5 with diarrhea, cough and difficulty breathing, fever, or skin disease and to identify determinants of care usage. Methods: A household survey of 962 households was administered to caretakers of children aged 1–5 years. A sample of clusters within Banda Aceh and Aceh Besar were selected and those caretakers within the cluster who fit the inclusion criteria were interviewed. Results: Of those caretakers who utilized formal health services as the first line of care for their sick child, 62% used a public health facility, 30% used a private health facility, and 8% used a mobile clinic. In terms of significant factors associated with public, private, and mobile care utilization, mobile clinics were at one side of the spectrum and private clinics were at the other side overall, with public care somewhere in between. This was true for several variables. Mobile clinic users reported the lowest cost of services and medicine and the highest perceived level of accessibility, and private care users reported the highest perceived level of satisfaction. Conclusions: Utilization of formal health services for children was quite high after the tsunami. The caretaker's perceived satisfaction with public health services could have been improved. Mobile clinics were an accessible source of health care and could be used in future disaster relief efforts to target those populations that seek less care for their sick children, including displaced populations, and those children whose parents have died. PMID:25750788

  8. Variability on the Hypoxic Conditions in the Northwestern Region of the Baja California Peninsula

    NASA Astrophysics Data System (ADS)

    Bustos-Serrano, H.

    2015-12-01

    The NW region of the Baja California peninsula in México is dominated by the California Current System (CCS). Dissolved oxygen (DO) is a key variable in water bodies because it is considered as a health in biological processes. Hypoxic conditions (DO 60 to 120 μmol kg-1) occur naturally in large areas of the ocean. In the Eastern Pacific, the DO can be altered by eutrophication, derived from anthropogenic activity, especially in shallow and enclosed seas. Fluctuations in the conditions of hypoxia zones may have significant ecological and economic impact. It is of interest in assessing whether hypoxic conditions in the vicinity of Bahia de Todos Santos (BTS) and Coronado Islands in México are altered by anthropogenic activity (Figs. 1 and 2 respectively). For the present study, we worked with data collected from oceanographic expeditions during the period October 2010 to June 2015. The DO was determined using a CTD (SBE Model 25) and by sea water collection with hydrographic bottles using a modification of the Winkler method. The signs of hypoxia are evident in the area near BTS and in the vicinity of Coronado´s Islands, mainly on locations between the Todos Santos Islands and the peninsula of Punta Banda, which shows that the hypoxic zone begins to occur in shallow water between 50-200 m depth. This particular area corresponds to the point where the Mexican Navy determined as a site for dredging materials from the ports of Ensenada and El Sauzal, it is possible that the anthropogenic activity alters the natural conditions of hypoxia in the area to enlarge. In June 2012 for the first time in that region we obtained sediment samples below 700 m depth, which are mixed terrigenous clastic and oceanic sediments.

  9. Seismicity associated with the Sumatra-Andaman Islands earthquake of 26 December 2004

    USGS Publications Warehouse

    Dewey, J.W.; Choy, G.; Presgrave, B.; Sipkin, S.; Tarr, A.C.; Benz, H.; Earle, P.; Wald, D.

    2007-01-01

    The U.S. Geological Survey/National Earthquake Information Center (USGS/ NEIC) had computed origins for 5000 earthquakes in the Sumatra-Andaman Islands region in the first 36 weeks after the Sumatra-Andaman Islands mainshock of 26 December 2004. The cataloging of earthquakes of mb (USGS) 5.1 and larger is essentially complete for the time period except for the first half-day following the 26 December mainshock, a period of about two hours following the Nias earthquake of 28 March 2005, and occasionally during the Andaman Sea swarm of 26-30 January 2005. Moderate and larger (mb ???5.5) aftershocks are absent from most of the deep interplate thrust faults of the segments of the Sumatra-Andaman Islands subduction zone on which the 26 December mainshock occurred, which probably reflects nearly complete release of elastic strain on the seismogenic interplate-thrust during the mainshock. An exceptional thrust-fault source offshore of Banda Aceh may represent a segment of the interplate thrust that was bypassed during the mainshock. The 26 December mainshock triggered a high level of aftershock activity near the axis of the Sunda trench and the leading edge of the overthrust Burma plate. Much near-trench activity is intraplate activity within the subducting plate, but some shallow-focus, near-trench, reverse-fault earthquakes may represent an unusual seismogenic release of interplate compressional stress near the tip of the overriding plate. The interplate-thrust Nias earthquake of 28 March 2005, in contrast to the 26 December aftershock sequence, was followed by many interplate-thrust aftershocks along the length of its inferred rupture zone.

  10. Fotometría UBVI en NGC 6231

    NASA Astrophysics Data System (ADS)

    Baume, G. L.; Vázquez, R. A.; Feinstein, A.

    Se ha realizado fotometría CCD UBVI en la zona del cúmulo abierto NGC 6231, habiéndose observado 1062 estrellas hasta una magnitud V≈ 19. Esto posibilita tener una imagen clara de la parte inferior de la secuencia principal del cúmulo. Combinando nuestros datos con tipos espectrales tomados de la literatura pudimos re-derivar la ley de absorción en dirección a este cúmulo y encontrar que los valores de R muestran variaciones de estrella a estrella. La secuencia principal inferior muestra también algunos rasgos intrigantes: hay un codo notorio en V≈ 13.5 seguido por un gran ``spread'' de magnitudes a color constante entre las estrellas débiles y una inusualmente alta densidad de estrellas a lo largo de una banda que se extiende 1.5 mag encima de la ZAMS. Los cálculos indican que el número esperado de estrellas de campo en dirección al cúmulo debería ser menor que el observado. Una re-evaluación de las funciones de luminosidad y masa dentro de los límites -7.5 < MV < 1.5 mag y 2 Msolar < M arroja pendientes planas para ambas funciones, lo que parece ser típico de cúmulos muy jóvenes. Todos estos rasgos son congruentes con un escenario joven donde las estrellas en fase de contracción están arribando a la secuencia principal.

  11. Taxas de eventos para as fontes astrofísicas do detector Mario Schenberg

    NASA Astrophysics Data System (ADS)

    Castro, C. S.; Araujo, J. C. N.; Miranda, O. D.; Aguiar, O. D.

    2003-08-01

    O detector de ondas gravitacionais Mario Schenberg será sensível a sinais que cheguem à Terra com amplitude h~10-21 e dentro da faixa em frequências que varia de 3,0 a 3,4 kHz. As principais fontes astrofísicas em condições de gerar um sinal detectável pela antena Schenberg são: colapsos estelares que produzam eventos do tipo supernova; instabilidades hidrodinâmicas em estrelas de nêutrons; excitação dos modos fluído (modos f) de estrelas de nêutrons; excitação dos primeiros modos quadrupolares de buracos negros com massa ~ 3,8 M¤; coalescências de estrelas de nêutrons e buracos negros em sistemas binários e, ainda, espiralações de mini-buracos negros. Neste trabalho nós determinamos as taxas de eventos para o Schenberg associadas a dois tipos de fontes: através da de-excitação dos modos f de estrelas de nêutrons e através da coalescência de mini-buracos negros de 0,5 M¤ (que atualmente têm sido colocados como possíveis candidatos a objetos massivos do halo Galáctico). Nós mostramos que esses tipos de fontes poderão produzir sinais em ondas gravitacionais com uma taxa em torno de um evento por ano dentro da banda do Schenberg.

  12. Application of remote sensing in coastal change detection after the tsunami event in Indonesia

    NASA Astrophysics Data System (ADS)

    Lim, H. S.; MatJafri, M. Z.; Abdullah, K.; Saleh, N. Mohd.; Surbakti, M. S.

    2008-10-01

    Shoreline mapping and shoreline change detection are critical in many coastal zone applications. This study focuses on applying remote sensing technology to identify and assess coastal changes in the Banda Aceh, Indonesia. Major changes to land cover were found along the coastal line. Using remote sensing data to detect coastal line change requires high spatial resolution data. In this study, two high spatial data with 30 meter resolution of Landsat TM images captured before and after the Tsunami event were acquired for this purpose. The two satellite images was overlain and compared with pre-Tsunami imagery and with after Tsunami. The two Landsat TM images also were used to generate land cover classification maps for the 24 December 2004 and 27 March 2005, before and after the Tsunami event respectively. The standard supervised classifier was performed to the satellite images such as the Maximum Likelihood, Minimum Distance-to-mean and Parallelepiped. High overall accuracy (>80%) and Kappa coefficient (>0.80) was achieved by the Maximum Likelihood classifier in this study. Estimation of the damage areas between the two dated was estimated from the different between the two classified land cover maps. Visible damage could be seen in either before and after image pair. The visible damage land areas were determined and draw out using the polygon tool included in the PCI Geomatica image processing software. The final set of polygons containing the major changes in the coastal line. An overview of the coastal line changes using Landsat TM images is also presented in this study. This study provided useful information that helps local decision makers make better plan and land management choices.

  13. [Tropical spastic paraparesis in a non tropical region].

    PubMed

    Pias-Peleteiro, L; Pias-Peleteiro, J M; Arias, M

    2015-10-16

    Introduccion. El virus linfotropo humano de celulas T tipo 1 (HTLV-1) es el agente causal de la paraparesia espastica tropical. Su prevalencia, elevada en determinadas areas tropicales, es baja en Europa y Norteamerica. Casos clinicos. Se describen dos casos de paraparesia espastica tropical en varones naturales y residentes en Galicia. Se realizaron estudios analiticos en la sangre y el liquido cefalorraquideo (LCR), examenes neurofisiologicos y resonancia magnetica craneal y medular. En ambos pacientes, la presentacion clinica fue la de una mielopatia cronica, con cuadro torpido y progresivo que evoluciono a paraparesia espastica. Un paciente desarrollo uveitis antes de la clinica neurologica. En los dos casos, el estudio del LCR demostro leve pleocitosis linfoide, ligera hiperproteinorraquia, bandas oligoclonales negativas y anticuerpos anti-HTLV-1 positivos. La reaccion en cadena de la polimerasa para HTLV-1 resulto positiva en ambos casos. La resonancia magnetica raquidea resulto normal en un paciente y mostro en el otro hiperseñal medular dorsal, que desaparecio tras el tratamiento. No se demostraron datos de polineuropatia periferica. Recibieron corticoides e interferon alfa, con leve mejoria y estabilizacion del cuadro clinico. La anamnesis dirigida revelo antecedentes de contactos sexuales de riesgo en regiones endemicas de HTLV-1. Conclusiones. La uveitis asociada a HTLV-1 podria ser predictora de paraparesia espastica tropical. Esta es probablemente una entidad infradiagnosticada (alto porcentaje de portadores asintomaticos, clinica insidiosa y bajo indice de sospecha en areas no endemicas). Debe considerarse su diagnostico en zonas no tropicales que reciben inmigrantes de areas endemicas y tambien en regiones con una tradicional emigracion a regiones tropicales.

  14. [Exercise and nutritional supplements; effects of combined use in people over 65 years; a systematic review].

    PubMed

    Vásquez-Morales, Andrea; Wanden-Berghe, Carmina; Sanz-Valero, Javier

    2013-01-01

    Objetivo: Revisar sistemáticamente la evidencia existente en la literatura científica, acerca de la influencia y los efectos de los suplementos nutricionales sobre la masa y fuerza muscular al combinarse con entrenamiento físico en ancianos sanos. Método: Estudio descriptivo transversal. Se seleccionó la literatura científica de las bases de datos: MEDLINE, EMBASE, ISI, CINAHL, COCHRANE y LILACS; Teniendo en cuenta como criterio de inclusión sólo ensayos clínicos aleatorizados (ECA) y excluyendo documentos que no basaban su estudio en ancianos sanos y que no implementaban un programa de entrenamiento. Resultados: De los 8 artículos seleccionados para la revisión, algunos estudios combinan suplemento con diversas formas de entrenamiento y otros diferentes suplementos con el entrenamiento con resistencia. Los suplementos administrados fueron: Suplemento proteico (bebible), Creatina, Vitamina D y calcio. El entrenamiento asignado fue de resistencia con: pesas, banda elástica, máquinas, ejercicios de equilibrio, orientación y ejercicio aeróbico. Conclusiones: - Combinar el suplemento con ejercicio físico, refuerza los efectos que independientemente cada uno puede tener sobre la mejora de fuerza, balance y velocidad. - La mejora del sistema musculoesquelético favorece la movilidad, contribuyendo a la prevención de sarcopenia y la prolongación de la independencia y autonomía de las personas mayores. - El uso de suplementos debe estar sujeto a un análisis de la ingesta nutricional diaria, las demandas energéticas individuales y la elección de un ejercicio de resistencia física practicado y prolongado en el tiempo, para conservar los beneficios obtenidos.

  15. Los cambios en la velocidad de rotación terrestre y los fenómenos geomagnéticos

    NASA Astrophysics Data System (ADS)

    Gianibelli, J. C.

    Uno de los aspectos importantes relativos a la geodinámica del interior terrestre es la correlación entre los eventos de cambio en la velocidad de rotación terrestre y los determinados en los elementos del campo geomagnético por ejemplo, la Declinación Magnética, o los coeficientes de los modelos matemáticos de representación global de dicho campo. En este trabajo se presentan los resultados de las características espectrales de los cambios observados en la longitud del día (ldd), y su relación con la estructura espectral de las coeficientes de los modelos matemáticos de campo denominados Campo Internacional Geomagnético de Referencia (CIGR). El intervalo estudiado comprende los últimos 100 años. Los resultados muestran una correlación en las bandas de 60 y 30 años, con posibles períodos mucho mayores que no son posibles determinar a partir de los modelos de CIRG. Se efectúa una simulación a partir de los resultados obtenidos por la aplicación del método de máxima entropía con longitudes del filtro predictor de error comprendida entre el 10% y el 95% de la longitud de la serie analizada. Se observan procesos sicrónicos y asincrónicos que, en muy largos intervalos de tiempos, podrían suponerse como caóticos.

  16. The Effect of the Great Barrier Reef on the Propagation of the 2007 Solomon Islands Tsunami Recorded in Northeastern Australia

    NASA Astrophysics Data System (ADS)

    Baba, Toshitaka; Mleczko, Richard; Burbidge, David; Cummins, Phil R.; Thio, Hong Kie

    2008-12-01

    The effect of offshore coral reefs on the impact from a tsunami remains controversial. For example, field surveys after the 2004 Indian Ocean tsunami indicate that the energy of the tsunami was reduced by natural coral reef barriers in Sri Lanka, but there was no indication that coral reefs off Banda Aceh, Indonesia had any effect on the tsunami. In this paper, we investigate whether the Great Barrier Reef (GBR) offshore Queensland, Australia, may have weakened the tsunami impact from the 2007 Solomon Islands earthquake. The fault slip distribution of the 2007 Solomon Islands earthquake was firstly obtained by teleseismic inversion. The tsunami was then propagated to shallow water just offshore the coast by solving the linear shallow water equations using a staggered grid finite-difference method. We used a relatively high resolution (approximately 250 m) bathymetric grid for the region just off the coast containing the reef. The tsunami waveforms recorded at tide gauge stations along the Australian coast were then compared to the results from the tsunami simulation when using both the realistic 250 m resolution bathymetry and with two grids having fictitious bathymetry: One in which the the GBR has been replaced by a smooth interpolation from depths outside the GBR to the coast (the “No GBR” grid), and one in which the GBR has been replaced by a flat plane at a depth equal to the mean water depth of the GBR (the “Average GBR” grid). From the comparison between the synthetic waveforms both with and without the Great Barrier Reef, we found that the Great Barrier Reef significantly weakened the tsunami impact. According to our model, the coral reefs delayed the tsunami arrival time by 5-10 minutes, decreased the amplitude of the first tsunami pulse to half or less, and lengthened the period of the tsunami.

  17. Central African Republic.

    PubMed

    1989-11-01

    The Central African Republic contains 242,000 square miles, which rolling terrain almost 2000 feet above sea level. The climate is tropical, and it has a population of 2.8 million people with a 2.5% growth rate. There are more than 80 ethnic groups including Baya 34%, Banda 28%, Sara 10%, Mandja 9%, Mboum 9%, and M'Baka 7%. The religions are traditional African 35%, protestant 25%, Roman Catholic 25%, and Muslim 15%, and the languages are French and Sangho. The infant mortality rate is 143/1000, with expectancy at 49 years and a 40% literacy rate. The work force of 1 million is 70% agricultural, industry 6% and commerce and service 6% and government 3%. The government consists of a president assisted by cabinet ministers and a single party. Natural resources include diamonds, uranium, timber, gold, and oil, and major industries are beverages, textiles, and soap. Agricultural products feature coffee, cotton, peanuts, tobacco, food crops and livestock. Most of the population live in rural areas and most of the 80 ethnic groups have their own language. This is one of the world's least developed countries, with a per capita income of $375/year. The main problems with development are the poor transportation infrastructure, and the weak internal and international marketing systems. The US and various international organizations have aided in agriculture development, health programs, and family planning. US investment is mainly in diamond and gold mining, and although oil drilling has been successful it is not economically feasible at current prices.

  18. Evaluation of an operational ocean model configuration at 1/12° spatial resolution for the Indonesian seas - Part 2: Biogeochemistry

    NASA Astrophysics Data System (ADS)

    Gutknecht, E.; Reffray, G.; Gehlen, M.; Triyulianti, I.; Berlianty, D.; Gaspar, P.

    2015-08-01

    In the framework of the INDESO (Infrastructure evelopment of Space Oceanography) project, an operational ocean forecasting system was developed to monitor the state of the Indonesian seas in terms of circulation, biogeochemistry and fisheries. This forecasting system combines a suite of numerical models connecting physical and biogeochemical variables to population dynamics of large marine predators (tunas). The physical/biogeochemical coupled component (INDO12BIO configuration) covers a large region extending from the western Pacific Ocean to the Eastern Indian Ocean at 1/12° resolution. The OPA/NEMO physical ocean model and the PISCES biogeochemical model are coupled in "on-line" mode without degradation in space and time. The operational global ocean forecasting system (1/4°) operated by Mercator Ocean provides the physical forcing while climatological open boundary conditions are prescribed for the biogeochemistry. This paper describes the skill assessment of the INDO12BIO configuration. Model skill is assessed by evaluating a reference hindcast simulation covering the last 8 years (2007-2014). Model results are compared to satellite, climatological and in situ observations. Diagnostics are performed on chlorophyll a, primary production, mesozooplankton, nutrients and oxygen. Model results reproduce the main characteristics of biogeochemical tracer distributions in space and time. The seasonal cycle of chlorophyll a is in phase with satellite observations. The northern and southern parts of the archipelago present a distinct seasonal cycle, with higher chlorophyll biomass in the southern (northern) part during SE (NW) monsoon. Nutrient and oxygen concentrations are correctly reproduced in terms of horizontal and vertical distributions. The biogeochemical content of water masses entering in the archipelago as well as the water mass transformation across the archipelago conserves realistic vertical distribution in Banda Sea and at the exit of the archipelago.

  19. Estudio del CH interestelar

    NASA Astrophysics Data System (ADS)

    Olano, C.; Lemarchand, G.; Sanz, A. J.; Bava, J. A.

    El objetivo principal de este proyecto consiste en el estudio de la distribución y abundancia del CH en nubes interestelares a través de la observación de las líneas hiperfinas del CH en 3,3 GHz. El CH es una molécula de amplia distribución en el espacio interestelar y una de las pocas especies que han sido observadas tanto con técnicas de radio como ópticas. Desde el punto de vista tecnológico se ha desarrollado un cabezal de receptor que permitirá la realización de observaciones polarimétricas en la frecuencia de 3,3 GHz, con una temperatura del sistema de 60 K y un ancho de banda de 140 MHz, y que será instalado en el foco primario de la antena parabólica del IAR. El cabezal del receptor es capaz de detectar señales polarizadas, separando las componentes de polarización circular derecha e izquierda. Para tal fin el cabezal consta de dos ramas receptoras que amplificarán la señal y la trasladarán a una frecuencia más baja (frecuencia intermedia), permitiendo de esa forma un mejor transporte de la señal a la sala de control para su posterior procesamiento. El receptor además de tener características polarimétricas, podrá ser usado en el continuo y en la línea, utilizando las ventajas observacionales y de procesamiento de señal que actualmente posee el IAR.

  20. Initiation of subduction by post-collision foreland thrusting and back-thrusting

    NASA Astrophysics Data System (ADS)

    Mitchell, A. H. G.

    1984-07-01

    While postulated causes of initial subduction and trench formation include underthrusting, controls on its location and age have not been determined. Consideration of the age of subduction zones bordering five collisional orogens suggests that subduction may have been initiated by foreland thrusts and back-thrusts. Foreland thrusts develop within a continental foreland on the subducting plate mostly within 50 my of collision with an arc system; where the foreland is narrow the thrusts may intersect the continent-ocean crust boundary. Back-thrusts develop in the fore-arc or back-arc area on the overriding plate within 10 to 20 my of collision, and can result in tectonic burial of the magmatic arc; where the arc system is oceanic the back-thrusts may intersect the arc-ocean crust boundary. Possible examples of subduction initiated by foreland thrusts are the start of subduction in the late Jurassic beneath the northern Sunda Arc, and at the end-Miocene in the Negros Trench. Examples of back-thrusts which have initiated or may initiate subduction are the late Cenozoic eastward translation of Taiwan over the Philippine Sea plate, the incipient southward subduction of the Banda Sea beneath Timor, and the W-dipping back-thrust comprising the Highland Boundary Fault zone and postulated early Ordovician thrusts to the SE in Scotland. The suggested relationship of subduction to collision helps to explain the persistence of Wilson cycles in the still-active late Mesozoic to Cenozoic orogenic belts and implies that orogeny will cease only with collision between major continents.

  1. On the link between orogenic shortening and back-arc extensional collapse in low topography orogens

    NASA Astrophysics Data System (ADS)

    Matenco, L. C.

    2012-04-01

    Classical models of orogenic evolution assume that back arc basins form in the hinterland of orogens, collapsing the upper plate above oceanic subduction zones. This is a common characteristic commonly thought to apply to all low-topography orogens of Mediterranean type driven by the fast roll-back of subducted slabs, or other analogues such as the Miocene to recent evolution of the SE Asia subduction zones. This extension may take place far at the interior of the upper plate, as is the case in various segments of the Carpathians or in the core of the SE Asian domain, but in most cases of the Dinarides, Apennines or Hellenides it take place superposed or far into the foreland of oceanic suture zones. Therefore, the term back-arc extension in many cases is misleading, as exhumation along major detachment zones takes place in the core of the orogen (Rif, Betics), in the accreted crustal material of the lower plate (Apennines, Dinarides) or even in a presumed former fore-arc (Aegean, Sunda-Banda arc). In all these subduction zones, collision has largely duplicated crustal blocks from the lower plate and has gradually shifted subduction zone far towards the lower plate. As a result, crustal thickening takes place in the foreland of the orogen, in contrast with the typical crustal roots of the high convergence orogens, such as the Alps or Himalaya. This demonstrate an active shift of the main subduction zone, the position of slabs detected by teleseismic mantle tomography is displaced to the foreland and cannot be connected with the position of the lower plate crust beneath the orogen. This shift is associated with large scale magmatism with unusual large crustal signatures, atypical for subduction related magmas. These observations demonstrate the need for an active reconsideration of existing orogenic models which should include displacements of subduction zones during orogenic shortening and an active investigation of the role of continental subduction and associated

  2. Variation in forearc basin development along the Sunda Arc, Indonesia

    NASA Astrophysics Data System (ADS)

    van der Werff, W.

    The present forearc basin configuration along the Sunda Arc initially appears to have been controlled by extension and differential subsidence of basement blocks in response to the late Eocene collision of India with Asia. The late Oligocene increase in convergence between the South-east Asian and Indian Plates associated with a new pulse of subduction, resulted in basement uplift and the formation of a regional unconformity that can be recognized along the entire Sunda Arc. From the early to late Miocene, the Sumba and Savu forearc sectors along the eastern Sunda Arc may have been characterized by forearc extension. Submarine fan deposition on the arcward side of the evolving accretionary prism represents the first phase in forearc basin deposition. These fans were subsequently covered by basin and slope sediments derived from the evolving magmatic arc. Structural response to increased late Miocene compression varied along strike of the Sunda Arc. North of Bali, Lombok and Sumbawa, the incipient collision between Australia and the western Banda Arc caused back-arc thrusting and basin inversion. Towards the south of Java, an increase in both the size of the accretionary prism and convergence rates resulted in uplift and large scale folding of the outer forearc basin strata. Along the west coast of Sumatra, increased compression resulted in uplift along the inner side of the forearc along older transcurrent faults. Uplift of West Sumatra was followed by the deposition of a westward prograding sequence of terrigenous sediments that resulted in the development of a broad shelf. Initial forearc basin subsidence relates to the age of the subducting oceanic lithosphere, on top of which the basin is situated. Along the western Sunda Arc, both fexural loading of the evolving accretionary prism, and across arc strike-slip faulting represent additional factors that result in forearc subsidence.

  3. Rotation of horizontal stresses in the Australian North West continental shelf due to the collision of the Indo-Australian and Eurasian Plates

    NASA Astrophysics Data System (ADS)

    Hillis, Richard R.; Mildren, Scott D.; Pigram, Chris J.; Willoughby, Don R.

    1997-04-01

    There is a 40° rotation of regional maximum horizontal stress (σhmax) orientation between the western end of the Australian North West Continental Shelf (Carnarvon Basin) and its eastern end (Bonaparte Basin). A total of 625 borehole breakouts covering a cumulative length of 7.7 km in 42 wells in the Carnarvon Basin indicates a σhmax orientation of 090°-100°N. A total of 616 borehole breakouts over 6.8 km in 46 wells in the Bonaparte Basin indicates a σhmax orientation of 055°N-060°N. Together with extant data from the World Stress Map, these results indicate that regional σhmax orientation is 050°-060°N from New Guinea westward through the Bonaparte Basin to the Canning Basin (central North West Shelf). Between the Canning Basin and the Carnarvon Basin, σhmax rotates to 090°-100°N. The parallelism of σhmax orientation in the Bonaparte Basin to the Australia/Banda Arc collisional zone indicates that this collision is not generating significant net push. Rather, the 050°-060°N σhmax orientation of much of the northern Australian margin is probably controlled by the more mature New Guinea orogen to which it is approximately orthogonal. The observed rotation of σhmax can be explained solely by the focusing of the forces balancing ridge push along collisional segments of the northeastern boundary of the Indo-Australian Plate (such as the New Guinea orogen). Although not required to account for the observed stress rotation, a slab pull force from oceanic Indo-Australian Plate being subducted beneath the Sunda Arc cannot be dismissed.

  4. Subduction Initiation in Eastern Indonesia

    NASA Astrophysics Data System (ADS)

    Hall, R.

    2014-12-01

    Subduction is often reported to be difficult to initiate, yet in the West Pacific and Eastern Indonesia there are many young subduction zones. Few theoretical or modelling studies consider such settings in which subduction commonly began close to boundaries between ocean crust and thickened crust of arc or continental origin. In Eastern Indonesia there are subduction zones at different stages of development. Some young examples such as the Banda Arc developed by propagation of an existing trench into a new area by tearing, probably along an ocean-continent boundary. This 'solves' the problem since the older subducted slab provides the driving force to drag down unsubducted ocean lithosphere. However, similar explanations cannot account for other subduction zones, such as North Sulawesi, nearby examples in which the subducted slab is not yet at 100 km depth, or troughs where subduction appears to be beginning. These examples show that subduction initiated at a point, such as a corner in an ocean basin, where there were very great differences in elevation between land and adjacent ocean floor. Depression of ocean crust by flow of arc/continent crust is associated with granitic magmatism and detachments within the upper crust. Once the oceanic corner reaches depths of c.100 km, eclogite formation may lead to slab pull that causes the new subduction zone to grow in both directions along strike; arc magmatism may or may not begin. The close relationship between subduction and extension in Eastern Indonesia links dramatic elevation of land, exhumation of deep crust, and spectacular subsidence of basins imaged by oil exploration seismic and multibeam data. Exhumed granites and high-grade metamorphic rocks at elevations up to 3 km, separated by Neogene alluvial sediments from carbonate reefs now at depths of 2 kilometres, imply vertical movements of several kilometres in a few million years. These observations raise the question of whether subduction is driving extension

  5. The Sumba enigma: Is Sumba a diapiric fore-arc nappe in process of formation?

    NASA Astrophysics Data System (ADS)

    Audley-Charles, M. G.

    1985-10-01

    The anomalous updomed morphological expression of Sumba island, its enigmatic lack of strong Neogene deformation and the northward morphological indentation of southern Sumbawa and Flores require explanation. The stratigraphy of Sumba may be correlated with the Cretaceous to Miocene part of the Timor allochthon. The sedimentary and eruptive rock succession in Sumba shows remarkable similarities with the allochthonous Palelo, Wiluba and Cablac deposits of Timor. In both islands the Cretaceous parts of these sequences are regarded as characteristic of fore-arc deposits built on thin continental crust. The Timor nappe is interpreted as a 5 km thick tectonic flake of the Banda fore-arc thrust onto the Australian continental margin in the mid-Pliocene collision. The postulated Sumba nappe has not yet been thrust onto the Australian margin which, in the Sumba region, has not yet converged as close to the arc as in the Timor area. The postulated Sumba nappe is interpreted as a diapiric elongated dome of the Sunda fore-arc that is being squeezed by the converging margin of Australia against the volcanic islands of Sumbawa and Flores. The absence of indications on the seismic reflection profiles for the presence of the thrust fault of the Sumba nappe may perhaps be explained by the thrusts being nearly horizontal within flat-lying strata. The Savu thrust is correlated with the probably older (pre-Late Pliocene) Wetar Suture as a major southward dipping lithospheric rupture. East of 124°E, this suture does not seem to have moved much since the mid-Pliocene collision that emplaced the nappes on Timor. However, microearthquake data suggest some activity is continuing.

  6. Análise da medição do raio solar em ultravioleta

    NASA Astrophysics Data System (ADS)

    Saraiva, A. C. V.; Giménez de Castro, C. G.; Costa, J. E. R.; Selhorst, C. L.; Simões, P. J. A.

    2003-08-01

    A medição acurada do raio solar em qualquer banda do espectro eletromagnético é de relevância na formulação e calibração de modelos da estrutura e atmosfera solar. Esses modelos atribuem emissão do contínuo do Sol calmo em microondas à mesma região da linha Ha do Hell. Apresentamos a medição do raio solar em UV com imagens do EIT (Extreme Ultraviolet Image Telescope) entre 1996 e 2002, no comprimento de onda 30,9 nm (Ha do Hell), que se forma na região de transição/cromosfera solar. A técnica utilizada para o cálculo do raio UV foi baseada na transformada Wavelet B3spline. Fizemos um banco de dados com 1 imagem por dia durante o período citado. Obtivemos como resultado o raio médio da ordem de 975.61" e uma diminuição do mesmo para o período citado variando em média -0,45" /ano. Comparamos estes dados com os valores obtidos pelo ROI (Radio Observatório de Itapetinga) em 22/48 GHz e Nobeyama Radio Heliograph em 17 GHz mostrando que os raios médios são muito próximos o que indica que a região de formação nessas freqüências é a mesma conforme os modelos. Comparamos os resultados também com outros índices de atividade solar.

  7. Estudio fotométrico y espectroscópico de dos cúmulos abiertos jóvenes del disco con apariencia globular

    NASA Astrophysics Data System (ADS)

    Piatti, A. E.; Clariá, J. J.; Bica, E.

    Se presentan y discuten resultados obtenidos en el CASLEO y en el Observatorio de Las Campanas de dos cúmulos abiertos compactos con apariencia globular: Westerlund1 (BH197), ubicado en dirección hacia el centro galáctico, y Westerlund2. A partir de espectroscopía CCD integrada de ambos e imágenes CCD en las bandas VI obtenidas para el primero de ellos, se derivan sus parámetros fundamentales y se examinan sus apariencias estructurales. Se encuentra que Westerlund1 es un cúmulo joven (7 ± 3 millones de años), ubicado sobre el plano galáctico a 1.0 ± 0.4 kpc del sol, en una región caracterizada por una absorción excepcionalmente elevada (Av~=13.0 mag), en tanto que Westerlund2 es también un cúmulo joven (4-6 millones de años) ubicado sobre el plano, en una región afectada por una absorción menor (Av~=5.7 mag). Desde el punto de vista estructural, Westerlund 1 se presenta como uno de los pocos cúmulos abiertos jóvenes de la Galaxia con apariencia tipicamente globular, en contraste con los cúmulos azules de las Nubes de Magallanes en los cuales la apariencia globular constituye un fenómeno común. Westerlund2, aunque menos rico en estrellas, puede también ser incluído dentro de esta interesante clase de objetos.

  8. A eficiência de formação estelar em Musca

    NASA Astrophysics Data System (ADS)

    Hickel, G. R.; Vilas-Boas, J. W. S.; Roberto, A. J.., Jr.; Khan, R. P.

    2003-08-01

    Apresentamos os resultados de um survey no infravermelho próximo (bandas J e H), executado no Laboratório Nacional de Astrofísica, na direção da nuvem escura em forma de filamento de Musca (observamos ao longo de todo o filamento, além de todas as fontes pontuais IRAS e/ou fontes ROSAT brilhantes a uma distância de 2o da nuvem). Nosso objetivo é determinar a eficiência de formação estelar para esta nuvem escura (massa de estrelas formadas/massa da nuvem), procurando por objetos estelares jovens de pequena massa no seu interior e/ou evoluídos o suficiente para estarem afastados do local de nascimento, mas ainda mostrando características de objetos pré-seqüência principal como emissão de raios-X e excesso de emissão no infravermelho próximo. Este survey não estabeleceu nenhum viés na seleção de fontes pontuais IRAS ou fontes ROSAT, uma vez que a imensa maioria das fontes pontuais IRAS nesta região têm qualidade de fluxo ruim. Os candidatos a objetos estelares jovens foram selecionados pelo excesso no índice de cor (J-H), descontados os efeitos da extinção interestelar na linha de visada, determinada através da emissão estendida no infravermelho distante (IRAS). Estimativas de massa foram feitas para estes candidatos, através da relação massa-luminosidade, para calcular a eficiência de formação estelar de Musca.

  9. A importância da poeira e ondas de Alfvén na estabilidade de nuvens moleculares anãs

    NASA Astrophysics Data System (ADS)

    Falceta-Gonçalves, D.; de Juli, M. C.; Jatenco-Pereira, V.

    2003-08-01

    Nuvens moleculares anãs se apresentam dinamicamente estáveis, embora possuam massas muito maiores que a massa de Jeans. Por este motivo, a estabilidade destes objetos não pode ser explicada considerando-se apenas a pressão térmica. Campos magnéticos, aproximadamente uniformes e de ~mG, exercem um termo extra de pressão que sustenta a nuvem, mas somente na direção perpendicular às linhas de campo. Para a direção paralela, ondas de Alfvén geradas por turbulências no meio, por exemplo, têm sido utilizadas. Estas, sendo supostamente fracamente amortecidas, poderiam sustentar a nuvem nesta direção. Entretanto, estes meios contêm grandes quantidades de poeira carregada eletricamente. Estes grãos de poeira possuem frequências cíclotron, que podem entrar em ressonância com as ondas. Neste trabalho calculamos os efeitos que o amortecimento cíclotron da poeira teriam na propagação da onda, e consequentemente na estabilidade da nuvem. Considerando um fluxo de ondas, com um dado espectro de frequências, e uma população de grãos de poeira, com distribuição de tamanho observada, foi possível mostrar que o amortecimento é eficiente em uma larga banda de frequências. Neste caso as ondas seriam rapidamente amortecidas gerando pequenas condensações de alta densidade, e não poderiam ser utilizadas para explicar a estabilidade de uma nuvem inteira. Desta forma, rotação e turbulência seriam candidatos alternativos para garantir a estabilidade destes objetos.

  10. Spondylotic myelopathy mimicking myelitis: diagnostic clues by magnetic resonance imaging.

    PubMed

    Rua, Adriana; Blanco, Yolanda; Sepúlveda, María; Sola-Valls, Núria; Martínez-Hernández, Eugenia; Llufriu, Sara; Berenguer, Joan; Graus, Francesc; Saiz, Albert

    2015-12-01

    Introduccion. La mielopatia espondilotica es la causa mas frecuente de mielopatia no traumatica. Sus caracteristicas radiologicas en ocasiones son indistinguibles de las de una mielopatia inflamatoria, y pueden ocasionar retrasos diagnosticos o llevar a un diagnostico y tratamiento incorrectos. La descripcion reciente de un patron caracteristico de realce de gadolinio puede ayudar a diferenciar la mielopatia espondilotica de la causa inflamatoria. Casos clinicos. Caso 1: varon de 38 años que consulto por historia de dos años de evolucion de parestesias en las extremidades superiores, a las que se añadieron un año mas tarde calambres en las extremidades derechas y acorchamiento en los dermatomas C5 y C6 en relacion con los movimientos del cuello. Caso 2: varon de 44 años que consulto por historia de un año de evolucion de alteracion progresiva de la marcha con trastorno sensitivo en las manos y disfuncion vesical reciente. En ambos casos, la resonancia magnetica medular mostro en las secciones sagitales una hiperseñal cervical fusiforme en T2, asociada a una banda transversa de realce de gadolinio en forma de barra (pancakelike) justo por debajo de la zona de maxima estenosis, y un realce circunferencial o hemimedular en los cortes axiales. Conclusiones. Las caracteristicas radiologicas de la mielopatia espondilotica pueden parecerse a las de origen inflamatorio. El reconocimiento de un realce transverso en barra inmediatamente por debajo del lugar de maxima compresion como signo radiologico tipico de la mielopatia espondilotica es importante para reducir el riesgo de errores diagnosticos, y de utilidad para el manejo de estos pacientes.

  11. Surface water processes in the Indonesian Throughflow as documented by a high-resolution coral (Delta)14C record

    SciTech Connect

    Fallon, S J; Guilderson, T P

    2008-04-23

    To explore the seasonal to decadal variability in surface water masses that contribute to the Indonesian Throughflow we have generated a 115-year bi-monthly coral-based radiocarbon time-series from a coral in the Makassar Straits. In the pre-bomb (pre-1955) era from 1890 to 1954, the radiocarbon time series occasionally displays a small seasonal signal (10-15{per_thousand}). After 1954 the radiocarbon record increases rapidly, in response to the increased atmospheric {sup 14}C content caused by nuclear weapons testing. From 1957 to 1986 the record displays clear seasonal variability from 15 to 60{per_thousand} and the post-bomb peak (163 per mil) occurred in 1974. The seasonal cycle of radiocarbon can be attributed to variations of surface waters passing through South Makassar Strait. Southern Makassar is under the influence of the Northwest Monsoon, which is responsible for the high Austral summer radiocarbon (North Pacific waters) and the Southeast Monsoon that flushes back a mixture of low (South Pacific and upwelling altered) radiocarbon water from the Banda Sea. The coral record also shows a significant {sup 14}C peak in 1955 due to bomb {sup 14}C water advected into this region in the form of CaCO{sub 3} particles (this implies that the particles were advected intact and then become entrapped in the coral skeleton--is this what we really mean? Wouldn't even fine particles settle out over the inferred transit time from Bikini to MAK?) or water particles with dissolved labeled CO{sub 2} produced during fallout from the Castle tests in 1954.

  12. Seismicity of the Earth 1900-2012 Sumatra and vicinity

    USGS Publications Warehouse

    Hayes, Gavin P.; Bernardino, Melissa; Dannemann, Fransiska; Smoczyk, Gregory; Briggs, Richard W.; Benz, Harley M.; Furlong, Kevin P.; Villaseñor, Antonio

    2013-01-01

    The plate boundary southwest of Sumatra is part of a long tectonic collision zone that extends over 8,000 km from Papua, New Guinea, in the east to the Himalayan front in the west. The Sumatra-Andaman part of the collision zone forms a subduction zone plate boundary, which accommodates convergence between the Indo-Australia and Sunda plates. This convergence is responsible for the intense seismicity in Sumatra. The Sumatra Fault, a major transform structure that bisects Sumatra, accommodates the northwest-increasing lateral component of relative plate motion. Most strain accumulation and release between the two plates occurs along the Sunda megathrust. The increasingly oblique convergence moving northwest is accommodated by crustal seismicity along several transform and normal faults, including the Sumatra Fault. Plate-boundary related deformation is also not restricted to the subduction zone and overriding plate: the Indo-Australian plate actually comprises two somewhat independent plates (India and Australia) that are joined along a broad, actively deforming region that produces seismicity up to several hundred kilometers west of the trench. This deformation is exemplified by the recent April 2012 earthquake sequence, which includes the April 11 M 8.6 and M 8.2 strike-slip events and their subsequent aftershocks. Since 2004, much of the Sunda megathrust between the northern Andaman Islands and Enggano Island, a distance of more than 2,000 km, has ruptured in a series of large subduction zone earthquakes—most rupturing the plate boundary south of Banda Aceh. These events include the great M 9.1 earthquake of December 26, 2004; the M 8.6 Nias Island earthquake of March 28, 2005; and two earthquakes on September 12, 2007, of M 8.5 and M 7.9. On October 25, 2010, a M 7.8 on the shallow portion of the megathrust to the west of the Mentawai Islands caused a substantial tsunami on the west coast of those islands.

  13. ALHAMBRA-survey: a new tool for photo-z calibrations in absence of spec-z information

    NASA Astrophysics Data System (ADS)

    Molino Benito, A.; Benitez Lozano, N.; The Alhambra-Team

    2013-05-01

    La estimación de los desplazamientos al rojo (redshift) de las galaxias, derivados mediante fotometría multi-banda, se conoce con el nombre de photometric redshifts (photo-z). Es bien sabido que la precisión alcanzable por estas técnicas puede verse incrementada si se dispone de una muestra espectroscópica de galaxias (cuyos redshifts (spec-z) sean conocidos) con la que re-calibrar los puntos cero fotométricos. (Coe et al. 2006, Ilbert et al. 2008, Molino et al. 2012 in prep). ALHAMBRA-survey, que es un cartografiado extragaláctico (de ˜4 grados cuadrados) dedicado a la realización de un estudio de la evolución de las propiedades y contenido del Universo (Moles et al. 2005, 2008), presenta solapamientos parciales con otros cartografiados espectroscópicos ya existentes con el objetivo de validar y mejorar la precisión de sus photo-z. Sin embargo, dada la variabilidad fotométrica entre sus campos, resulta ineficiente extrapolar las correcciones de punto cero, introduciendo sesgos de inhomogeneidad en la precisión de los resultados. En este trabajo se presenta una nueva metodología que permite mejorar la calibración de los puntos cero fotométricos mediante la utilización de la información estadística proporcionada por los propios photo-z. Mediante esta técnica resulta posible no sólo mejorar la precisión de las estimaciones sino, además, soslayar la necesidad de obtener grandes muestras espectroscópicas.

  14. Tectonic controls of Mississippi Valley-type lead-zinc mineralization in orogenic forelands

    USGS Publications Warehouse

    Bradley, D.C.; Leach, D.L.

    2003-01-01

    Most of the world's Mississippi Valley-type (MVT) zinc-lead deposits occur in orogenic forelands. We examine tectonic aspects of foreland evolution as part of a broader study of why some forelands are rich in MVT deposits, whereas others are barren. The type of orogenic foreland (collisional versus Andean-type versus inversion-type) is not a first-order control, because each has MVT deposits (e.g., Northern Arkansas, Pine Point, and Cevennes, respectively). In some MVT districts (e.g., Tri-State and Central Tennessee), mineralization took place atop an orogenic forebulge, a low-amplitude (a few hundred meters), long-wavelength (100-200 km) swell formed by vertical loading of the foreland plate. In the foreland of the active Banda Arc collision zone, a discontinuous forebulge reveals some of the physiographic and geologic complexities of the forebulge environment, and the importance of sea level in determining whether or not a forebulge will emerge and thus be subject to erosion. In addition to those on extant forebulges, some MVT deposits occur immediately below unconformities that originated at a forebulge, only to be subsequently carried toward the orogen by the plate-tectonic conveyor (e.g., Daniel's Harbour and East Tennessee). Likewise, some deposits are located along syn-collisional, flexure-induced normal and strike-slip faults in collisional forelands (e.g., Northern Arkansas, Daniel's Harbour, and Tri-State districts). These findings reveal the importance of lithospheric flexure, and suggest a conceptual tectonic model that accounts for an important subset of MVT deposits-those in the forelands of collisional orogens. The MVT deposits occur both in flat-lying and in thrust-faulted strata; in the latter group, mineralization postdated thrusting in some instances (e.g., Picos de Europa) but may have predated thrusting in other cases (e.g., East Tennessee).

  15. Issues in Indonesia's tsunami disaster management system revealed after the 2004 Sumatra event

    NASA Astrophysics Data System (ADS)

    Sugimoto, M.; Koyama, A.; Sun, H.; Kang, I.; Arakawa, T.; Kobayashi, J.; Nagata, M.; Nakanishi, R.; Nakano, M.; Noguchi, S.

    2014-12-01

    During the 2004 Indian Ocean Tsunami, Indonesia had the largest number of casualties around 170,000. International society has supported tsunami early warning system, disaster management and disaster education for Indonesia. The past ten years saw several tsunamis in Indonesia after the 2004 Indian Ocean tsunami. Construction of tsunami early warning system was not in time the 2006 Pangandaran tsunami in Jawa Island. On the other hand, tsunami science has been developed for this decade. Tsunami early warning system has been developed by deep ocean pressure gauges (DART system), coastal tide gauges, GPS buoys and so on. Tsunami folklore has been collected and used education and connected with tsunami deposit. However, the tsunami early warning system and other science application were not widely used at once in Indonesia. GPS buoys were stolen by fishery people. One tsunami evacuation building are not used for evacuation by local people in Aceh Sumatra Island in 2012 though locations of the buildings were selected by scientific numerical simulation. Big panic and trafic accidents occurred by M8.6 earthquake in Aceh in April 2012 and reveal lack of disaster management planning in urban planning during reconstruction (Fig.1: Trafic jam in Banda Aceh, source MSN news photo). In addition to this, the 2011 Tohoku earthquake and tsunami reveal fragilities tsunami preparedness. How should we decide to use the tsunami science? We research field situation in Aceh the after 10 years past from the 2004 Sumatra event. This presentation discusses issues of the gap between tsunami science and operations through field research in Aceh now.

  16. Protótipo do primeiro interferômetro brasileiro - BDA

    NASA Astrophysics Data System (ADS)

    Cecatto, J. R.; Fernandes, F. C. R.; Neri, J. A. C. F.; Bethi, N.; Felipini, N. S.; Madsen, F. R. H.; Andrade, M. C.; Soares, A. C.; Alonso, E. M. B., Sawant, H. S.

    2004-04-01

    A interferometria é uma poderosa ferramenta usada para investigar estruturas espaciais de fontes astrofísicas fornecendo uma riqueza de detalhes inatingível pelas técnicas convencionais de imageamento. Em particular, a interferometria com ondas de rádio abre o horizonte de conhecimento do Universo nesta ampla banda do espectro eletromagnético, que vai de cerca de 20 kHz até centenas de GHz já próximo ao infravermelho, e que está acessível a partir de instrumentos instalados em solo. Neste trabalho, apresentamos o interferômetro designado por Arranjo Decimétrico Brasileiro (BDA). Trata-se do primeiro interferômetro a ser desenvolvido no Brasil e América Latina que já está em operação na fase de protótipo. Apresentamos o desenvolvimento realizado até o momento, o sítio de instalação do instrumento, o protótipo e os principais resultados dos testes de sua operação, as perspectivas futuras e a ciência a ser desenvolvida com o instrumento nas fases II e III. Neste trabalho é dada ênfase ao desenvolvimento, testes de operação e principais resultados do protótipo. É discutida brevemente a ciência que pode ser feita com o instrumento. Tanto os detalhes técnicos quanto os principais parâmetros estimados para o instrumento nas próximas fases de desenvolvimento e o desempenho do protótipo serão publicados em breve.

  17. Unraveling topography around subduction zones from laboratory models

    NASA Astrophysics Data System (ADS)

    Husson, Laurent; Guillaume, Benjamin; Funiciello, Francesca; Faccenna, Claudio; Royden, Leigh H.

    2012-03-01

    The relief around subduction zones results from the interplay of dynamic processes that may locally exceed the (iso)static contributions. The viscous dissipation of the energy in and around subduction zones is capable of generating kilometer scale vertical ground movements. In order to evaluate dynamic topography in a self-consistent subduction system, we carried out a set of laboratory experiments, wherein the lithosphere and mantle are simulated by means of Newtonian viscous materials, namely silicone putty and glucose syrup. Models are kept in their most simple form and are made of negative buoyancy plates, of variable width and thickness, freely plunging into the syrup. The surface of the model and the top of the slab are scanned in three dimensions. A forebulge systematically emerges from the bending of the viscous plate, adjacent to the trench. With a large wavelength, dynamic pressure offsets the foreside and backside of the slab by ~ 500 m on average. The suction, that accompanies the vertical descent of the slab depresses the surface on both sides. At a distance equal to the half-width of the slab, the topographic depression amounts to ~ 500 m on average and becomes negligible at a distance that equals the width of the slab. In order to explore the impact of slab rollback on the topography, the trailing edge of the plates is alternatively fixed to (fixed mode) and freed from (free mode) the end wall of the tank. Both the pressure and suction components of the topography are ~ 30% lower in the free mode, indicating that slab rollback fosters the dynamic subsidence of upper plates. Our models are compatible with first order observations of the topography around the East Scotia, Tonga, Kermadec and Banda subduction zones, which exhibit anomalous depths of nearly 1 km as compared to adjacent sea floor of comparable age.

  18. Variabilidade óptica de longo período e precessão de jato: o caso de BL Lacertae

    NASA Astrophysics Data System (ADS)

    Caproni, A.; Abraham, Z.

    2003-08-01

    Variabilidade é tipicamente uma característica de AGNs, sendo observada em toda a faixa eletromagnética. Em relação às escalas de tempo, variações desde horas até de algumas décadas foram encontradas por vários autores. Em alguns casos, análises temporais de curvas de luz mostram a existência de periodicidade nas variações observadas. Um exemplo de objeto que preenche as características mencionadas acima é BL Lacertae, o protótipo da classe BL Lac dos AGNs. Neste trabalho, nós interpretamos a variabilidade periódica de longo período detectada na curva de luz na banda B (~7,5 anos) como o resultado da periodicidade na amplificação da radiação oriunda do jato relativístico. Neste cenário, a amplificação periódica seria induzida pela precessão, que muda o ângulo entre o jato e a linha de visada. Com esta abordagem e vínculos adicionais fornecidos por observações em altas energias, nós podemos impor limites para os parâmetros do modelo de precessão, tais como o fator de Lorentz associado ao movimento global do jato, o ângulo de abertura do cone de precessão e o ângulo entre o eixo do cone e a linha de visada.

  19. Stable isotopes of helium, nitrogen and carbon in a coastal submarine hydrothermal system

    NASA Astrophysics Data System (ADS)

    Vidal, Francisco V.; Welhan, John; Vidal, Victor M. V.

    1982-03-01

    Geothermal gases from submarine and subaerial hot springs in Ensenada, Baja California Norte, Mexico, were sampled for determination of gas chemistry and helium, nitrogen and stable carbon isotope composition. The submarine hot spring gas is primarily nitrogen (56.1% by volume) and methane (43.5% by volume), whereas nearby subaerial hot spring gases are predominantly nitrogen (95-99% by volume). The N 2/Ar ratios and σ 15N values of the subaerial hot spring gas indicate that it is atmospheric air, depleted in oxygen and enriched in helium. The submarine hot spring gas is most probably derived from marine sediments of Cretaceous age rich in organic matter. CH 4 is a major component of the gas mixture ( σ 13C = -44.05% 0), with only minor amounts of CO 2 ( σ13C= -10.46% 0). The σ 15N of N 2 is + 0.2% 0 with a very high N 2/Ar ratio of 160. The calculated isotopic equilibra tion temperature for CH 4CO 2 carbon exchange at depth in the Punta Banda submarine geothermal field is approximately 200°C in agreement with other geothermometry estimates. The 3He/ 4He ratios of the hot spring gases range from 0.3 to 0.6 times the atmospheric ratio, indicating that helium is predominantly derived from the radioactive decay of U and Th within the continental crust. Thus, not all submarine hydrothermal systems are effective vehicles for mantle degassing of primordial helium.

  20. A numerical study of the barotropic tides and tidal energy distribution in the Indonesian seas with the assimilated finite volume coastal ocean model

    NASA Astrophysics Data System (ADS)

    Ding, Yang; Bao, Xianwen; Yu, Huaming; Kuang, Liang

    2012-04-01

    The tides and tidal energetics in the Indonesian seas are simulated using a three-dimensional finite volume coastal ocean model. The high-resolution coastline-fitted model is configured to better resolve the hydrodynamic processes around the numerous barrier islands. A large model domain is adopted to minimize the uncertainty adjacent to open boundaries. The model results with elevation assimilation based on a simple nudge scheme faithfully reproduced the general features of the barotropic tides in the Indonesian Seas. The mean root-mean-square errors between the observed and simulated tidal constants are 2.3, 1.1, 2.4, and 1.5 cm for M2, S2, K1, and O1, respectively. Analysis of the model solutions indicates that the semidiurnal tides in the Indonesian Seas are primarily dominated by the Indian Ocean, whereas the diurnal tides in this region are mainly influenced by the Pacific Ocean, which is consistent with previous studies. Examinations of tidal energy transport reveal that the tidal energy for both of the simulated tidal constituents are transported from the Indian Ocean into the IS mainly through the Lombok Strait and the Timor Sea, whereas only M2 energy enters the Banda Sea and continues northward. The tidal energy dissipates the most in the passages on both sides of Timor Island, with the maximum M2 and K1 tidal energy transport reaching about 750 and 650 kW m-1, respectively. The total energy losses of the four dominant constituents in the IS are nearly 338 GW, with the M2 constituent dissipating 240.8 GW. It is also shown that the bottom dissipation rate for the M2 tide is about 1-2 order of magnitudes larger than that of the other three tidal components in the Indonesian seas.

  1. [Not Available].

    PubMed

    Viñuela García, Manuel; Vera Ibáñez, Antonio; Colomer Poveda, David; Márquez Sánchez, Gonzalo; Romero Arenas, Salvador

    2016-01-01

    Introducción: actualmente los programas de entrenamiento interválicos de alta intensidad parecen ser una forma de optimizar el tiempo, provocando cambios en la composición corporal debido a la activación de diferentes mecanismos hormonales y metabólicos.Objetivo: observar el efecto de cuatro semanas de entrenamiento de esprints repetidos basados en la prueba de Wingate sobre la potencia y la composición corporal en adultos jóvenes.Métodos: los participantes (22,4 ± 1,8 años) fueron asignados aleatoriamente a un grupo experimental o a un grupo control. Antes de comenzar y al acabar el periodo experimental, a los sujetos se les realizó una densitometría de cuerpo completo y una prueba de Wingate. El grupo experimental realizó 12 sesiones de esprints repetidos, realizando de 3 a 6 esprints de 30 segundos con un tiempo de recuperación de 4 minutos. El grupo control continuó con su rutina diaria y no se le aplicó ningún tipo de intervención.Resultados: en el grupo experimental, la potencia media y máxima incrementó un 9,4-16,5% (p < 0,001). Además, disminuyó la masa grasa total un 8,1% (p < 0,028) y la grasa abdominal un 10,0% (p < 0,038). El grupo control no sufrió cambios en ninguna de las variables estudiadas.Conclusiones: cuatro semanas de entrenamiento de esprints repetidos basados en la prueba de Wingate con un volumen específico de ~3 minutos por sesión y una frecuencia de 3 sesiones por semana, muestra mejoras estadísticamente significativas en la potencia máxima y media. Además, provoca cambios en la composición corporal, principalmente en la masa grasa total y de la zona abdominal. PMID:27513499

  2. [Not Available].

    PubMed

    Viñuela García, Manuel; Vera Ibáñez, Antonio; Colomer Poveda, David; Márquez Sánchez, Gonzalo; Romero Arenas, Salvador

    2016-06-30

    Introducción: actualmente los programas de entrenamiento interválicos de alta intensidad parecen ser una forma de optimizar el tiempo, provocando cambios en la composición corporal debido a la activación de diferentes mecanismos hormonales y metabólicos.Objetivo: observar el efecto de cuatro semanas de entrenamiento de esprints repetidos basados en la prueba de Wingate sobre la potencia y la composición corporal en adultos jóvenes.Métodos: los participantes (22,4 ± 1,8 años) fueron asignados aleatoriamente a un grupo experimental o a un grupo control. Antes de comenzar y al acabar el periodo experimental, a los sujetos se les realizó una densitometría de cuerpo completo y una prueba de Wingate. El grupo experimental realizó 12 sesiones de esprints repetidos, realizando de 3 a 6 esprints de 30 segundos con un tiempo de recuperación de 4 minutos. El grupo control continuó con su rutina diaria y no se le aplicó ningún tipo de intervención.Resultados: en el grupo experimental, la potencia media y máxima incrementó un 9,4-16,5% (p < 0,001). Además, disminuyó la masa grasa total un 8,1% (p < 0,028) y la grasa abdominal un 10,0% (p < 0,038). El grupo control no sufrió cambios en ninguna de las variables estudiadas.Conclusiones: cuatro semanas de entrenamiento de esprints repetidos basados en la prueba de Wingate con un volumen específico de ~3 minutos por sesión y una frecuencia de 3 sesiones por semana, muestra mejoras estadísticamente significativas en la potencia máxima y media. Además, provoca cambios en la composición corporal, principalmente en la masa grasa total y de la zona abdominal.

  3. [Efficiency of initiation with ambrisentan versus bosentan in the treatment of pulmonary arterial hypertension].

    PubMed

    Villa, Guillermo; Morano, Raúl; Román, Antonio; Gil, Joan

    2013-01-01

    Objetivo: Se pretende evaluar la eficiencia del tratamiento secuencial de combinación de la hipertensión arterial pulmonar iniciado con antagonistas del receptor de la endotelina, ambrisentan o bosentan, seguido de inhibidores de la fosfodiesterasa- 5 y prostanoides, desde la perspectiva del Sistema Nacional de Salud. Métodos: Se desarrolló un modelo de Markov basado en las cuatro clases funcionales de la New York Heart Association. Un panel de tres expertos alcanzó un consenso sobre el manejo del paciente basado en la práctica clínica. Los pacientes revisaron su tratamiento cada 12 semanas, en función de su estado de salud y de la medicación recibida previamente. Se incluyeron costes farmacológicos y costes asociados al manejo de eventos adversos (EA) muy frecuentes, en un horizonte de 60 semanas. Los resultados se expresaron en términos de los años de vida ajustados por calidad (AVAC). Se realizó un análisis de sensibilidad probabilístico. Resultados: No se encontraron diferencias clínicamente relevantes en los AVAC por paciente y año para el inicio con ambrisentan y bosentan: 0,6853 y 0,6902, respectivamente. El inicio con ambrisentan resultó en un coste farmacológico y asociado al manejo de EA menor: 35.550 ??y 117 ??frente a 40.224 ??y 171 ?. En el análisis de sensibilidad, el inicio con ambrisentan presentó una diferencia de costes totales negativa y significativa: -4.982 ?; IC95%[-8.014 ?; -2.500 ?]; mientras que no se detectaron diferencias significativas en los AVAC: -0,0044; IC95%[-0,0189; 0,0101]. Conclusiones: El tratamiento secuencial de combinación de la HAP iniciado con ambrisentan, seguido de inhibidores de la fosfodiesterasa- 5 y prostanoides, proporciona resultados en salud comparables y menores costes que el tratamiento iniciado con bosentan.

  4. Use of black vulture (Coragyps atratus) in complementary and alternative therapies for cancer in Colombia: A qualitative study

    PubMed Central

    2012-01-01

    Background Although Coragyps atratus has been used as a traditional therapy for patients with cancer, the scientific literature does not contain enough information on how this therapy is used or the mechanisms that explain this therapeutic practice. Objectives To understand the methods of use and the reasons given by patients and caregivers for the use of Coragyps atratus in cancer treatment. Methods This study used a qualitative design based on twenty in-depth interviews of patients with cancer or caregivers of patients with the disease. The analysis of the text was based on an inductive thematic approach. Results Resistance to disease and immune enhancement are properties attributed to Coragyps atratus when used for cancer treatment. The most recommended method of use is fresh blood ingestion, and the associated mechanism of action is transfer of immune factors to the individual who consumes it. Conclusions Use of Coragyps atratus as a treatment for cancer is a popular alternative therapy in Colombia. More studies are needed to understand the clinical effects of this intervention in cancer patients. Spanish abstract Introducción Aunque Coragyps atratus se usa tradicionalmente como terapia para pacientes con cáncer, no existe suficiente información en la literatura científica sobre su forma de utilización ni sobre los mecanismos explicativos que subyacen a esta práctica terapéutica. Objetivos Conocer métodos de utilización y mecanismos explicativos dados por los pacientes y cuidadores de pacientes sobre el uso de Coragyps atratus en el tratamiento del cáncer. Materiales y métodos Diseño cualitativo basado en veinte entrevistas en profundidad de pacientes con cáncer o cuidadores de pacientes con esta enfermedad. Análisis de texto basado en enfoque temático inductivo. Resultados Al Coragyps atratus se le atribuyen propiedades de resistencia y fortalecimiento del sistema inmune de personas enfermas de cáncer. La forma de utilización mas común es la

  5. Revision curricular a partir de un analisis comparativo de las discrepancias en los curriculos de una escuela de optometria en Puerto Rico con las competencias requeridas para las agencias de revalida y acreditacion 2004

    NASA Astrophysics Data System (ADS)

    Rivera Pacheco, Andres

    El proposito de esta investigacion, un estudio cualitativo de caso, fue comparar y contrastar el curriculo vigente de la Escuela de Optometria de la UIAPR con las competencias y estandares requeridos por las agencias de acreditacion y de revalida. Con este proposito, decidimos realizar una revision y un analisis de documentos: el prontuario de cada uno de los cursos de los curriculos implantados en el 1993 y en el 2001; las competencias y estandares establecidos por las agencias de revalida y de acreditacion; y las estadisticas en las que se analiza el porcentaje de estudiantes que aprueban cada una de las partes de los examenes de revalida entre el 1998 al 2003. Se realizaron entrevistas dirigidas para dar apoyo y complementar la revision y el analisis de estos documentos. Los participantes de las entrevistas fueron tres estudiantes de la clase de optometria del 2004 (ultima clase del curriculo del 1993); tres estudiantes de la clase de optometria del 2005 (primera clase graduanda del curriculo vigente) y tres profesores y/o directores de los Departamentos de Ciencias Basicas, Ciencias Clinicas y Cuidado al Paciente. Esta investigacion se enmarco en el modelo de evaluacion curricular de discrepancia de Malcolm Provus y en el modelo de desarrollo basado en competencias. Uno de los hallazgos mas importantes del estudio es que los cambios que se implantaron al curriculo del 2001 no han logrado que los estudiantes mejoren su ejecucion en los examenes de revalida. Por otro lado, se encontro que el curriculo vigente atiende completamente los estandares de la practica de Optometria, pero no las competencias. Esta informacion fue validada mediante el uso de una tabla de cotejo para el analisis de los cursos y de la informacion obtenida de las entrevistas. El estudio determina y concluye que existen discrepancias entre los prontuarios de los cursos del curriculo y las competencias requeridas por la agencia de revalida. Segundo, que el Departamento de Ciencias Basicas es el

  6. [Effectiveness of a program for treatment of overweight and nonmorbid obesity in primary healthcare and its influence lifestyle modification].

    PubMed

    Arrebola Vivas, E; Gómez-Candela, C; Fernández Fernández, C; Bermejo López, L; Loria Kohen, V

    2013-01-01

    Introducción y Objetivos: la modificación de conductas no saludables es fundamental para tratar la obesidad. El objetivo de este estudio fue evaluar los efectos de un programa basado en dieta, ejercicio y apoyo psicológico en la modificación conductual de pacientes con sobrepeso y obesidad tratados en Atención Primaria. Métodos: 60 pacientes con sobrepeso grado II y obesidad grado I-II fueron incluidos en este ensayo piloto. Edad entre 18-50 2013s. Los pacientes recibieron un programa que combinaba educación nutricional, actividad física y apoyo psicológico. Formato grupal, periodicidad quincenal. Los principales resultados medidos al inicio y 6 meses fueron parámetros antropométricos (índice de masa corporal, porcentaje de masa grasa, perímetro cintura) y de estilos de vida usando el Cuestionario para la valoración de hábitos de vida relacionados con el sobrepeso y la obesidad. Consta de 5 dimensiones: contenido calórico de la dieta (CC), alimentación saludable (AS), ejercicio físico (EF), comer por bienestar psicológico (BP) y consumo de alcohol (CA). La mayor puntuación indica mejores hábitos para CC, AS y EF y peores para BP y CA. Resultados: al final de la intervención mejoraron las escalas CC (2,60± 0,5 vs 3,49± 0,7, p<0,001), EF (2,19± 0,9 vs 3,17± 1,0, p<0,001) y AS (3,04± 0,4 vs 3,43± 0,4, p<0,05) del cuestionario; CA (3,98± 0,7 vs. 4,25± 0,7, p<0,05) y BP (2,82± 1,0 vs. 3,34± 0,7, p<0,001) empeoraron. Conclusión: el programa basado en moderada restricción de la dieta, aumento de actividad física y apoyo psicológico puede mejorar parámetros antropométricos y estilos de vida en pacientes obesos tratados en un centro de Atención Primaria.

  7. Evolución de estrellas enanas blancas en el contexto de una constante de gravitación G variable en el tiempo

    NASA Astrophysics Data System (ADS)

    Benvenuto, O. G.; Althaus, L. G.; Torres, D. F.

    En este trabajo se estudia por primera vez de manera autoconsistente la evolución de las estrellas enanas blancas en el caso de una constante de gravitación G variable en el tiempo. Teniendo en cuenta que: 1) las enanas blancas son en general estrellas muy viejas y 2) su fuente de energía es básicamente de origen térmico y gravitacional, estos objetos son en principio muy adecuados para analizar distintas teorías de gravitación. Los cálculos que aquí presentamos fueron realizados utilizando nuestro código de evolución estelar, el cual calcula la evolución de estrellas enanas blancas por medio del esquema iterativo de Henyey. Dicho código, basado en una descripción física muy detallada, ha sido modificado para tener en cuenta la variación del valor de G. Encontramos que un G variable (decreciente en el tiempo) modifica fuertemente la evolución de las enanas blancas, conduciendo a un rápido enfriamiento de la estrella. Nuestros resultados son comparados con recientes datos observacionales sobre la función de luminosidad de las enanas blancas.

  8. [Family intervention for the management of overweight and obesity in schoolchildren].

    PubMed

    González-Heredia, Ricardo; Castañeda-Sánchez, Oscar; López-Morales, Cruz Mónica; Brito-Zurita, Olga Rosa; Sabag-Ruize, Enrique

    2014-01-01

    INTRODUCTIÓN: el manejo de la obesidad es complejo y debe ser multidisciplinario; los tratamientos conductuales basados en la familia para el control de la obesidad infantil tienen un alto grado de eficacia. Se ha argumentado que cuando los niños y los padres son blanco de los cambios de comportamiento en conjunto, los resultados de pérdida de peso generalmente mejoran. El objetivo es determinar el efecto de una intervención basada en la familia para la reducción de peso en escolares con sobrepeso u obesidad. MÉTODOS: estudio cuasi experimental en escolares de 6 a 12 años de la Unidad Médica Familiar 1 en Ciudad Obregón, Sonora. El grupo de intervención correspondió a 30 escolares con sobrepeso u obesidad, además de que uno o ambos padres presentaron sobrepeso u obesidad; en el grupo control se incluyeron 30 escolares con sobrepeso u obesidad, y padres con peso normal. Se midió peso, talla e índice de masa corporal (IMC) basal, final y mensual. Se utilizó t de Student para contrastar las variables cuantitativas, por medio del programa SPSS, versión 15.

  9. The relationship between obesity and forced vital capacity among university students.

    PubMed

    Sun, Xugui; Chen, Xiaohong

    2015-05-01

    Objetivo: Hemos tratado de explorar la relación entre la capacidad vital y la obesidad entre los estudiantes universitarios en China Métodos: Un estudio transversal fue diseñado para recoger los exámenes de salud para estudiantes universitarios en 2013. La altura, el peso y la fuerza así como la capacidad vital de los estudiantes, y el IMC se calcula con la altura y el peso, así como para estimar la relación entre la capacidad de la fuerza vital y la obesidad. Resultados: Basado en el Grupo de trabajo sobre la obesidad de referencia en China, la obesidad tiene una clara prevalencia sobre la capacidad vital en tanto hombres y mujeres estudiantes universitarias. No se encontró ninguna correlación entre la capacidad vital y el IMC. Conclusión: La obesidad puede tener efecto sobre la función pulmonar entre los estudiantes universitarios, lo que supone una referencia para profundizar el estudio de la epidemia.

  10. [RELEVANCE OF A PROGRAM BALANCE IN HEALTH-RELATED QUALITY OF LIFE OF OBESE ELDERLY WOMEN].

    PubMed

    Prieto, Jose Antonio; Del Valle, Miguel; Nistal, Paloma; Méndez, David; Barcala-Furelos, Roberto; Abelairas-Gómez, Cristian

    2015-12-01

    Objetivo: el objetivo de este estudio ha sido analizar los efectos de un programa de intervención específico de fuerza y equilibrio en la calidad de vida en mujeres obesas mayores. Material y método: participaron 56 mujeres obesas mayores (media 67,2 +/- 2,1 años) que se distribuyeron aleatoriamente en grupo control (28) y experimental (28). El grupo experimental llevó a cabo un programa de ejercicio basado en el equilibrio y la fuerza del tren inferior, durante 24 semanas. Se midió la fuerza y el equilibrio antes y después de la intervención. Del mismo modo, se determinó la percepción de la calidad de vida relacionada con la salud (CVRS) a través del cuestionario SF-36. Resultados: el grupo experimental mostró una mejora significativa en todas las pruebas. En el test de la silla se observó un incremento del 28,3 % después del programa (P.

  11. Como Lo Hago Yo: Lipomas Medulares

    PubMed Central

    Portillo, Santiago

    2014-01-01

    Basados en la experiencia de 82 casos; en 5% se observaron anomalías pélvicas asociadas. En los menores de 3 años el motivo de consulta (85%) fue la tumoración. En los mayores de 3 años (42%) tenía problemas neurológicos. Solo el 24% preocupados por la tumoración. El objetivo de la cirugía es desanclar la médula y no remover la totalidad del lipoma. El lipoma de filum es el que es mas simple para operar. Aún cuando la escuela francesa propone operar solamente cuando hay síntomas favorezco cirugía preventiva. Favorezco una segunda cirugía si hay signos de anclaje postoperatorio, aún cuando observamos empeoramiento postoperatorio motor en 2.5% de los operados y urológico a largo plazo en 6% de los operados. PMID:24791218

  12. Elastoplasticidad anisotropa de metales en grandes deformaciones

    NASA Astrophysics Data System (ADS)

    Caminero Torija, Miguel Angel

    El objetivo de este trabajo es el desarrollo de modelos y algoritmos numericos que simulen el comportamiento del material bajo estas condiciones en el contexto de programas de elementos finitos, dando como resultado predicciones mas precisas de los procesos de conformado y deformacion plastica en general. Para lograr este objetivo se han desarrollado diversas tareas destinadas a mejorar las predicciones en tres aspectos fundamentales. El primer aspecto consiste en la mejora de la descripcion del endurecimiento cinematico anisotropo en pequenas deformaciones, lo cual se ha realizado a traves de modelos y algoritmos implicitos de superficies multiples. Ha sido estudiada la consistencia de este tipo de modelos tanto si estan basados en una regla implicita similar a la de Mroz o en la regla de Prager. Ademas se han simulado los ensayos de Lamba y Sidebottom, obteniendo, en contra de la creencia general, muy buenas predicciones con la regla de Prager. Dichos modelos podrian ser extendidos de forma relativamente facil para considerar grandes deformaciones a traves de procedimientos en deformaciones logaritmicas, similares a los desarrollados en esta tesis y detallados a continuacion. El segundo aspecto consiste en la descripcion de la anisotropia elastoplastica inicial. Esto se ha conseguido mediante el desarrollo de modelos y algoritmos para plasticidad anisotropa en grandes deformaciones, bien ignorando la posible anisotropia elastica, bien considerandola simultaneamente con la anisotropia plastica. Para ello ha sido necesario desarrollar primero un nuevo algoritmo de elastoplasticidad anisotropa en pequenas deformaciones consistentemente linealizado y sin despreciar ningun termino, de tal forma que se conserve la convergencia cuadratica de los metodos de Newton. Este algoritmo en pequenas deformaciones ha servido para realizar la correccion plastica de dos algoritmos en grandes deformaciones. El primero de estos algoritmos es una variacion del clasico algoritmo de

  13. Ajuste de parámetros libres en teorías de campos camaleones a partir de espectros de nubes moleculares galácticas y experimentos terrestres

    NASA Astrophysics Data System (ADS)

    Teppa Pannia, F. A.; Landau, S. J.

    Resultados recientes, basados en el análisis de espectros moleculares de nubes galácticas a través del método del amoníaco, han arrojado nuevos límites sobre la variación del parámetro adimensional μ=m_e /m_p. Los resultados indican Δ μ/μ = (μ_{obs}-μ_{lab})/μ_{lab}= (2.2± 0.4_{est} ±0.3_{sist}) times 10 ^{-8}, en acuerdo con una variación no nula de dicha cantidad (Levshakov et al. 2010). En este trabajo, motivado por los datos astronómicos, estudiamos la solución lineal del modelo teórico fenomenológico de campo escalar camaleón, presentado por Mota y Shaw (2007), que predice variaciones en μ. Con el fin de cotejar estas predicciones con los resultados observacionales, utilizamos datos de experimentos terrestres que testean violaciones al Principio de Equivalencia para analizar el valor de los parámetros libres presentes en el modelo. El trabajo realizado muestra que la solución estudiada no se puede ajustar a los datos experimentales, sugiriendo que el modelo lineal debe ser descartado para explicar las observaciones astronómicas. FULL TEXT IN SPANISH

  14. PubMed

    Litewka, Sergio; Goodman, Kenneth; Braunschweiger, Y Paul

    2008-01-01

    El Programa CITI (Collaborative Institutional Training Initiative) es un curso basado en Internet y desarrollado por voluntarios, que brinda material educacional sobre protección de sujetos humanos en investigaciones biomédicas y de conducta, buenas prácticas clínicas, conducta responsable de la investigación y trato humanitario a animales de laboratorio. Es un esfuerzo conjunto del Fred Hutchinson Cancer Research Center y la Universidad de Miami.Con la colaboración de expertos locales, gran parte del contenido se ha adaptado para América Latina, se ha traducido al español y portugués y se han establecido acuerdos de colaboración con instituciones especializadas en bioética en Chile, Brasil, Costa Rica y Perú. Los autores presentan una metodología accesible para la capacitación en ética de la investigación y una justificación de su uso y difusión en América Latina.

  15. Vigilando la Calidad del Agua de los Grandes Rios de la Nacion: El Programa NASQAN del Rio Grande (Rio Bravo del Norte)

    USGS Publications Warehouse

    Lurry, Dee L.; Reutter, David C.; Wells, Frank C.; Rivera, M.C.; Munoz, A.

    1998-01-01

    La Oficina del Estudio Geologico de los Estados Unidos (U.S. Geological Survey, 0 USGS) ha monitoreado la calidad del agua de la cuenca del Rio Grande (Rio Bravo del Norte) desde 1995 como parte de la rediseiiada Red Nacional para Contabilizar la Calidad del Agua de los Rios (National Stream Quality Accounting Network, o NASOAN) (Hooper and others, 1997). EI programa NASOAN fue diseiiado para caracterizar las concentraciones y el transporte de sedimento y constituyentes quimicos seleccionados, encontrados en los grandes rios de los Estados Unidos - incluyendo el Misisipi, el Colorado y el Columbia, ademas del Rio Grande. En estas cuatro cuencas, el USGS opera actualmente (1998) una red de 40 puntos de muestreo pertenecientes a NASOAN, con un enfasis en cuantificar el flujo en masa (la cantidad de material que pasa por la estacion, expresado en toneladas por dial para cada constituyente. Aplicacando un enfoque consistente, basado en la cuantificacion de flujos en la cuenca del Rio Grande, el programa NASOAN esta generando la informacion necesaria para identificar fuentes regionales de diversos contaminantes, incluyendo sustancias qui micas agricolas y trazas elementos en la cuenca. EI efecto de las grandes reservas en el Rio Grande se puede observar segun los flujos de constituyentes discurren a 10 largo del rio. EI analisis de los flujos de constituyentes a escala de la cuenca proveera los medios para evaluar la influencia de la actividad humana sobre las condiciones de calidad del agua del Rio Grande.

  16. [Pathogenesis of spinal cord injuries and mechanisms of repair induced by olfactory ensheathing cells].

    PubMed

    Botero, Lucía; Gomez, Rosa Margarita; Chaparro, Orlando

    2013-05-16

    Introduccion. La lesion medular es un evento catastrofico, cuyas consecuencias persisten durante toda la vida del paciente. La investigacion en tratamiento se ha basado principalmente en el desarrollo de terapias que reduzcan la discapacidad, pero desde los anos noventa hay un avance significativo y se han probado varios trasplantes celulares en modelos animales de lesion medular, celulas de Schwann, astrocitos y celulas de la glia envolvente olfatoria (CGEO). Objetivo. Hacer un recuento detallado de la patogenia de la lesion medular primaria y secundaria y de los mecanismos por los cuales las CGEO inducirian sus posibles efectos regenerativos descritos en la bibliografia. Desarrollo. Despues del traumatismo, la lesion se desarrolla en dos fases, la primaria se caracteriza por las lesiones de compresion y la secundaria se produce por una serie de factores que se dan en paralelo y que incluyen factores vasculares, celulares, moleculares y formacion de cicatriz glial. La mayoria de los modelos de lesion medular y trasplante con CGEO han comunicado recuperacion funcional, remielinizacion y regeneracion axonal. Estas celulas ejercen su accion de manera indirecta a traves de la produccion de factores de crecimiento y de manera directa induciendo regeneracion neuronal, axonal y remielinizacion. Conclusiones. Las CGEO son una opcion terapeutica en pacientes con lesion medular debido a que inducen de modo directo o indirecto regeneracion neuronal, axonal, remielinizacion de axones, disminucion de cicatriz glial y otros efectos que conducen a la recuperacion funcional.

  17. Diseno de una Actividad de Aprendizaje Basada en la Argumentacion Dialogica en un curso Virtual de Biotecnologia y su Incidencia en el Desarrollo de Competencias Cientificas

    NASA Astrophysics Data System (ADS)

    Ortiz Benavides, Fedra Lorena

    El proposito de la investigacion fue evaluar la efectividad de una actividad de aprendizaje basado en la argumentacion dialogica en linea y su incidencia en el desarrollo de competencias cientificas. Se fundamenta en la teoria del aprendizaje socio cultural de Vigotsky (1984), los principios del diseno instruccional de la cognicion situada por Hung y Der-Thang (2001) y como estrategia se aplico la argumentacion dialogica utilizando el Modelo Argumentativo de Toulmin MAT (1984). El diseno experimental comparo dos grupos de estudiantes A y B en el curso virtual de Biotecnologia. El grupo A (experimental) desarrollo la discusion a partir de la estrategia disenada para este estudio y el grupo B (control) realizo la discusion desde las actividades tradicionales. El desarrollo de la competencia argumentativa se valoro con el instrumento de evaluacion para argumentacion dialogica en linea propuesta por Clark y Sampson (2008). La evaluacion de las competencias cientificas se realizo a partir de una postprueba. Los datos fueron analizados con pruebas estadisticas no parametricas. Los resultados de la investigacion, indicaron diferencias significativas en el nivel de la competencia argumental en el grupo experimental en comparacion al grupo control. Igualmente se demostro que existe una relacion positiva entre el nivel de desarrollo de la competencia argumentativa y el nivel de desarrollo de las competencias cientificas.

  18. Modelo semi-empírico de protuberancia solar a partir del diagnóstico de densidades

    NASA Astrophysics Data System (ADS)

    Cirigliano, D.; Vial, J. C.; Rovira, M.

    A partir de la observación del espectro del quintuplete de C III alrededor de 1175 Å, se ha realizado el diagnóstico de la densidad y presión electrónica, basado en el cálculo del cociente de las intensidades observadas. Una vez establecida la densidad electrónica, y con el cálculo de las velocidades Doppler, hemos investigado el flujo de masa en la protuberancia en función de la temperatura. Estableciendo como hipótesis la conservación del número de partículas que ingresan y salen del cuerpo de la protuberancia, se investiga la variación del área de un tubo de flujo semi-empírico en función de la temperatura. A partir de dicho diagnóstico, se examina el comportamiento del radio del tubo magnético en función de la temperatura, los que dan cuenta de la abertura de las líneas de campo magnético que confinan el plasma y de la divergencia del campo magnético en diferentes alturas de la atmósfera solar.

  19. Simulaciones hidrodinámicas de flujos complejos

    NASA Astrophysics Data System (ADS)

    María Ibáñez Cabanell, José

    Son muchos los escenarios astrofísicos en que los procesos hidrodinámicos juegan un papel clave. En la complejidad que encierra la descripción de dichos procesos destaca el de la correcta simulación de flujos complejos donde la presencia de ondas de choque fuertes que, eventualmente, interaccionan entre ellas o también la presencia de inestabilidades (Kelvin-Helmholtz, Rayleigh-Taylor, etc.) suponen un verdadero desafío numérico. Los códigos hidrodinámicos basados en la solución de un problema de valores iniciales discontinuo (problema de Riemann) son, en la actualidad, los más robustos en el campo de la dinámica de fluidos computacional. En esta charla se dará un resumen de los fundamentos de dichas técnicas numéricas (esquemas de alta resolución de captura de choques) y se ilustrará su potencialidad mostrando una amplia gama de resultados en diferentes aplicaciones astrofísicas.

  20. EL PROGRAMA CITI: UNA ALTERNATIVA PARA LA CAPACITACIÓN EN ÉTICA DE LA INVESTIGACIÓN EN AMÉRICA LATINA

    PubMed Central

    Litewka, Sergio; Goodman, Kenneth; Braunschweiger, y Paul

    2011-01-01

    El Programa CITI (Collaborative Institutional Training Initiative) es un curso basado en Internet y desarrollado por voluntarios, que brinda material educacional sobre protección de sujetos humanos en investigaciones biomédicas y de conducta, buenas prácticas clínicas, conducta responsable de la investigación y trato humanitario a animales de laboratorio. Es un esfuerzo conjunto del Fred Hutchinson Cancer Research Center y la Universidad de Miami. Con la colaboración de expertos locales, gran parte del contenido se ha adaptado para América Latina, se ha traducido al español y portugués y se han establecido acuerdos de colaboración con instituciones especializadas en bioética en Chile, Brasil, Costa Rica y Perú. Los autores presentan una metodología accesible para la capacitación en ética de la investigación y una justificación de su uso y difusión en América Latina PMID:21687817

  1. [Early development of language in small children with autism spectrum disorder using alternative systems].

    PubMed

    Fortea-Sevilla, M Sol; Escandell-Bermúdez, M Olga; Castro-Sánchez, José Juan; Martos-Pérez, Juan

    2015-02-25

    Introduccion. Los ultimos hallazgos en investigacion demuestran la importancia de la atencion temprana en niños con trastorno del espectro autista (TEA) en todas las areas del desarrollo y tambien del lenguaje. El uso de sistemas de comunicacion aumentativa y alternativa (SAAC) favorece el desarrollo comunicativo y linguistico. Objetivo. Demostrar la efectividad de los SAAC a la hora de desarrollar el lenguaje oral en niños pequeños no verbales con diagnostico de TEA. Pacientes y metodos. Treinta niños (25 varones y 5 mujeres) a los que se les diagnostico TEA cuando tenian entre 18 meses y 30 meses, mediante los instrumentos ADOS y ADIR. Ninguno de ellos presentaba desarrollo del lenguaje oral en el momento de la evaluacion. Se diseño un programa de intervencion sobre el area del lenguaje basado en el uso de comunicacion total por parte del terapeuta y entrenamiento del niño en el sistema de comunicacion por intercambio de imagenes. Pasado un año se evaluaron los aspectos formales del lenguaje a traves de la prueba de lenguaje oral de Navarra revisada, ya que se habia desarrollado el lenguaje oral. Resultados. Todos ellos han desarrollado el lenguaje oral en alguna medida en un periodo de un año. Conclusiones. La atencion temprana y el uso de SAAC con apoyos visuales favorecen el desarrollo del lenguaje oral en niños con TEA en los primeros años de vida.

  2. Relación masa-radio para estrellas enanas blancas y la interpretación de recientes mediciones hechas por Hipparcos

    NASA Astrophysics Data System (ADS)

    Panei, J. A.; Althaus, L. G.; Benvenuto, O. G.

    Recientes mediciones de la masa y el radio hechas por Hipparcos de las estrellas enanas blancas 40 Eri B y Procyon B (Shipman, H. & Provencal, J. - ApJ. 1998, 494, 759), sugieren un núcleo compuesto de hierro para dichas estrellas, en lugar de carbono y oxígeno como predice la teoría standard de evolución estelar. Para interpretar estas observaciones, presentamos aquí, relaciones masa-radio para configuraciones degeneradas a temperatura finita para distintas composiciones químicas centrales. Para tal fin hemos calculado secuencias evolutivas de enanas blancas utilizando el código de evolución estelar, desarrollado en el Observatorio de La Plata. Dicho código resuelve las ecuaciones de estructura y evolución estelar mediante la técnica de relajación de Henyey, y esta basado en una descripción física muy detallada y actualizada.

  3. [Consensus document on spasticity in patients with multiple sclerosis. Grupo de Enfermedades Desmielinizantes de la Sociedad Española de Neurología].

    PubMed

    Oreja-Guevara, Celia; Montalban, Xavier; de Andrés, Clara; Casanova-Estruch, Bonaventura; Muñoz-García, Delicias; García, Inmaculada; Fernández, Óscar

    2013-10-16

    Introduccion. La esclerosis multiple es una enfermedad neurologica cronica, desmielinizante e inflamatoria. Los neurologos implicados en el tratamiento sintomatico de esta enfermedad tienden a aplicar criterios diagnosticos y de tratamiento heterogeneos. Objetivo. Elaborar un documento de consenso para establecer criterios homogeneos para el tratamiento de la espasticidad, basados en el conocimiento cientifico disponible que faciliten la toma de decisiones en la practica clinica habitual. Desarrollo. Un grupo de expertos españoles en esclerosis multiple del Grupo de Enfermedades Desmielinizantes de la Sociedad Española de Neurologia (SEN) se reunieron para revisar los aspectos relacionados con la espasticidad en esta enfermedad y elaborar el consenso. Tras una busqueda bibliografica exhaustiva y siguiendo la metodologia metaplan se establecieron unas recomendaciones preliminares para incorporar al documento. Finalmente, cada argumento se clasifico segun su grado de recomendacion, atendiendo a las categorias del sistema SIGN (Scottish Intercollegiate Guidelines Network). El texto resultante fue sometido a la revision de los miembros del Grupo de Enfermedades Desmielinizantes de la SEN. Se ha alcanzado un consenso de expertos respecto a los factores desencadenantes de la espasticidad, la sintomatologia relacionada, los criterios diagnosticos, los metodos de valoracion de la espasticidad, la calidad de vida y los criterios en el manejo terapeutico (farmacologicos y no farmacologicos). Conclusion. Las recomendaciones contenidas en este consenso pueden ser una herramienta util para el neurologo para la practica clinica del dia a dia y para mejorar la calidad de vida del paciente, ya que permiten un mejor diagnostico y tratamiento de la espasticidad.

  4. La dinámica demográfica y la desigualdad educativa en Méxicoa

    PubMed Central

    Giorguli Saucedo, Silvia E.; Vargas Valle, Eunice D.; Ulloa, Viviana Salinas; Hubert, Celia; Potter, Joseph E.

    2015-01-01

    En este trabajo se presenta una investigación sobre el vínculo entre los procesos educativos y la dinámica demográfica en México. La tradición del pensamiento sobre población y desarrollo ha partido de la hipótesis de que el ritmo de crecimiento poblacional, el tamaño de las familias y la migración influyen sobre la acumulación de capital humano entre la población en edades escolares. Se explora aquí la relación del desempeño educativo de los jóvenes entre 14 y 23 años y la razón de dependencia juvenil, la fecundidad adolescente y la migración interna e internacional; para ello se utilizan datos agregados a escala municipal del año 2000. El análisis incluye indicadores de la oferta educativa municipal basados en estadísticas administrativas de la SEP. PMID:26146427

  5. [A FOOD FREQUENCY QUESTIONNAIRE TO ASSESS DIET QUALITY IN THE PREVENTION OF IRON DEFICIENCY].

    PubMed

    Toxqui Abascal, Laura; Díaz Álvarez, Alejandra; Vaquero, María Pilar

    2015-09-01

    Introducción: A pesar del amplio conocimiento sobre la biodisponibilidad del hierro, no se ha implementado aún un cuestionario de frecuencia de consumo de alimentos (CFCA) para su aplicación en grupos poblacionales con predisposición a anemia. Objetivos: Diseñar un CFCA basado en los potenciadores e inhibidores de la absorción del hierro y valorar su aplicabilidad en un grupo de mujeres en edad fértil. Métodos: Se elaboró un CFCA específico de 28 preguntas, 10 de ellas con indicación del momento de consumo de alimentos, en el desayuno y en comida/cena (CC). Se seleccionaron 179 mujeres sanas jóvenes que se distribuyeron en 3 grupos en función de su estado del hierro, ferritina sérica 30 ng/mL. Resultados: La reproducibilidad del CFCA fue muy alta (coeficiente de Spearman>0.500, p.

  6. VALIDATION AND COMPARISON OF EQ-5D-3L AND SF-6D INSTRUMENTS IN A SPANISH PARKINSON´S DISEASE POPULATION SAMPLE.

    PubMed

    Garcia-Gordillo, Miguel Ángel; Del Pozo-Cruz, B; Adsuar, J C; Cordero-Ferrera, J M; Abellan-Perpiñan, J M; Sanchez-Martinez, F I

    2015-12-01

    Introducción: el uso de cuestionarios de calidad de vida basados en preferencias poblacionales están recibiendo cada vez más atención en el proceso de toma de decisiones en el ámbito sanitario. Sin embargo, a nuestro entender, EQ-5D y SF-6D nunca han sido comparados en una muestra de población con la enfermedad de Parkinson. Objetivo: el objetivo de este trabajo fue evaluar las propiedades psicométricas de ambos instrumentos en una muestra de población española con enfermos de Parkinson. Métodos: un total de 133 pacientes fueron entrevistados utilizando EQ-5D y SF-6D. La validez, el grado de acuerdo y la sensibilidad de ambos instrumentos fueron calculados para su posterior comparación. Las preferencias de la población española fueron utilizadas en ambos instrumentos. Resultados: las utilidades de EQ-5D y SF-6D han mostrado una fuerte correlación (r> 0,50 y p.

  7. [Implementation of the food choice questionnaire in young adolescents and their relationship to overweight and other socio-demographic variables].

    PubMed

    Canales Ronda, Pedro; Hernández Fernández, Asunción

    2015-05-01

    Objetivo: El objetivo del presente trabajo se centra en analizar el comportamiento en la elección de los alimentos entre los jóvenes adolescentes españoles, así como su efecto sobre los posibles problemas relacionados con su peso (sobrepeso y obesidad) y otras variables socio-demográficas. Método: En el estudio participaron 590 alumnos de colegios públicos y privados de la ciudad de Valencia, con edades entre los 14 y 17 años, elegidos aleatoriamente. Se realizó un cuestionario personal basado en el Food Choice Questionaire. Resultados: En general, los jóvenes eligen sus alimentos en función de los aspectos sensoriales y el precio de los mismos, y no les preocupan los efectos que sobre su peso tienen sus hábitos alimentarios. No se detectan diferencias entre los alumnos de centros públicos o privados, ni tampoco entre aquellos con normopeso o sobrepeso. Si que existe alguna diferencia en cuanto al género del encuestado. Conclusiones: Los adolescentes, a la hora de elegir su alimentación, no son muy conscientes de los posibles efectos de los mismos sobre su salud actual y futura.

  8. Implications of the 26 December 2004 Sumatra-Andaman earthquake on tsunami forecast and assessment models for great subduction-zone earthquakes

    USGS Publications Warehouse

    Geist, Eric L.; Titov, Vasily V.; Arcas, Diego; Pollitz, Fred F.; Bilek, Susan L.

    2007-01-01

    Results from different tsunami forecasting and hazard assessment models are compared with observed tsunami wave heights from the 26 December 2004 Indian Ocean tsunami. Forecast models are based on initial earthquake information and are used to estimate tsunami wave heights during propagation. An empirical forecast relationship based only on seismic moment provides a close estimate to the observed mean regional and maximum local tsunami runup heights for the 2004 Indian Ocean tsunami but underestimates mean regional tsunami heights at azimuths in line with the tsunami beaming pattern (e.g., Sri Lanka, Thailand). Standard forecast models developed from subfault discretization of earthquake rupture, in which deep- ocean sea level observations are used to constrain slip, are also tested. Forecast models of this type use tsunami time-series measurements at points in the deep ocean. As a proxy for the 2004 Indian Ocean tsunami, a transect of deep-ocean tsunami amplitudes recorded by satellite altimetry is used to constrain slip along four subfaults of the M >9 Sumatra–Andaman earthquake. This proxy model performs well in comparison to observed tsunami wave heights, travel times, and inundation patterns at Banda Aceh. Hypothetical tsunami hazard assessments models based on end- member estimates for average slip and rupture length (Mw 9.0–9.3) are compared with tsunami observations. Using average slip (low end member) and rupture length (high end member) (Mw 9.14) consistent with many seismic, geodetic, and tsunami inversions adequately estimates tsunami runup in most regions, except the extreme runup in the western Aceh province. The high slip that occurred in the southern part of the rupture zone linked to runup in this location is a larger fluctuation than expected from standard stochastic slip models. In addition, excess moment release (∼9%) deduced from geodetic studies in comparison to seismic moment estimates may generate additional tsunami energy, if the

  9. Validation of stratospheric and mesospheric ozone observed by SMILES from International Space Station

    NASA Astrophysics Data System (ADS)

    Kasai, Y.; Sagawa, H.; Kreyling, D.; Dupuy, E.; Baron, P.; Mendrok, J.; Suzuki, K.; Sato, T. O.; Nishibori, T.; Mizobuchi, S.; Kikuchi, K.; Manabe, T.; Ozeki, H.; Sugita, T.; Fujiwara, M.; Irimajiri, Y.; Walker, K. A.; Bernath, P. F.; Boone, C.; Stiller, G.; von Clarmann, T.; Orphal, J.; Urban, J.; Murtagh, D.; Llewellyn, E. J.; Degenstein, D.; Bourassa, A. E.; Lloyd, N. D.; Froidevaux, L.; Birk, M.; Wagner, G.; Schreier, F.; Xu, J.; Vogt, P.; Trautmann, T.; Yasui, M.

    2013-09-01

    We observed ozone (O3) in the vertical region between 250 and 0.0005 hPa (~ 12-96 km) using the Superconducting Submillimeter-Wave Limb-Emission Sounder (SMILES) on the Japanese Experiment Module (JEM) of the International Space Station (ISS) between 12 October 2009 and 21 April 2010. The new 4 K superconducting heterodyne receiver technology of SMILES allowed us to obtain a one order of magnitude better signal-to-noise ratio for the O3 line observation compared to past spaceborne microwave instruments. The non-sun-synchronous orbit of the ISS allowed us to observe O3 at various local times. We assessed the quality of the vertical profiles of O3 in the 100-0.001 hPa (~ 16-90 km) region for the SMILES NICT Level 2 product version 2.1.5. The evaluation is based on four components: error analysis; internal comparisons of observations targeting three different instrumental setups for the same O3 625.371 GHz transition; internal comparisons of two different retrieval algorithms; and external comparisons for various local times with ozonesonde, satellite and balloon observations (ENVISAT/MIPAS, SCISAT/ACE-FTS, Odin/OSIRIS, Odin/SMR, Aura/MLS, TELIS). SMILES O3 data have an estimated absolute accuracy of better than 0.3 ppmv (3%) with a vertical resolution of 3-4 km over the 60 to 8 hPa range. The random error for a single measurement is better than the estimated systematic error, being less than 1, 2, and 7%, in the 40-1, 80-0.1, and 100-0.004 hPa pressure regions, respectively. SMILES O3 abundance was 10-20% lower than all other satellite measurements at 8-0.1 hPa due to an error arising from uncertainties of the tangent point information and the gain calibration for the intensity of the spectrum. SMILES O3 from observation frequency Band-B had better accuracy than that from Band-A. A two month period is required to accumulate measurements covering 24 h in local time of O3 profile. However such a dataset can also contain variation due to dynamical, seasonal, and

  10. PROKARYOTIC EXPRESSION AND BIOACTIVITY EVALUATION OF THE CHIMERIC GENE DERIVED FROM THE GROUP 1 ALLERGENS OF DUST MITES.

    PubMed

    Zhan, Xiaodong; Li, Chaopin; Guo, Wei; Jiang, Yuxin

    2015-12-01

    Antecedentes: se reconstituyó con éxito el gen del grupo 1 alérgenos de los ácaros del polvo, y obtuvo un conjunto de genes barajadas. Con el fin de verificar la predicción en el gen quimérico, hemos clonado tentativamente R8 en el vector que se expresó prokaryoticly, purificó y se evaluó por sus actividades-bio. Métodos: el producto expresado se detectó por SDS-PAGE y la proteína diana se purificó. La proteína purificada R8 se detectó por ELISA. Setenta y cinco ratones BALB/ c se dividieron en 5 grupos, a saber: PBS, rDer f1, rDer p1, R8 y el grupo de asma. Los ratones fueron tratados con alérgenos de ácaros del polvo a los 0, 7, 14 días mediante inyección intraperitoneal y inhaladas desafío como aerosol en día 21 durante 7 días. La inmunoterapia específica para el alérgeno se realizó utilizando rDer f1, rDer p1 y alérgenos R8, respectivamente. El nivel de IFN e IL-4 en BALF se detectó por ELISA. Resultados: el gen quimérico R8 se expresó con una banda de aproximadamente Mr 35000. En comparación con los grupos de rDer f 1 y rDer p 1 [(80,44 ± 15,50) y (90,79 ± 10,38) μg/ml, respectivamente], la capacidad de unión a IgE de la proteína R8 (37,03 ± 12,46) μg/ml fue estadísticamente inferior (P.

  11. Modelagem do vento e da fotosfera de AG Carinae

    NASA Astrophysics Data System (ADS)

    Groh, J. H.; Damineli, A.

    2003-08-01

    A trajetória evolutiva das estrelas de alta massa depende fortemente de suas taxas de perda de massa. Apesar do rápido progresso no estudo destas estrelas, a taxa de perda de massa e outros parâmetros físicos básicos, como a temperatura superficial e a velocidade terminal do vento ainda não estão bem determinados. Isto ocorre devido à presença de ventos irregulares, rápidos e fortes ao redor destas estrelas, tornando a interpretação dos seus espectros uma tarefa difícil. Assim, a modelagem do vento e da fotosfera dessas estrelas está sendo cada vez mais usada para obter tais parâmetros a partir dos espectros. O aumento da taxa de perda de massa durante a fase LBV (Variáveis Luminosas Azuis), comparado com outros tipos de estrelas, tem sido atribuído a instabilidades do tipo S Doradus. Dispomos de uma base de dados espectroscópicos cobrindo 22 anos de observações de AG Carinae, incluindo um ciclo S Doradus completo, com espectros CCD em alta resolução na faixa óptica e infravermelha. Utilizamos o programa desenvolvido por Schmutz (1997) para uma análise preliminar desse ciclo, obtendo a taxa de perda de massa a partir da linha do Ha. Não existe uma correlação clara da taxa de perda de massa com mudanças da temperatura efetiva, do raio da estrela e do fluxo na banda V. A estrela atingiu seu mínimo fotométrico (raio mínimo) em 1990 e o máximo fotométrico (raio máximo) em 1995, enquanto que o fluxo máximo da linha do Ha ocorreu em 1996. Além disso a taxa de perda de massa não segue esse ciclo, contrariamente às idéias correntes. Para fazer um modelo mais realista estamos usando o programa CMFGEN (Hillier & Miller), que trata a fotosfera e o vento estelar de forma consistente, considerando a radiação fora do equilíbrio termodinâmico (NLTE) e com blanketting total de linhas. Simulamos o espectro de AG Carinae em duas épocas extremas do ciclo S Dor para testar os resultados obtidos com o modelo mais simplificado.

  12. Desenvolvimento das câmeras de raios-X duros do satélite MIRAX

    NASA Astrophysics Data System (ADS)

    Braga, J.; Rothschild, R.; Staubert, R.; Heise, J.; Remillard, R.; D'Amico, F.; Jablonski, F.; Mejía, J.; Carvalho, H.; Heindl, B.; Matteson, J.; Kendziorra, E.; Wilms, J.; in't Zand, J.; Kuulkers, E.

    2003-08-01

    O MIRAX (Monitor e Imageador de RAios-X) é um projeto de desenvolvimento de um pequeno satélite astronômico de raios-X (~200 kg, ~240 W). A estratégia básica da missão será observar continuamente (~9 meses por ano) a região central (~1000 graus2) do plano Galáctico e realizar estudos espectroscópicos de banda larga (2-200 keV) e alta sensibilidade de um grande conjunto de fontes através de imagens com resolução de ~6'. Isso proporcionará uma cobertura inédita do "espaço de descobertas" através da detecção, localização, identificação e estudo detalhado de fenômenos imprevisíveis, tais como transientes fracos de raios-X, novas rápidas de raios-X e bursts de raios gama, assim como o estudo de fontes com emissão persistente. Neste trabalho apresentamos o projeto das duas câmeras de raios-X duros (CXDs) do MIRAX, que irão operar na faixa de 10 a 200 keV. Cada CXD consistirá de um plano de detectores CZT (Cd0,9Zn0,1Te) de 0,5 mm de resolução espacial e 370 cm2 de área total, e de uma máscara codificada com elementos quadrados de 1,3 mm de lado e 0,5 cm de espessura. A máscara terá dimensões de 315 cm ´ 275 cm e será montada a 700 cm de distância dos detectores. Com essa configuração as CXDs terão 6' de resolução angular e, quando colocadas a um ângulo de 29° entre si, as duas câmeras propiciam um campo totalmente codificado de 39° ´ 6°12' e um campo total de 76° ´ 44°. Serão apresentadas simulações de observações da região do plano Galáctico com o conjunto formado pelas duas CXDs.

  13. Preliminary results of teleseismic double-difference relocation of earthquakes around Indonesian archipelago region

    SciTech Connect

    Nugraha, Andri Dian Widiyantoro, Sri; Shiddiqi, Hasbi Ash; Ramdhan, Mohamad; Wandono,; Sutiyono,; Handayani, Titi; Nugroho, Hendro

    2015-04-24

    Indonesian archipelago region is located in active tectonic setting and high seismicity zone. During the last decade, Indonesian was experienced with destructive major earthquakes causing damage and victims. The information of precise earthquake location parameters are very important in partular for earthquake early warning to the society and for advance seismic studies. In this study, we attempted to improve hypocenter location compiled by BMKG for time periods of April, 2009 up to June, 2014 for about 22,000 earthquake events around Indonesian region. For the firts time, we applied teleseismic double-difference relocation algorithm (teletomoDD) to improve hypocenter region in Indonesia region combining regional and teleseismic stations. Hypocenter relocation was performed utilizing local, regional, and teleseismic P-wave arrival time data. Our relocation result show that travel-time RMS errors were greatly reduced compared to the BMKG catalog. Seismicity at shallower depth (less than 50 km) shows significantly improvement especially in depth, and refined shallow geological structures, e.g. trench and major strike slip faults. Clustered seismicity is also detected beneath volcanic region, and probably related volcano activities and also major faults nearby. In the Sunda arc region, seismicity at shallower depth centered at two major distributions parallel to the trench strike direction, i.e. around fore-arc and in mainland that related to major fault, e.g. the Sumatran fault, and volcanic fronts. Below Central Java region, relocated hypocenter result showed double seismic zone pattern. A seismic gap is detected around the Sunda-Banda transition zone where transition between oceanic subduction to continental crust collision of Australian plate occurs. In Eastern Indonesia region, shallow earthquakes are observed related to major strike slip faults, e.g. Sorong and Palu-Koro fault, volcanism, and shallow part of subduction and collision zones. We also compare our

  14. Why did we lose the 59 climbers in 2014 Ontake Volcano Eruption?

    NASA Astrophysics Data System (ADS)

    Kimata, F.

    2015-12-01

    The first historical eruption at Ontake volcano, central Japan was in 1979, and it was a phreatic eruption. Until then, most Japanese volcanologists understood that Ontake is a dormant or an extinct volcano. Re-examination of active volcanoes was done after the eruption.After the first historical eruption in 1979, two small eruptions are repeated in 1991 and 2007. Through the three eruptions, nobody has got injured. The last eruption on September 27, 2014, we lost 65 people included missing. Because it was fine weekend and there were many climbers on the summit. The eruption was almost at lunchtime. Clearly, casualties by tsunamis are inhabitants along the coastlines, and casualties by eruption are visitors not inhabitants around the volcano. Basically, visitors have small information of Ontake volcano. After the accident, one mountain guide tells us that we never have long broken such as lunch around the summit, because an active creator is close, and they are afraid of the volcano gas accidents. All casualties by eruption were lost their lives in the area of 1.0 km distance from the 2014 creators. In 2004 Sumatra Earthquake Tsunami, we could not recognize the tsunami inspiration between the habitants in Banda Aceh, Sumatra. They have no idea of tsunami, and they called "Rising Sea" never"Tsunami". As the result, they lost many habitants close to the coast. In 2011 Tohoku Earthquake Tsunami, when habitants felt strong shaking close to coast, they understood the tsunami coming. 0ver 50 % habitants decide to evacuate from the coast. However, 20-30 % habitants believe in themselves no tsunami attacking for them. As a result we lost many habitants. Additionally, the tsunami height was higher than broadcasting one by JMA. According to the results of the questionnaire survey in climbers or bereaved families of the eruption day on Ontake volcano (Shinano Mainich Newspaper, 2015), 39 % of them were climbing no understand of "Ontake active volcano". Moreover, only 10

  15. [Acute gastric volvulus: late complication of Nissen fundoplication. Report of two cases and review of the literature].

    PubMed

    Reyes-Zamorano, Jesús

    2014-01-01

    Antecedentes: el vólvulo gástrico puede clasificarse por su etiología en primario o secundario, por su anatomía en órgano axial o mesentérico axial y por su presentación en crónico o agudo. El tratamiento del vólvulo gástrico secundario agudo siempre debe ser quirúrgico y la elección del procedimiento basarse en la etiología y en los casos asociados con cirugía previa será importante la lisis de adherencias y el retiro de cuerpos extraños (material de sutura, mallas, banda gástrica). La funduplicatura Nissen es un procedimiento seguro y efectivo que rara vez puede tener complicaciones tardías severas entre las que se encuentran el vólvulo gástrico. Objetivo: comunicar 2 casos y revisar la bibliografía médica. Casos clínicos: se describen 2 casos de vólvulo gástrico agudo secundarios a funduplicatura tipo Nissen laparoscópica, con síntomas de dolor epigástrico y vómito no productivo, ambos tratados por laparoscopia. Se revisan los síntomas de presentación, incidencia, diagnóstico, tratamiento y los factores predisponentes de vólvulo gástrico postfunduplicatura. Conclusión: el vólvulo gástrico rara vez puede ser una complicación de una funduplicatura Nissen con incidencia similar a la de otras de sus complicaciones tardías. Los mecanismos descritos que lo originan se relacionan con adherencias postquirúrgicas, material de sutura (poliéster), mallas, tubos de gastrostomía, gastropexia y por herniación gástrica interna a través del túnel "transfunduplicatura." En pacientes con síntomas de obstrucción gástrica dentro del primer año posterior a una funduplicatura Nissen laparoscópica se requiere un alto índice de sospecha. El tratamiento quirúrgico laparoscópico es seguro con o sin gastropexia para corregir los mecanismos que lo originan.

  16. Detrital Zircon Geochronology of Cambro-Ordovician Siliciclastic Units of the Humber Arm Allochthon, Newfoundland, Canada

    NASA Astrophysics Data System (ADS)

    Gittens, A.; Casey, J. F.; Lapen, T. J.; Dewey, J. F.; Reid, D.

    2012-12-01

    (Makkovik Province, Torngat Arc Province, and New Quebec Province) may possibly provide a more local source for sediments derivation for the Irishtown, Lower Head, and Goose Tickle Formations; and (5) development of an accretionary wedge in front of the advancing arc may have acted as a sediment barrier to significant arc-derived sediment, explaining low young zircon yields from flysch (e.g. the modern-day Sunda-Banda and Barbados Arcs).

  17. Hf sbnd Nd sbnd Sr isotopes and incompatible element abundances in island arcs: implications for magma origins and crust-mantle evolution

    NASA Astrophysics Data System (ADS)

    White, William M.; Patchett, Jonathan

    1984-02-01

    We present Hf, Nd and Sr isotopic data and abundances of K, Rb, Cs, Ba, Sr, Hf and REE for 32 samples from seven intra-oceanic island arcs. Samples from the Marianas, Izu, Aleutian and New Britain arcs have tightly grouped 176Hf/ 177Hf˜ 0.28320, 143Nd/ 144Nd˜ 0.51303 and 87Sr/ 86Sr˜ 0.7035 close to, but distinct from, mid-ocean ridge basalts (MORB) for 143Nd/ 144Nd and 87Sr/ 86Sr . In contrast, samples from the Sunda, Banda and Lesser Antilles arcs are much more variable towards lower 176Hf/ 177Hf and 143Nd/ 144Nd , and higher 87Sr/ 86Sr . Isotopically, island arcs on the whole are closely similar to ocean islands. Some commonly-occurring features of the trace element geochemistry of island arcs are apparent in our data: alkali and alkaline-earth elements, particularly Cs, have high abundance relative to LREE compared to oceanic basalts; negative Ce anomalies occur in six out of seven arcs. However, Hf does not appear underabundant relative to REE. The isotopic data require a continental component in all island arcs, in addition to probable mantle and oceanic crust contributions, even for the arcs with isotope ratios close to MORB. In the absence of continental crust, we can best explain this component by subducted pelagic sediment in the arc magma source region. The involvement of sediments in all arcs implies that there is an inherent recycling of older continent to island arcs, and potentially to new continent, of at least 1%. Conservative calculations show that the upper subducted slab (basalt + sediment) passes beyond the arc magma genesis zone and enters the deep mantle with a minimum of 500-1000 ppm K, and corresponding amounts of other incompatible elements. If this material is not completely homogenized with the mantle and later becomes part of the source of ocean island magmas, then the ocean island—island arc isotopic similarity is a result of their similar mix of source materials—mantle peridotite with trace element signatures from oceanic crust

  18. Stress in the Indo-Australian plate

    NASA Astrophysics Data System (ADS)

    Cloetingh, Sierd; Wortel, Rinus

    1986-12-01

    on the down-going slab in each of these. The state of compression in west and central Australia is induced by the action of resistive forces at the Himalayan and Banda arc collision zones. The joint occurrence of high levels of compression in the plate's interior and normal faulting seismicity in the near-ridge areas, is a transient feature unique to the present dynamic situation of the Indo-Australian plate.

  19. Global tectonics since the breakup of Pangea 180 million years ago: evolution maps and lithospheric budget

    NASA Astrophysics Data System (ADS)

    Weijermars, Ruud

    Pangea, the Earth's youngest single supercontinent, broke up 180 million years ago. Tectonic plates were subsequently formed by dispersal of the continental fragments and accretion of new oceanic lithosphere. The configurations of all the major lithospheric plates at 0, 20, 65, 95, 140, 180 Ma BP are reconstructed on six globes of the Earth, each with a radius of 10 cm. It appears that plate boundaries maintain a remarkably close fit on model globes of constant radii if the reconstructions include the recovery of subducted spreading patterns. This is illustrated with maps in equatorial orthographic, oblique orthographic and transverse Hammer-Aitoff projections. The snug fit of the tectonic plates at every tested time since the breakup of Pangea 180 Ma BP is consistent with the theory of plate tectonics on a non-expanding Earth and contradicts rapidly expanding Earth models. The areas of oceanic lithosphere produced and consumed during the past 180 Ma BP are estimated from surface measurements of the globes reconstructed on the basis of particular assumptions. These measurements suggest a consistent increase in the production rate of oceanic lithosphere during the past 140 Ma. It was decided to revise the assumptions and see if alternative reconstructions of the ancient spreading patterns on the floors of the Tethys and Eo-Pacific oceans could avoid implying an increase of lithospheric production rates with time. This appeared to be possible. The revised maps suggest that ophiolites older than 180 Ma BP may have been obducted in Cenozoic collision zones of the Himalayas, Andes, Rockies, and the western part of the Banda Arc (Timor, New Guinea). Estimates of the ocean floor production and consumption budget appear to be quite similar for both map series, and only the possible ranges are summarized here, time averaged for the past 180 Ma. World-wide production and consumption of oceanic lithosphere appears to have varied between 2.6 and 3.5 km 2 a -1 at most. The mean

  20. Microearthquake seismicity and fault plane solutions related to arc-continent collision in the Eastern Sunda Arc, Indonesia

    NASA Astrophysics Data System (ADS)

    McCaffrey, Robert; Molnar, Peter; Roecker, Steven W.; Joyodiwiryo, Yoko S.

    1985-05-01

    The collision of Australia with the eastern Sunda and Banda arcs of Indonesia represents a modern example of the early stages of arc-continent collision. In order to obtain a more detailed view of the tectonics of the collision zone, a microearthquake survey was conducted around the Savu Sea, the region that encompasses the transition from subduction of Indian Ocean lithosphere on the west to collision or subduction of Australian continental lithosphere on the east. Intermediate depth earthquakes were concentrated near Pantar Island, the easternmost active volcano of the Sunda arc, and outline a northwest dipping zone that strikes N65°E from 70 to 150 km depth. The seismic zone probably marks the western edge of the collision zone and its more northerly strike, and the orientations of nodal planes from fault plane solutions indicate a 25° bend in the subducted slab to a depth of at least 150 km. Because the convergence rate and the timing of collision from geologic observations on Timor suggest that the part of the slab now at 150 km depth was at the trench when Australia first collided with Timor, we infer that continental crust (or at least rifted continental margin crust) caused the bend in the convergent margin and has been subducted to 150 km depth. Fault plane solutions of several events show nearly vertical nodal planes that trend parallel to the strike of the seismic zone, along which a northwest-side-down sense of displacement is indicated: these events are concentrated at the southern (top) side of the seismic zone and suggest that the subducted lithosphere is presently detaching in the 50-100 km depth range beneath the eastern Savu Sea. Fault plane solutions for earthquakes within the upper part of the detaching slab (70-100 km depth) have P and T axes whose trends lie parallel to the strike of the seismic zone and horizontal, southeast trending B axes. These earthquakes are interpreted as due to stresses caused by the bend in the subducting plate.

  1. Late Jurassic-Cenozoic reconstructions of the Indonesian region and the Indian Ocean

    NASA Astrophysics Data System (ADS)

    Hall, Robert

    2012-10-01

    The heterogeneous Sundaland region was assembled by closure of Tethyan oceans and addition of continental fragments. Its Mesozoic and Cenozoic history is illustrated by a new plate tectonic reconstruction. A continental block (Luconia-Dangerous Grounds) rifted from east Asia was added to eastern Sundaland north of Borneo in the Cretaceous. Continental blocks that originated in western Australia from the Late Jurassic are now in Borneo, Java and Sulawesi. West Burma was not rifted from western Australia in the Jurassic. The Banda (SW Borneo) and Argo (East Java-West Sulawesi) blocks separated from western Australia and collided with the SE Asian margin between 110 and 90 Ma, and at 90 Ma the Woyla intra-oceanic arc collided with the Sumatra margin. Subduction beneath Sundaland terminated at this time. A marked change in deep mantle structure at about 110°E reflects different subduction histories north of India and Australia since 90 Ma. India and Australia were separated by a transform boundary that was leaky from 90 to 75 Ma and slightly convergent from 75 to 55 Ma. From 80 Ma, India moved rapidly north with north-directed subduction within Tethys and at the Asian margin. It collided with an intra-oceanic arc at about 55 Ma, west of Sumatra, and continued north to collide with Asia in the Eocene. Between 90 and 45 Ma Australia remained close to Antarctica and there was no significant subduction beneath Sumatra and Java. During this interval Sundaland was largely surrounded by inactive margins with some strike-slip deformation and extension, except for subduction beneath Sumba-West Sulawesi between 63 and 50 Ma. At 45 Ma Australia began to move north; subduction resumed beneath Indonesia and has continued to the present. There was never an active or recently active ridge subducted in the Late Cretaceous or Cenozoic beneath Sumatra and Java. The slab subducted between Sumatra and east Indonesia in the Cenozoic was Cretaceous or older, except at the very western end

  2. Seismotectonics of the central segment of the Indonesian Arc

    NASA Astrophysics Data System (ADS)

    Eva, C.; Cattaneo, M.; Merlanti, F.

    1988-01-01

    In this paper, a revision of seismicity affecting the central segment of the Indonesian island arc ranging between 110° and 126° E is presented. Using the areal and in-depth distribution of seismic activity, strain release maps and focal mechanisms, lateral changes in the Wadati-Benioff zone have been analyzed to determine possible boundaries between portions of lithosphere with different subduction geometries. The seismicity pattern indicates that the Sumbawa-Flores-Wetar sector shows different forms of behaviour with respect to the adjacent sectors. These include driving mechanism, inclination and continuity of the subducting slab and subduction features. This area therefore seems to be isolated from the Sunda and Banda arcs by two principal boundaries, these having a nearly N-S trend in the Bali region and with a nearly E-W trend in the region ranging between Wetar-Northern Timor and Tanibar. The first boundary, characterized by an absolute minimum of seismic activity at all ranges of depth, has been interpreted in terms of subduction of the Roo Rise aseismic bathymetric ridge. For the second boundary, dividing a northwardly steeply-dipping slab from an E-W subducting slab dipping with an angle of 30 ° -40 °, a tear in the upper part (depth less than 300 km) and a hinge fault system in the deepest part of the lithosphere, have been proposed. From the analysis of focal mechanisms of shallow earthquakes, it was inferred that the central part of the Indonesian Arc is subject to a vortex-shaped stress field centred on the Savu Basin. In this model, the compressive axes appear to rotate counterclockwise (from SW to NNE) in the Sumba-Sumbawa-Western Flores region and clockwise (from W to NNW) in the Timor-Eastern Flores zone. To interpret these features, on the basis of seismological evidence, a lateral discontinuity in the arc-trench system close to Sumba, a collision between Sumba and Sumbawa and a rotation towards the north-northeast of Sumba have been

  3. The 1977 Sumba earthquake series: Evidence for Slab pull force acting at a subduction zone

    NASA Astrophysics Data System (ADS)

    Spence, William

    1986-06-01

    The great 1977 Sumba earthquake occurred at the eastern Sunda trench, just west of the collision of Australian continental lithosphere with the island arc. The length of the aftershock zone of this normal-faulting earthquake is about 200 km. Aftershocks are concentrated 65-115 km east of the main shock epicenter, with very few aftershocks in a 50-km-long segment that spans the main shock epicenter. Relocated hypocenters and focal mechanism data are consistent with normal faulting throughout the upper 28 km of the oceanic lithosphere. There is no evidence for thrust faulting of the deeper aftershocks. These data imply that the neutral bending surface must be at least 35-40 km deep. A second aftershock zone, about 180 km northwest of the main shock, became active immediately following the main shock, but events were concentrated during days 50-52. This zone is a 70-km-long lineation that trends toward the main shock epicenter and reflects right-lateral, strike-slip faulting within the subducted oceanic plate. Seismicity exists to a depth of about 650 km in the very old plate beneath the Sunda-Banda arc, and that plate's negative buoyancy causes very large slab pull forces. Great interface thrust earthquakes are absent at the Sumba region, and slab pull forces are inferred to have partially decoupled the subducted plate from the overriding plate. This decoupling permits slab pull stresses to be guided updip to the region of the Sumba main shock. Such shallow-acting slab pull provides a bending moment at the trench and explains the deformation and timing observed for the entire Sumba earthquake series. In this model, slab pull forces stretch the subducted plate until the increasing stresses at the shallow subduction zone lead to a subduction zone earthquake. Postseismically, the released oceanic plate undergoes a pulse of downdip strain, returning the plate to a less extended state. The moment of this downdip plate motion could exceed the seismic moment of the main

  4. [Pseudomyxoma peritonei. Two-case-report].

    PubMed

    Carranza-Martínez, Ixchel; Cornejo-López, Gilberto; Monroy-Argumedo, Montserrat; Villanueva-Sáenz, Eduardo

    2014-01-01

    Antecedentes: el pseudomixoma peritoneal se caracteriza por la diseminación celular intraperitoneal de un tumor adenomucinoso; el apéndice cecal es la etiología más frecuente. Objetivo: reportar la experiencia de un grupo de Cirugía General y revisar la bibliografía. Casos clínicos: 1: paciente femenina de 74 años de edad, que cuatro días previos inició con dolor abdominal tipo cólico en el mesogastrio y fosa iliaca derecha, evacuaciones diarreicas y fiebre. A su ingreso al hospital se la encontró con datos de irritacion peritoneal y resistencia muscular, leucocitosis de 14,500 células por mm3, neutrófilos 89%, bandas 1%. Se diagnosticó: apendicitis aguda y se programó para laparoscopia diagnóstica, con distensión importante de asas, por lo que se decidió convertir a laparotomía. Caso 2: paciente masculino de 73 años de edad; el padecimiento actual se inició con dolor intermitente en la fosa iliaca derecha e hipogastrio, de un año de evolución. Al cuadro se agregaron: disnea, estreñimiento alternado con periodos de diarrea, plenitud gástrica, y pirosis. A la exploración física se encontró un tumor palpable en el mesogastrio y ambas fosas iliacas. Por eso se le realizó la laparotomía exploradora. En ambos casos el diagnóstico se estableció en el transoperatorio con el hallazgo de múltiples implantes tumorales mucinosos multilobulados diseminados en la cavidad peritoneal, el diagnóstico se confirmó con el reporte histopatológico de pseudomixoma peritoneal. Conclusiones: el pseudomixoma peritoneal es una neoplasia poco frecuente y de difícil diagnóstico, caracterizada por producción copiosa de ascitis mucinosa y de múltiples implantes tumorales en la serosa de las vísceras intracavitarias. El tratamiento ideal es la cirugía citorreductiva y la quimioterapia intraperitoneal perioperatoria o la quimioterapia postoperatoria, o ambas.

  5. Abundâncias em estrelas de Bário

    NASA Astrophysics Data System (ADS)

    Allen, D. M.

    2003-08-01

    Estrelas de Bário apresentam linhas intensas de elementos produzidos pelo processos (ex: Ba, Y, Sr, Zr) e bandas intensas de CN, C2 e CH. A hipótese mais aceita sobre a origem deste grupo peculiar é a de que essas estrelas façam parte de sistemas binários, tendo recebido material enriquecido em elementos pesados da companheira mais evoluída. Apresentamos neste trabalho uma análise detalhada de uma amostra de estrelas desta classe, incluindo determinação de parâmetros atmosféricos e cálculo de abundâncias. As temperaturas efetivas foram determinadas a partir de dados fotométricos obtidos com o Fotrap instalado no telescópio Zeiss do LNA (Laboratório Nacional de Astrofísica) (B-V, V-I, R-I, V-R), e coletados na literatura nos catálogos Hipparcos (B-V), 2MASS (Two Micron All Sky Survey) (V-K) e The General Catalogue Photometric Data (sistema Geneva). Obtivemos uma faixa de temperaturas de 4400 £ Tef £ 6500. As metalicidades foram determinadas a partir de linhas de Fe I e Fe II, estando os resultados no intervalo -1 £ [Fe/H] £ +0.1. O log g foi determinado pelo equilíbrio de ionização e pela relação com a magnitude bolométrica, a temperatura e a massa, sendo os resultados na faixa 1.5 £ log g £ 4.5. As distâncias utilizadas foram determinadas com o auxílio das paralaxes Hipparcos, e as massas determinadas por modelos de isócronas. Os espectros utilizados foram obtidos com o espectrógrafo FEROS no Telescópio de 1,5m do ESO (European Southern Observatory). As abundâncias foram calculadas por meio de síntese espectral de linhas individuais incluindo elementos alfa, pico do Fe, s e r. Encontramos um excesso de elementos pesados em relação ao Fe, como esperado para estrelas de Bário.

  6. A global outer-rise/outer-trench-slope (OR/OTS) earthquake study

    NASA Astrophysics Data System (ADS)

    Wartman, J. M.; Kita, S.; Kirby, S. H.; Choy, G. L.

    2009-12-01

    Using improved seismic, bathymetric, satellite gravity and other geophysical data, we investigated the seismicity patterns and focal mechanisms of earthquakes in oceanic lithosphere off the trenches of the world that are large enough to be well recorded at teleseismic distances. A number of prominent trends are apparent, some of which have been previously recognized based on more limited data [1], and some of which are largely new [2-5]: (1) The largest events and the highest seismicity rates tend to occur where Mesozoic incoming plates are subducting at high rates (e.g., those in the western Pacific and the Banda segment of Indonesia). The largest events are predominantly shallow normal faulting (SNF) earthquakes. Less common are reverse-faulting (RF) events that tend to be deeper and to be present along with SNF events where nearby seamounts, seamount chains and other volcanic features are subducting [Seno and Yamanaka, 1996]. Blooms of SNF OR/OTS events usually occur just after and seaward of great interplate thrust (IPT) earthquakes but are far less common after smaller IPT events. (2) Plates subducting at slow rates (<20 mm/a) often show sparse OR/OTS seismicity. It is unclear if such low activity is a long-term feature of these systems or is a consequence of the long return times of great IPT earthquakes (e.g., the sparse OR/OTS seismicity before the 26 December 2004 M9.2 Sumatra earthquake and many subsequent OR/OTS events). (3) OR/OTS shocks are generally sparse or absent where incoming plates are very young (<20 Ma) (e.g., Cascadia, southern Mexico, Nankai, and South Shetlands). (4) Subducting plates of intermediate age (20 to about 65 Ma) display a diversity of focal mechanisms and seismicity patterns. In the Philippines, NE Indonesia, and Melanesia, bands of reverse faulting events occur at or near the trench and SNF earthquakes are restricted to OR/OTS sites further from the trench. (5) Clustering of OR/OTS events of all types commonly occurs where

  7. Multi-parameter observation of pre-earthquake signals and their potential for short -term earthquake forecasting

    NASA Astrophysics Data System (ADS)

    Kalenda, Pavel; Ouzounov, Dimitar; Bobrovskiy, Vadim; Neumann, Libor; Boborykina, Olga; Nazarevych, Andrij; Šebela, Stanka; Kvetko, Július; Shen, Wen-Bin

    2013-04-01

    We present methodologies for the multi-parameter observations of pre-earthquake phenomena and their retrospective/prospective testing. The hypothesis that the strongest earthquakes depend on the global stress field leads to global observations and a multi-parameter and multi-sensors approach. In 2012 we performed coordinated tests of several geophysical and environmental parameters, which are associated with the earthquakes preparation processes, namely: 1) Rocks deformation measurements (Kalenda et al. 2012); 2) Subterranean non-stationary electric processes (Bobrovskij 2011); 3) superconducting gravimeters (SGs) records and broadband seismometers (BS) time series (Shen et al); and 4) satellite infra-red observations (10-13 μm) measured at the top of the atmosphere (Ouzounov et al , 2011). In the retrospective test for the two most recent major events in Asia: Wenchuan earthquake (2008,China) and the latest Tohoku earthquake/tsunami (2011, Japan) our combined analysis showed a coordinated appearance of anomalies in advance (days) that could be explained by a coupling process between the observed physical parameters and the earthquake preparation processes. In 2012 three internal retrospective alerts were issued in advance (days) associated with the following events: M7.7 Okhotsk sea of August 14; M7.3 Honshu EQ of December 7 and M7.1 Banda sea EQ on December 10. Not all observations were able to detect anomalies before the M 7.4 Guatemala EQ of November 11. We discuss the reliability of each observation, their time lag, ability to localize and estimate the magnitude of the main shock. References Bobrovskij V. (2011): Kamchatkian Subterranean Electric Operative Forerunners of Catastrophic Earthquake with M9, occurred close to Honshu Island 2011/03/11 . IUGG Meeting Melbourne, 2011. postrer. Kalenda P. et al. (2012): Tilts, global tectonics and earthquake prediction. SWB, London, 247pp. Ozounov D. et al. (2011): Atmosphere-Ionosphere Response to the M9 Tohoku

  8. Preliminary results of teleseismic double-difference relocation of earthquakes around Indonesian archipelago region

    NASA Astrophysics Data System (ADS)

    Nugraha, Andri Dian; Shiddiqi, Hasbi Ash; Widiyantoro, Sri; Ramdhan, Mohamad; Wandono, Sutiyono, Handayani, Titi; Nugroho, Hendro

    2015-04-01

    Indonesian archipelago region is located in active tectonic setting and high seismicity zone. During the last decade, Indonesian was experienced with destructive major earthquakes causing damage and victims. The information of precise earthquake location parameters are very important in partular for earthquake early warning to the society and for advance seismic studies. In this study, we attempted to improve hypocenter location compiled by BMKG for time periods of April, 2009 up to June, 2014 for about 22,000 earthquake events around Indonesian region. For the firts time, we applied teleseismic double-difference relocation algorithm (teletomoDD) to improve hypocenter region in Indonesia region combining regional and teleseismic stations. Hypocenter relocation was performed utilizing local, regional, and teleseismic P-wave arrival time data. Our relocation result show that travel-time RMS errors were greatly reduced compared to the BMKG catalog. Seismicity at shallower depth (less than 50 km) shows significantly improvement especially in depth, and refined shallow geological structures, e.g. trench and major strike slip faults. Clustered seismicity is also detected beneath volcanic region, and probably related volcano activities and also major faults nearby. In the Sunda arc region, seismicity at shallower depth centered at two major distributions parallel to the trench strike direction, i.e. around fore-arc and in mainland that related to major fault, e.g. the Sumatran fault, and volcanic fronts. Below Central Java region, relocated hypocenter result showed double seismic zone pattern. A seismic gap is detected around the Sunda-Banda transition zone where transition between oceanic subduction to continental crust collision of Australian plate occurs. In Eastern Indonesia region, shallow earthquakes are observed related to major strike slip faults, e.g. Sorong and Palu-Koro fault, volcanism, and shallow part of subduction and collision zones. We also compare our

  9. Calibración del retardo ionosférico en observaciones astrométricas y geodésicas a partir de observaciones GPS

    NASA Astrophysics Data System (ADS)

    Brunini, C.; Kleusberg, A.; Arias, E. F.; de Biasi, M. S.

    Los parámetros astrométricos y geodésicos de precisión se determinan hoy mediante la observación con técnicas espaciales (VLBI, GPS y LSR). Las técnicas VLBI y GPS operan en la banda de microondas y en ella la ionósfera terrestre es dispersiva. Las señales que provienen de las radiofuentes y de los satélites atraviesan la ionósfera, donde el índice de refracción difiere de la unidad en una cantidad que es proporcional a la densidad de electrones libres e inversamente proporcional al cuadrado de la frecuencia de la onda portadora. Actualmente el International GPS Service for Geodynamics (IGS) mantiene operacional una red global integrada por más de 50 estaciones equipadas con receptores GPS de alta performance; las observaciones diarias son accesibles a los usuarios mediante ftp. La posibilidad de utilizar estas observaciones en un monitoreo continuo de la ionósfera fue señalada por diversos autores, razón por la cual en los últimos años se ha invertido un significativo esfuerzo en la producción de mapas ionosféricos regionales y globales. En el presente trabajo se utilizan 28 estaciones cuyas observaciones mapean la mayor parte de la ionósfera global. Los resultados obtenidos demuestran la posibilidad de obtener mapas ionosféricos globales con una resolución de medio día y con una precisión de (1.5 nseg (rms)). Dichos mapas proveen valores medios globales para el intervalo ajustado. Los residuos del ajuste por mínimos cuadrados constituyen una señal a partir de la cual pueden estudiarse mejor las variaciones geográficas de la ionósfera y las componentes estadísticas de su variación temporal.

  10. On ambiente de binárias de pequena massa em formação: o caso do glóbulo cometário CG30 e IRAS08076-3556

    NASA Astrophysics Data System (ADS)

    Hickel, G. R.; Vilas-Boas, J. W. S.

    2003-08-01

    Neste trabalho, combinamos observações de polarização linear no óptico (banda R), dados no infravermelho distante (IRAS) e observações de transições moleculares em radiofreqüências (CO e espécies isotópicas, HCN e HCO+) para analisar o glóbulo cometário (GC) CG30 (na região da IRAS Vela Shell), que apresenta objetos Herbig-Haro e ejeções de matéria, além de uma fonte pontual IRAS em seu interior. Os objetivos deste estudo são: determinar a eficiência de formação estelar nos glóbulos cometários, através da relação entre a massa total do GC e da massa das estrelas em formação; determinar como o campo magnético influencia na formação de estrelas no interior destes objetos; e analisar as modificações que ejeções de matéria de estrelas em formação causam no gás e no campo magnético dos GCs. Combinando nossos dados com trabalhos já publicados, mostramos que CG30 tem uma eficiência de formação estelar em torno de 3%; que o campo magnético é importante na manutenção da estrutura global do GC e demonstra sinais de torção e compressão; e que a ejeção bipolar de matéria das estrelas do par formam uma ejeção quadripolar, a qual influencia na densidade e temperatura do gás e no grau de polarização dos grãos de poeira associados ao gás do GC.

  11. Vernal Point and Plate Tectonics: Indo-Australian

    NASA Astrophysics Data System (ADS)

    Chavez C, Teodosio; Chavez-Sumarriva, Israel; Chavez S, Nadia

    2013-04-01

    A precession coordinate system (eccentricity -100Ka, obliquity -40Ka and precession -25Ka) developed by Milankovicht was the precession of the equinoxes, where the vernal point retrograde 1° every 72 years approximately and enter (0°) into the Aquarius constellation on March 20, 1940. On earth this entry was verify through: a) stability of the magnetic equator in the south central zone of Peru and in the north zone of Bolivia, b) the greater intensity of equatorial electrojet (EEJ) in Peru and Bolivia since 1940. The vernal point is a maximum conductivity sensitive axis in the EEJ given at the equinoxes. There was a relationship between the equatorial electrojet - magnetic equator - crust, and besides there was a long history of studies of coupling between earthquake-ionosphere that can be founded in the following revisions: Liperovsky et al. (1990); Gaivoronskaya (1991); Liperovsky et al. (1992); Parrot et al. (1993); Pulinets et al. (1994) and Gokhberg et al. (1995). In IUGG (2007), Cusco was propose as a prime meridian (72° W == 0°) that was parallel to the Andes; the objective was to synchronize the earth sciences phenomena (e.g. geology, geophysics, etc.). The coordinate system had the vernal point from meridian (72° W == 0°) and March 20, 1940. The retrograde movement of the vernal point was the first precessional degree (2012 = 1940 + 72); from the new prime meridian (72° W == 0°) it has obtained the opposite meridian (72° E == 180°). The first precessional degree (2012) near the meridian (72 ° E) was related to the date of April 11, 2012 where a massive earthquake of 8.6 on the Richter scale, followed by several aftershocks, one of 8.2 degrees struck Indonesia with epicenter near Banda Aceh. Five months after that date, Matthias Delescluse et.al (2012), Han Yue et.al (2012), and Fred F. Pollitz et.al, (2012), explained that the two violent earthquakes would be evidence of a break in the Indo-Australian Plate Tectonics caused earthquakes around

  12. Integrated study of geophysical and biological anomalies before earthquakes (seismic and non-seismic), in Austria and Indonesia

    NASA Astrophysics Data System (ADS)

    Straka, Wolfgang; Assef, Rizkita; Faber, Robert; Ferasyi, Reza

    2015-04-01

    Earthquakes are commonly seen as unpredictable. Even when scientists believe an earthquake is likely, it is still hard to understand the indications observed, as well as their theoretical and practical implications. There is some controversy surrounding the concept of using animals as a precursor of earthquakes. Nonetheless, several institutes at University of Natural Resources and Life Sciences, and Vienna University of Technology, both Vienna, Austria, and Syiah Kuala University, Banda Aceh, as well as Terramath Indonesia, Buleleng, both Indonesia, cooperate in a long-term project, funded by Red Bull Media House, Salzburg, Austria, which aims at getting some decisive step forward from anecdotal to scientific evidence of those interdependencies, and show their possible use in forecasting seismic hazard on a short-term basis. Though no conclusive research has yet been published, an idea in this study is that even if animals do not respond to specific geophysical precursors and with enough notice to enable earthquake forecasting on that basis, they may at least enhance, in conjunction with other indications, the degree of certainty we can get of a prediction of an impending earthquake. In Indonesia, indeed, before the great earthquakes of 2004 and 2005, ominous geophysical as well as biological phenomena occurred (but were realized as precursors only in retrospect). Numerous comparable stories can be told from other times and regions. Nearly 2000 perceptible earthquakes (> M3.5) occur each year in Indonesia. Also, in 2007, the government has launched a program, focused on West Sumatra, for investigating earthquake precursors. Therefore, Indonesia is an excellent target area for a study concerning possible interconnections between geophysical and biological earthquake precursors. Geophysical and atmospheric measurements and behavioral observation of several animal species (elephant, domestic cattle, water buffalo, chicken, rat, catfish) are conducted in three areas

  13. 2011 Tohoku tsunami runup hydrographs, ship tracks, upriver and overland flow velocities based on video, LiDAR and AIS measurements

    NASA Astrophysics Data System (ADS)

    Fritz, H. M.; Phillips, D. A.; Okayasu, A.; Shimozono, T.; Liu, H.; Takeda, S.; Mohammed, F.; Skanavis, V.; Synolakis, C.; Takahashi, T.

    2014-12-01

    The 2004 Indian Ocean tsunami marked the advent of survivor videos mainly from tourist areas in Thailand and basin-wide locations. Near-field video recordings on Sumatra's north tip at Banda Aceh were limited to inland areas a few kilometres off the beach (Fritz et al., 2006). The March 11, 2011, magnitude Mw 9.0 earthquake off the Tohoku coast of Japan caused catastrophic damage and loss of life resulting in the costliest natural disaster in recorded history. The mid-afternoon tsunami arrival combined with survivors equipped with cameras on top of vertical evacuation buildings provided numerous inundation recordings with unprecedented spatial and temporal resolution. High quality tsunami video recording sites at Yoriisohama, Kesennuma, Kamaishi and Miyako along Japan's Sanriku coast were surveyed, eyewitnesses interviewed and precise topographic data recorded using terrestrial laser scanning (TLS). The original video recordings were recovered from eyewitnesses and the Japanese Coast Guard (JCG). The analysis of the tsunami videos follows an adapted four step procedure (Fritz et al., 2012). Measured overland flow velocities during tsunami runup exceed 13 m/s at Yoriisohama. The runup hydrograph at Yoriisohama highlights the under sampling at the Onagawa Nuclear Power Plant (NPP) pressure gauge, which skips the shorter period second crest. Combined tsunami and runup hydrographs are derived from the videos based on water surface elevations at surface piercing objects and along slopes identified in the acquired topographic TLS data. Several hydrographs reveal a draw down to minus 10 m after a first wave crest exposing harbor bottoms at Yoriisohama and Kamaishi. In some cases ship moorings resist the main tsunami crest only to be broken by the extreme draw down. A multi-hour ship track for the Asia Symphony with the vessels complete tsunami drifting motion in Kamaishi Bay is recovered from the universal ship borne AIS (Automatic Identification System). Multiple

  14. 2011 Tohoku tsunami video and TLS based measurements: hydrographs, currents, inundation flow velocities, and ship tracks

    NASA Astrophysics Data System (ADS)

    Fritz, H. M.; Phillips, D. A.; Okayasu, A.; Shimozono, T.; Liu, H.; Takeda, S.; Mohammed, F.; Skanavis, V.; Synolakis, C. E.; Takahashi, T.

    2012-12-01

    The March 11, 2011, magnitude Mw 9.0 earthquake off the coast of the Tohoku region caused catastrophic damage and loss of life in Japan. The mid-afternoon tsunami arrival combined with survivors equipped with cameras on top of vertical evacuation buildings provided spontaneous spatially and temporally resolved inundation recordings. This report focuses on the surveys at 9 tsunami eyewitness video recording locations in Myako, Kamaishi, Kesennuma and Yoriisohama along Japan's Sanriku coast and the subsequent video image calibration, processing, tsunami hydrograph and flow velocity analysis. Selected tsunami video recording sites were explored, eyewitnesses interviewed and some ground control points recorded during the initial tsunami reconnaissance in April, 2011. A follow-up survey in June, 2011 focused on terrestrial laser scanning (TLS) at locations with high quality eyewitness videos. We acquired precise topographic data using TLS at the video sites producing a 3-dimensional "point cloud" dataset. A camera mounted on the Riegl VZ-400 scanner yields photorealistic 3D images. Integrated GPS measurements allow accurate georeferencing. The original video recordings were recovered from eyewitnesses and the Japanese Coast Guard (JCG). The analysis of the tsunami videos follows an adapted four step procedure originally developed for the analysis of 2004 Indian Ocean tsunami videos at Banda Aceh, Indonesia (Fritz et al., 2006). The first step requires the calibration of the sector of view present in the eyewitness video recording based on ground control points measured in the LiDAR data. In a second step the video image motion induced by the panning of the video camera was determined from subsequent images by particle image velocimetry (PIV) applied to fixed objects. The third step involves the transformation of the raw tsunami video images from image coordinates to world coordinates with a direct linear transformation (DLT) procedure. Finally, the instantaneous tsunami

  15. 2011 Japan tsunami current and flow velocity measurements from survivor videos using LiDAR

    NASA Astrophysics Data System (ADS)

    Fritz, H. M.; Phillips, D. A.; Okayasu, A.; Shimozono, T.; Liu, H.; Mohammed, F.; Skanavis, V.; Synolakis, C.; Takahashi, T.

    2011-12-01

    On March 11, 2011, a magnitude Mw 9.0 earthquake occurred off the coast of Japan's Tohoku region causing catastrophic damage and loss of life. Numerous tsunami reconnaissance trips were conducted in Japan (Tohoku Earthquake and Tsunami Joint Survey Group). This report focuses on the surveys at 9 tsunami eyewitness video recording locations in Yoriisohama, Kesennuma, Kamaishi and Miyako along Japan's Sanriku coast and the subsequent video image calibration, processing and tsunami flow velocity analysis. Selected tsunami video recording sites were visited, eyewitnesses interviewed and some ground control points recorded during the initial tsunami reconnaissance from April 9 to 25. A follow-up survey from June 9 to 15, 2011 focused on terrestrial laser scanning (TLS) at locations with previously identified high quality eyewitness videos. We acquired precise topographic data using TLS at nine video sites with multiple scans acquired from different instrument positions at each site. These ground-based LiDAR measurements produce a 3-dimensional "point cloud" dataset. Digital photography from a scanner-mounted camera yields photorealistic 3D images. Integrated GPS measurements allow accurate georeferencing of the TLS data in an absolute reference frame such as WGS84. We deployed a Riegl VZ-400 scanner (1550 nm wavelength laser, 42,000 measurements/second, <600 meter max range) and peripheral equipment from the UNAVCO instrument pool. The original full length videos recordings were recovered from eyewitnesses and the Japanese Coast Guard (JCG). Multiple videos were synchronized and referenced in time (UTC). The analysis of the tsunami videos follows a four step procedure developed for the analysis of 2004 Indian Ocean tsunami videos at Banda Aceh, Indonesia (Fritz et al., 2006). The first step requires the calibration of the sector of view present in the eyewitness video recording based on visually identifiable ground control points measured in the LiDAR point cloud data

  16. 2011 Japan tsunami survivor video based hydrograph and flow velocity measurements using LiDAR

    NASA Astrophysics Data System (ADS)

    Fritz, H. M.; Phillips, D. A.; Okayasu, A.; Shimozono, T.; Liu, H.; Mohammed, F.; Skanavis, V.; Synolakis, C. E.; Takahashi, T.

    2012-04-01

    On March 11, 2011, a magnitude Mw 9.0 earthquake occurred off the coast of Japan's Tohoku region causing catastrophic damage and loss of life. Numerous tsunami reconnaissance trips were conducted in Japan (Tohoku Earthquake and Tsunami Joint Survey Group). This report focuses on the surveys at 9 tsunami eyewitness video recording locations in Yoriisohama, Kesennuma, Kamaishi and Miyako along Japan's Sanriku coast and the subsequent video image calibration, processing, tsunami hydrograph and flow velocity analysis. Selected tsunami video recording sites were visited, eyewitnesses interviewed and some ground control points recorded during the initial tsunami reconnaissance from April 9 to 25. A follow-up survey from June 9 to 15, 2011 focused on terrestrial laser scanning (TLS) at locations with previously identified high quality eyewitness videos. We acquired precise topographic data using TLS at nine video sites with multiple scans acquired from different instrument positions at each site. These ground-based LiDAR measurements produce a 3-dimensional "point cloud" dataset. Digital photography from a scanner-mounted camera yields photorealistic 3D images. Integrated GPS measurements allow accurate georeferencing of the TLS data in an absolute reference frame such as WGS84. We deployed a Riegl VZ-400 scanner (1550 nm wavelength laser, 42,000 measurements/second, <600 meter max range) and peripheral equipment from the UNAVCO instrument pool. The original full length videos recordings were recovered from eyewitnesses and the Japanese Coast Guard (JCG). Multiple videos were synchronized and referenced in time (UTC). The analysis of the tsunami videos follows a four step procedure developed for the analysis of 2004 Indian Ocean tsunami videos at Banda Aceh, Indonesia (Fritz et al., 2006). The first step requires the calibration of the sector of view present in the eyewitness video recording based on visually identifiable ground control points measured in the LiDAR point

  17. Effects of Isotropic and Anisotropic Structure in the Lowermost Mantle on High-Frequency Body Waveforms

    NASA Astrophysics Data System (ADS)

    Parisi, L.; Ferreira, A. M. G.; Ritsema, J.

    2015-12-01

    It has been observed that vertically (SV) and horizontally (SH) polarised S waves crossing the lowermost mantle sometimes are split by a few seconds The splitting of such waves is often interpreted in terms of seismic anisotropy in the D" region. Here we investigate systematically the effects of elastic, anelastic, isotropic and anisotropic structure on shear-wave splitting, including 3-D variations in some of these physical properties. Taking advantage of accurate waveform modeling techniques such as Gemini and the Spectral Element Method we generate three-component theoretical waveforms in a wide set of 1-D and 3-D, isotropic and radially anisotropic earth models, accurate down to a wave period of T~5.6s. Our numerical simulations in isotropic earth models show that the contamination of S waves by other phases can generate an apparent splitting between SH and SV waves. In particular, in the case of very shallow sources, the sS phase can interfere with the direct S phase, resulting in split SH and SV pulses when the SH and SV (or sSH and sSV) waves have different polarity or a substantial amplitude difference. In the case of deep earthquake sources, a positive shear velocity jump at the top of the D" can cause the triplication of S waves and the ScSH and ScSV phases can have different polarity. Thus, when the triplicated S wave is combined with the ScS phase, the resulting SH-ScSH and SV-ScSV phases may seem split. On the other hand, in the absence of a sharp vertical variation in the shear wave velocity, the difference in polarity between ScSH and ScSV can make the SH pulse larger than SV and thus also lead to apparent splitting between these phases. This effect depends on the thickness of the D" and the Vs gradient within it. S waveforms simulated in radially anisotropic models reveal that a radial anisotropy of ξ=1.07 in the D" seems to be necessary to explain the 2-3s of splitting observed in waveforms recorded in Tanzania from an event in the Banda Sea

  18. Sedimentary deposits of the 26 December 2004 tsunami on the northwest coast of Aceh, Indonesia

    USGS Publications Warehouse

    Moore, A.; Nishimura, Y.; Gelfenbaum, G.; Kamataki, T.; Triyono, R.

    2006-01-01

    The 2004 Sumatra-Andaman tsunami flooded coastal northern Sumatra to a depth of over 20 m, deposited a discontinuous sheet of sand up to 80 cm thick, and left mud up to 5 km inland. In most places the sand sheet is normally graded, and in some it contains complex internal stratigraphy. Structures within the sand sheet may record the passage of up to 3 individual waves. We studied the 2004 tsunami deposits in detail along a flow-parallel transect about 400 m long, 16 km southwest of Banda Aceh. Near the shore along this transect, the deposit is thin or absent. Between 50 and 400 m inland it ranges in thickness from 5 to 20 cm. The main trend in thickness is a tendency to thicken by filling low spots, most dramatically at pre-existing stream channels. Deposition generally attended inundation - along the transect, the tsunami deposited sand to within about 40 m of the inundation limit. Although the tsunami deposit contains primarily material indistinguishable from material found on the beach one month after the event, it also contains grain sizes and compositions unavailable on the current beach. Along the transect we studied, these grains become increasingly dominant both landward and upward in the deposit; possibly some landward source of sediment was exposed and exploited by the passage of the waves. The deposit also contains the unabraded shells of subtidal marine organisms, suggesting that at least part of the deposit came from offshore. Grain sizes within the deposit tend to fine upward and landward, although individual units within the deposit appear massive, or show reverse grading. Sorting becomes better landward, although the most landward sites generally become poorly sorted from the inclusion of soil clasts. These sites commonly show interlayering of sandy units and soil clast units. Deposits from the 2004 tsunami in Sumatra demonstrate the complex nature of the deposits of large tsunamis. Unlike the deposits of smaller tsunamis, internal stratigraphy is

  19. Toward tsunami early warning system in Indonesia by using rapid rupture durations estimation

    SciTech Connect

    Madlazim

    2012-06-20

    Indonesia has Indonesian Tsunami Early Warning System (Ina-TEWS) since 2008. The Ina-TEWS has used automatic processing on hypocenter; Mwp, Mw (mB) and Mj. If earthquake occurred in Ocean, depth < 70 km and magnitude > 7, then Ina-TEWS announce early warning that the earthquake can generate tsunami. However, the announcement of the Ina-TEWS is still not accuracy. Purposes of this research are to estimate earthquake rupture duration of large Indonesia earthquakes that occurred in Indian Ocean, Java, Timor sea, Banda sea, Arafura sea and Pasific ocean. We analyzed at least 330 vertical seismogram recorded by IRIS-DMC network using a direct procedure for rapid assessment of earthquake tsunami potential using simple measures on P-wave vertical seismograms on the velocity records, and the likelihood that the high-frequency, apparent rupture duration, T{sub dur}. T{sub dur} can be related to the critical parameters rupture length (L), depth (z), and shear modulus ({mu}) while T{sub dur} may be related to wide (W), slip (D), z or {mu}. Our analysis shows that the rupture duration has a stronger influence to generate tsunami than Mw and depth. The rupture duration gives more information on tsunami impact, Mo/{mu}, depth and size than Mw and other currently used discriminants. We show more information which known from the rupture durations. The longer rupture duration, the shallower source of the earthquake. For rupture duration greater than 50 s, the depth less than 50 km, Mw greater than 7, the longer rupture length, because T{sub dur} is proportional L and greater Mo/{mu}. Because Mo/{mu} is proportional L. So, with rupture duration information can be known information of the four parameters. We also suggest that tsunami potential is not directly related to the faulting type of source and for events that have rupture duration greater than 50 s, the earthquakes generated tsunami. With available real-time seismogram data, rapid calculation, rupture duration discriminant

  20. Screening in a Lactobacillus delbrueckii subsp. bulgaricus collection to select a strain able to survive to the human intestinal tract.

    PubMed

    Vázquez, Clotilde; Botella-Carretero, José I; García-Albiach, Raimundo; Pozuelo, María J; Rodríguez-Baños, Mercedes; Baquero, Fernando; Baltadjieva, María A; del Campo, Rosa

    2013-01-01

    Objetivos: Se determinaron la diversidad genética y la resistencia de una colección de más de 100 cepas de Lactobacillus bulgaricus subespecie delbrueckii, aisladas de diferentes yogures caseros de las áreas rurales de Bulgaria. Métodos: La cepa K98 fue la más resistente a las sales biliares y al pH bajo. La supervivencia y los efectos sobre la producción de ácidos grasos de cadena corta se evaluó en 20 voluntarios sanos. Se observó una alta diversidad genética en la colección de L. bulgaricus mediante RAPD, mientras que la capacidad de tolerar concentraciones altas del ácido desoxicólico y de diferentes niveles de pH fue variable. Se seleccionó la cepa K98 y se usó para preparar un yogur casero que se administró a los 20 voluntarios (500 ml/día durante 15 días). Se recogieron muestras fecales basales y tras la ingesta del yogur. Resultados: Los experimentos DGGE, empleando cebadores universales y para bacterias ácido-lácticas (BAL) demostraron que no hubo cambios significativos en la composición cualitativa de la composición de la microflora intestinal. Se observó una banda correspondiente a L. bulgaricus en las 20 muestras. Sólo se recuperó una cepa viable de L. bulgaricus K98 en un único voluntario. Tras la ingesta de yogur, hallamos un aumento de BAL y de Clostridium perfringens y una disminución de Bacteroides- Prevotella-Porphyromonas. Además, se detectó un aumento en las heces de los ácidos acético, butírico y 2-hidroxibutírico. Conclusiones: La diversidad genética de L. delbrueckii subespecie bulgaricus es alta. Hemos aislado una cepa probiótica resistente a la bilis y a la acidez elevada, L. delbrueckii subesp. bulgaricus-K98. Se hallaron cambios cualitativos y cuantitativos en la microflora intestinal tras la ingesta de yogur casero que contenía esta cepa, con un aumento concomitante en las heces de AGCC. Nuestros hallazgos apoyan el interés por desarrollar estudios futuros con cantidades variables de L. delbrueckii

  1. Constraining Basin Geometry and Fault Kinematics on the Santo Tomas Segment of the Agua Blanca Fault Through a Combined Geophysical and Structural Study

    NASA Astrophysics Data System (ADS)

    Springer, A.; Wetmore, P.; Fletcher, J.; Connor, C. B.; Callihan, S.; Beeson, J.; Wilson, J.

    2008-12-01

    The Santo Tomas basin, located in northern Baja California, formed at a right step in the dextral Agua Blanca fault (ABF). The ABF extends for more than 120km east from Punta Banda, with an east-west strike, and represents the southernmost fault in the San Andreas system of faulting. The basin is located roughly 40km south of Ensenada where the Agua Blanca fault intersects the Maximos fault. A detailed geophysical analysis defines the basin geometry, and helps to constrain the distribution and offset of mapped and concealed faults. Geophysical and structural data sets are combined to constrain the kinematic evolution of the Santo Tomas basin, including determining the relative amount of dip-slip and strike-slip motion on basin-bounding faults. Gravity data was collected over seven transects across and along the axis of the basin at 500 meter intervals, with 200 meter intervals at locations of known or inferred faults. Magnetic data were taken over the same lines, and are used in conjunction with gravity data to constrain the locations, geometries and displacements of intrabasinal faults. The combined gravity and magnetic data are modeled using Geosoft Oasis montaj software to create 2 3/4D models along profiles across the study area. Modeling of the geophysical data combined with structural mapping indicates that the Santo Tomas basin is bound by two major strike-slip faults, the ABF on the northeastern side and the Maximos fault on south, Based on offset markers, most of the strike-slip motion appears to be concentrated on the ABF on the north side of the basin. The ABF fault is characterized by multiple subparallel fault strands that appear to coalesce into single strands to the northwest and southeast of the basin. The Maximos is characterized by a single strand throughout the basin and it exhibits a minor dip-slip component. Basin sediments thicken slightly against the Maximos fault to as much as 1km. A third fault, cutting across the basin southeast of the

  2. Refinements on the inferred causative faults of the great 2012 Indian Ocean earthquakes

    NASA Astrophysics Data System (ADS)

    Revathy, P. M.; Rajendran, K.

    2014-12-01

    As the largest known intra-plate strike-slip events, the pair of 2012 earthquakes in the Wharton Basin is a rarity. Separated in time by 2 hours these events rouse interest also because of their short inter-event duration, complex rupture mechanism, and spatial-temporal proximity to the great 2004 Sumatra plate boundary earthquake. Reactivation of fossil ridge-transform pairs is a favoured mechanism for large oceanic plate earthquakes and their inherent geometry triggers earthquakes on conjugate fault systems, as observed previously in the Wharton Basin. The current debate is whether the ruptures occurred on the WNW-ESE paleo ridges or the NNE-SSW paleo transforms. Back-projection models give a complex rupture pattern that favours the WNW-ESE fault [1]. However, the static stress changes due to the 2004 Sumatra earthquake and 2005 Nias earthquake favour the N15°E fault [2]. We use the Teleseismic Body-Wave Inversion Program [3] and waveform data from Global Seismic Network, to obtain the best fit solutions using P and S-wave synthetic modelling. The preliminary P-wave analysis of both earthquakes gives source parameters that are consistent with the Harvard CMT solutions. The obtained slip distribution complies with the NNE-SSW transforms. Both these earthquakes triggered small tsunamis which appear as two distinctive pulses on 13 Indian Ocean tide gauges and buoys. Frequency spectra of the tsunami recordings from various azimuths provide additional constraint for the choice of the causative faults. References: [1] Yue, H., T. Lay, and K. D. Koper (2012), En echelon and orthogonal fault ruptures of the 11 April 2012 great intraplate earthquakes, Nature, 490, 245-249, doi:10.1038/nature11492 [2] Delescluse, M., N. Chamot-Rooke, R. Cattin, L. Fleitout, O. Trubienko and C. Vigny April 2012 intra-oceanic seismicity off Sumatra boosted by the Banda-Aceh megathrust, Nature, 490(2012), pp. 240-244, doi:10.1038/nature11520 [3] M. Kikuchi and H. Kanamori, Note on

  3. Phreatomagmatic to Strombolian eruptive activity of basaltic cinder cones: Montaña Los Erales, Tenerife, Canary Islands

    NASA Astrophysics Data System (ADS)

    Clarke, Hilary; Troll, Valentin R.; Carracedo, Juan Carlos

    2009-03-01

    Phreatomagmatic activity results from the interaction of magma and external water during a volcanic eruption and is a frequent eruptive phenomenon worldwide. Such 'fuel-coolant' reactions change the eruptive dynamics, thus generating particles that reflect the degree of explosivity. Different eruptive phases may thus be identified from deposits, allowing us to reconstruct conditions that prevailed in the past and use these to predict the level of explosivity in a given geological setting in the future. A detailed study of the deposits from Montaña Los Erales, a 70 m-high Quaternary cinder cone belonging to a rift-related chain of vents in the Bandas del Sur region, in Southeast Tenerife, was undertaken. Field observations on excavated sections and SEM analysis of tephra suggest that the eruption style changed progressively from an initial phreatomagmatic phase, through a transitional stage, to one that was entirely Strombolian. To investigate the causes and the nature of these changes in eruptive style, products from each major unit were analysed for their morphology using hand specimen observations, secondary electron microscopy, backscatter electron microscopy, and reflected light microscopy to examine fragment size variation, fragment morphologies, vesicularity, and the level of secondary hydrous alteration (e.g. palagonitisation and zeolitisation). Study results demonstrate that the initial phase of activity was largely driven by magma-water interaction, where magma may have interacted with a lens of fresh ground- or surface water. With proceeding eruptive activity the water became exhausted, giving rise to an entirely Strombolian eruptive style. Examples of phreatomagmatic activity that occur on typical rift-related basaltic vent alignments are not infrequent in the Canary Islands. These vent systems usually erupt in Strombolian fashion, producing scoria and lava flows that do not generally extend far beyond the vent area. However, aligned feeders may

  4. The origin of mélanges: Cautionary tales from Indonesia

    NASA Astrophysics Data System (ADS)

    Barber, A. J.

    2013-10-01

    The origin of block-in-matrix mélanges has been the subject of intense speculation by structural and tectonic geologists working in accretionary complexes since their first recognition in the early twentieth century. Because of their enigmatic nature, a number of important international meetings and a large number of publications have been devoted to the problem of the origin of mélanges. As mélanges show the effects of the disruption of lithological units to form separate blocks, and also apparently show the effects shearing in the scaly fabric of the matrix, a tectonic origin has often been preferred. Then it was suggested that the disruption to form the blocks in mélanges could also occur in a sedimentary environment due to the collapse of submarine fault scarps to form olistostromes, upon which deformation could be superimposed tectonically. Subsequently it has proposed that some mélanges have originated by overpressured clays rising buoyantly towards the surface, incorporating blocks of the overlying rocks in mud or shale diapirs and mud volcanoes. Two well-known examples of mélanges from the Banda and Sunda arcs are described, to which tectonic and sedimentary origins were confidently ascribed, which proved on subsequent examination to have been formed due to mud diapirism, in a dynamically active environment, as the result of tectonism only indirectly. Evidence from the Australian continental Shelf to the south of Sumba shows that large quantities of diapiric mélange were generated before the diapirs were incorporated in the accretionary complex. Comparable diapirs can be recognised in Timor accreted at an earlier stage. Evidence from both Timor and Nias shows that diapiric mélange can be generated well after the initial accretion process was completed. The problem is: Why, when diapirism is so abundantly found in present convergent margins, is it so rarely reported from older orogenic belts? Many occurrences of mélanges throughout the world to

  5. Spatial variations of effective elastic thickness of the Lithosphere in the Southeast Asia regions

    NASA Astrophysics Data System (ADS)

    Shi, Xiaobin; Kirby, Jon; Yu, Chuanhai; Swain, Chris; Zhao, Junfeng

    2016-04-01

    The effective elastic thickness Te corresponds to the thickness of an idealized elastic beam that would bend similarly to the actual lithosphere under the same applied loads, and could provide important insight into rheology and state of stress. Thus, it is helpful to improve our understanding of the relationship between tectonic styles, distribution of earthquakes and lithospheric rheology in various tectonic settings. The Southeast Asia, located in the southeastern part of the Eurasian Plate, comprises a complex collage of continental fragments, volcanic arcs, and suture zones and marginal oceanic basins, and is surrounded by tectonically active margins which exhibit intense seismicity and volcanism. The Cenozoic southeastward extrusion of the rigid Indochina Block due to the Indo-Asian collision resulted in the drastic surface deformation in the western area. Therefore, a high resolution spatial variation map of Te might be a useful tool for the complex Southeast Asia area to examine the relationships between surface deformation, earthquakes, lithospheric structure and mantle dynamics. In this study, we present a high-resolution map of spatial variations of Te in the Southeast Asia area using the wavelet method, which convolves a range of scaled wavelets with the two data sets of Bouguer gravity anomaly and topography. The topography and bathymetry grid data was extracted from the GEBCO_08 Grid of GEBCO digital atlas. The pattern of Te variations agrees well with the tectonic provinces in the study area. On the whole, low lithosphere strength characterizes the oceanic basins, such as the South China Sea, the Banda sea area, the Celebes Sea, the Sulu Sea and the Andaman Sea. Unlike the oceanic basins, the continental fragments show a complex pattern of Te variations. The Khorat plateau and its adjacent area show strong lithosphere characteristics with a Te range of 20-50 km, suggesting that the Khorat plateau is the strong core of the Indochina Block. The West

  6. Impact of the viscoelastic postseismic deformation following megathrust earthquake on seismic hazard in subduction zones : the case of the Maule and Illapel earthquakes in Chile

    NASA Astrophysics Data System (ADS)

    Klein, Emilie; Vigny, Christophe; Fleitout, Luce; Garaud, Jean-Didier

    2016-04-01

    , precisely where the Illapel earthquake occurred. Therefore, we suggest that post-seismic relaxation after the Maule Earthquake has been instrumental (along with geometrical particularities of the slab geometry in this area) in triggering the 2015 rupture and forbidding (for now) a similar earthquake in front of Valparaiso. We suggest the same mechanism has been active along the Sumatran trench where a similar highly coupled and mature seismic gap remains unbroken between the Banda-Aceh and Nias earthquakes of 2004 and 2005 on one side and the Bengkulu earthquake of 2007 on the other side : the Padang gap.

  7. Evaluation of an operational ocean model configuration at 1/12° spatial resolution for the Indonesian seas (NEMO2.3/INDO12) - Part 2: Biogeochemistry

    NASA Astrophysics Data System (ADS)

    Gutknecht, Elodie; Reffray, Guillaume; Gehlen, Marion; Triyulianti, Iis; Berlianty, Dessy; Gaspar, Philippe

    2016-04-01

    Banda Sea and at the exit of the archipelago. While the model overestimates the mean surface chlorophyll a, the seasonal cycle is in phase with satellite estimations, with higher chlorophyll a concentrations in the southern part of the archipelago during the SE monsoon and in the northern part during the NW monsoon. The time series of chlorophyll a anomalies suggests that meteorological and ocean physical processes that drive the interannual variability of biogeochemical properties in the Indonesian region are reproduced by the model.

  8. Iron oxide reduction in deep Baltic Sea sediments: the potential role of anaerobic oxidation of methane

    NASA Astrophysics Data System (ADS)

    Egger, Matthias; Slomp, Caroline P.; Dijkstra, Nikki; Sapart, Célia J.; Risgaard-Petersen, Nils; Kasten, Sabine; Riedinger, Natascha; Barker Jørgensen, Bo

    2015-04-01

    Methane is a powerful greenhouse gas and its emission from marine sediments to the atmosphere is largely controlled by anaerobic oxidation of methane (AOM). Traditionally, sulfate is considered to be the most important electron acceptor for AOM in marine sediments. However, recent studies have shown that AOM may also be coupled to the reduction of iron (Fe) oxides (Beal et al., 2009; Riedinger et al., 2014; Egger et al., 2014). In the Baltic Sea, the transition from the Ancylus freshwater phase to the Littorina brackish/marine phase (A/L-transition) ca. 9-7 ka ago (Zillén et al., 2008) resulted in the accumulation of methanogenic brackish/marine sediments overlying Fe-oxide rich lacustrine deposits. The downward diffusion of methane from the brackish/marine sediments into the lake sediments leads to an ideal diagenetic system to study a potential coupling between Fe oxide reduction and methane oxidation. Here, we use porewater and sediment geochemical data obtained at sites M0063 and M0065 during the IODP Baltic Sea Paleoenvironment Expedition 347 in 2013 to identify the potential mechanisms responsible for the apparent Fe oxide reduction in the non-sulfidic limnic sediments below the A/L transition. In this presentation, we will review the various explanations for the elevated ferrous Fe in the porewater in the lake sediments and we will specifically address the potential role of the reaction of methane with Fe-oxides. References: Beal E. J., House C. H. and Orphan V. J. (2009) Manganese- and iron-dependent marine methane oxidation. Science 325, 184-187. Egger M., Rasigraf O., Sapart C. J., Jilbert T., Jetten M. S. M., Röckmann T., van der Veen C., Banda N., Kartal B., Ettwig K. F. and Slomp C. P. (2014) Iron-mediated anaerobic oxidation of methane in brackish coastal sediments. Environ. Sci. Technol. 49, 277-283. Riedinger N., Formolo M. J., Lyons T. W., Henkel S., Beck A. and Kasten S. (2014) An inorganic geochemical argument for coupled anaerobic oxidation of

  9. Observações espectroscópicas da candidata a pós-AGB IRAS 19386+0155

    NASA Astrophysics Data System (ADS)

    Lorenz-Martins, S.; Pereira, C. B.

    2003-08-01

    Nesse trabalho apresentamos a análise fotosférica da estrela candidata a pós-AGB IRAS 19386+0155. Com os dados obtidos no espectrógrafo FEROS foram determinados os parâmetros atmosféricos e abundâncias fotosféricas utilizando o código MOOG. A análise do espectro mostrou que IRAS 19386+0155 possui os seguintes parâmetros atmosféricos : Teff = 6800K, log g = 1.4, [M/H] = -1.5 e Vt = 8.4 km/s. O padrão de abundância obtido para os elementos mais leves (Carbono, Nitrogênio e Oxigênio) e elementos a (Magnésio, Silício e Cálcio) foi inferior ao solar (log C = 7.74, log N = 7.28, Log O = 8.43, log Mg = 7.14, log Si = 7.54 e log Ca = 5.91). Uma inspeção visual do espectro ISO deste objeto revela a presença de poeira fria na forma de silicatos cristalinos. Embora as bandas mais marcantes de silicatos amorfos (em 10 mm e 18mm) não sejam observadas, a emissão em 21 mm, presente em algumas pós-AGBs também não está presente. O espectro ISO parece revelar um meio rico em oxigênio, mas a forma da distribuição de energia no infravermelho não obedece ao padrão apresentado por outras pós-AGBs. Nossos resultados nos levam a sugerir que IRAS 19386+0155 talvez faça parte de um sistema binário, uma vez que outras pós-AGBs que são membros de sistemas binários apresentam padrão de abundância semelhante.

  10. Three factors to enlarge tsunami disaster in Indonesia after the 2004 Indian Ocean tsunami

    NASA Astrophysics Data System (ADS)

    Sugimoto, M.; Satake, K.

    2010-12-01

    NGO now just concentrates on the first factor, tsunami hazard. We have contributed to education program by using tsunami height poles in Banda Aceh (Fig 1). As for Padang, we try to visualize tsunami by showing inundation data, hazard map and tsunami height poles for people to understand hazard. It is important build up social system to deal with natural hazard. Otherwise natural hazard is amplified by social aspects without proper deals. *Acknowledgment: This work was supported by SATREPS by JST, JICA, RISTEK and LIPI.

  11. A distância e o conteúdo estelar da região HII gigante G333.1-0.4 - vínculos para a taxa de formação estelar da galáxia

    NASA Astrophysics Data System (ADS)

    Figuerêdo, E.; Damineli, A.; Blum, R.; Conti, P.

    2003-08-01

    Neste trabalho apresentamos imagens de alta resolução angular da região HII gigante G333.1-0.4 obtidas através dos filtros J, H e K no telescópio de 4-m do CTIO. Este trabalho faz parte de um estudo de regiões HII gigantes no infravermelho próximo que tem por objetivo estudar a natureza da formação de estrelas massivas e traçar a estrutura espiral de nossa galáxia. Nossa determinação da distância é baseada no método da paralaxe espectroscópica de estrelas OB localizadas na seqüência principal de idade zero (ZAMS) do Diagrama HR. No caso de G333.1-0.4, a magnitude aparente das estrelas localizadas na ZAMS indica que a distância não pode ser maior do que o limite inferior determinado por técnica rádio (2,8 kpc). Resultados semelhantes foram encontrados para regiões estudadas anteriormente, reforçando a idéia de que a taxa de formação estelar na Via Láctea é menor do que o determinado a partir de dados rádio. Nossos resultados mais recentes sobre o conteúdo estelar de G333.1-0.4 revelaram vários objetos que possuem cores bastante avermelhadas (H-K > 2,0). Nós identificamos estes objetos usando os diagramas cor-cor e cor-magnitude dos aglomerados. Estes objetos apresentam um forte excesso em emissão na banda K e possivelmente se tratam de estrelas do tipo OB envolvidas por um disco/envelope circumestelar espesso. O estudo da função de massa inical desta região, em conjunto com resultados de nossos trabalhos anteriores, aponta para uma IMF independente da posição galática. A contagem de estrelas nos fornece um valor para o número de fótons no contínuo de Lyman que corrobora com a afirmação de que G333.1-0.4 se encontra mais próxima da menor distância determinada por rádio.

  12. Las fulguraciones como manifestación de reconexión en el campo magnético solar

    NASA Astrophysics Data System (ADS)

    Bagalá, L. G.; Mandrini, M. C.; Rovira, M. G.; Démoulin, P.

    Las fulguraciones solares son fenómenos transitorios de liberación de energía que se desarrollan en las estructuras magnéticas de las regiones activas del Sol. Las fulguraciones pueden llegar a liberar hasta 1032 erg en 100 seg. en todo el rango electromagnético, y acelerar partículas. En este trabajo mostramos que la ubicación de los abrillantamientos en Hα de diversas fulguraciones está relacionado con las propiedades de las conexiones de las líneas del campo magnético de la región, como se espera por las teorías de reconexión en 3D recientemente desarrolladas (Démoulin et al, 1996a). El campo magnético coronal se extrapola del campo fotosférico observado suponiendo una configuración libre de fuerzas lineal. Por medio de un algoritmo se determinan las regiones donde existe un cambio drástico en la conectividad de las líneas de campo (límites ``cuasi-discontinuos'', o cuasi-separatrices CS). Las CS son bandas abiertas que identifican zonas donde el campo magnético se reconectará con más probabilidad y, siempre que las mismas sean lo suficientemente finas, se producirá allíla liberación de energía proveniente del campo magnético. Hemos encontrado que en todas las regiones fulgurantes estudiadas (Démoulin et al, 1996b) existen CS en los mismos lugares donde se observaron los abrillantamientos en Hα. Allídonde coinciden los abrillantamientos con las CS, éstas tienen un espesor menor que 1 Mm. Las líneas de campo coronales extrapoladas de nuestro modelo tienen sus orígenes fotosféricos a ambos lados de las CS, como se espera dados los recientes estudios de reconexión magnética en 3D. Estos resultados ponen a prueba los modelos presentes sobre fulguraciones solares.

  13. Survey infravermelho do braço espiral de scuttum e da barra no centro galáctico

    NASA Astrophysics Data System (ADS)

    Amôres, E. B.; Lépine, J. R. D.

    2003-08-01

    O survey infravermelho consiste de observações utilizando a CAMIV no telescópio de 60 cm do LNA. Nosso principal objetivo é melhor caracterizar a população estelar dos braços espirais e de uma estrutura existente no centro galáctico que acreditamos ser devido à existência de uma barra, cujas extremidades estariam localizadas em longitudes galácticas l~23° e l~14°. As observações realizadas em vários filtros (imagens J, H e K) são particularmente importantes nas direções que tangenciam os braços espirais, desta forma, comparamos uma direção que atravessa um braço a uma direção próxima que não passa pelo braço, sendo que ambas possuem a mesma contribuição de contagens foreground. Nas missões realizadas até o presente, observamos a região na direção tangencial ao braço de Scuttum, com observações de l = 30.04° até l = 31.04°, a cada intervalo de longitude de 0.1°, para latitude galáctica de 0.0°, 0.25°, 0.50°. Para as regiões que acreditamos serem as extremidades da barra, observamos as faixas de longitude compreendidas entre -15° £ l £ -13° e 24° £ l £ 22° a cada intervalo de 0.25°, para latitude galáctica de 0.0° e 0.25°. As observações nos filtros J e H foram feitas com tempo de integração de 60s, na banda K, as observações foram feitas utilizando o filtro C1 com tempo de integração de aproximadamente 210 s (12x15s). Elaboramos diagramas cor-cor e cor-magnitude onde podemos verificar a existência de regiões com diferentes contagens e população estelar à medida que um braço espiral é atravessado.

  14. Identificação de variáveis cataclísmicas eruptivas na direção do bojo galáctico e Nuvens de Magalhães usando dados do OGLE

    NASA Astrophysics Data System (ADS)

    Cieslinski, D.; Diaz, M. P.; Mennickent, R.; Pietrzyski, G.

    2003-08-01

    Na década de 90 iniciaram-se vários programas para a pesquisa de matéria escura na Galáxia usando o efeito de microlentes gravitacionais. Entre os projetos mais bem conhecidos podemos mencionar o OGLE (Optical Gravitational Lensing Experiment) e o MACHO (MAssive Compact Halo Objects). A estratégia usada por eles consiste em fazer fotometria de banda larga (normalmente B, R e I) de um grande número de estrelas (dezenas de milhões) tão freqüentemente quanto possí vel e por longos perí odos de tempo (anos). Uma tal sistemática de observação, além de descobrir inúmeras lentes gravitacionais, é também muito apropriada para a descoberta de estrelas variáveis. De fato, inúmeras novas variáveis de vários tipos foram descobertas como subproduto. Exemplos podem ser encontrados nos endereços http://bulge.princeton.edu/~ogle/ e http://wwwmacho.mcmaster.ca/. As variáveis cataclí smicas eruptivas (novas clássicas, novas recorrentes e novas anãs) são objetos que apresentam variabilidade de grande amplitude com escalas de tempo de dias a centenas de dias e, por esta razão, devem ter sido detectadas em grande número nestes "surveys". Para testar esta possibilidade nós procuramos nos dados do OGLE por tais sistemas e o presente trabalho mostra os resultados desta pesquisa. Os objetos foram selecionados entre as variáveis detectadas usando a amplitude de variação de brilho como critério principal. Este critério forneceu 13756 objetos, sendo 2169 na direção da Grande Nuvem de Magalhães, 1162 na direção da Pequena Nuvem de Magalhães e o restante na direção do Bojo Galáctico. A análise foi feita inspecionando-se visualmente cada curva de luz por erupções com as características acima mencionadas. Os resultados obtidos podem ser sumarizados como: descoberta de duas novas clássicas e 33 novas anãs. Além disso, pode-se mencionar a identificação de candidatas a outros tipos de variáveis como: estrelas simbióticas, RV Tauri, R Coronae

  15. Discovering Plate Boundaries Update: Builds Content Knowledge and Models Inquiry-based Learning

    NASA Astrophysics Data System (ADS)

    Sawyer, D. S.; Pringle, M. S.; Henning, A. T.

    2009-12-01

    Discovering Plate Boundaries (DPB) is a jigsaw-structured classroom exercise in which students explore the fundamental datasets from which plate boundary processes were discovered. The exercise has been widely used in the past ten years as a classroom activity for students in fifth grade through high school, and for Earth Science major and general education courses in college. Perhaps more importantly, the exercise has been used extensively for professional development of in-service and pre-service K-12 science teachers, where it simultaneously builds content knowledge in plate boundary processes (including natural hazards), models an effective data-rich, inquiry-based pedagogy, and provides a set of lesson plans and materials which teachers can port directly into their own classroom (see Pringle, et al, this session for a specific example). DPB is based on 4 “specialty” data maps, 1) earthquake locations, 2) modern volcanic activity, 3) seafloor age, and 4) topography and bathymetry, plus a fifth map of (undifferentiated) plate boundary locations. The jigsaw is structured so that students are first split into one of the four “specialties,” then re-arranged into groups with each of the four specialties to describe the boundaries of a particular plate. We have taken the original DPB materials, used the latest digital data sets to update all the basic maps, and expanded the opportunities for further student and teacher learning. The earthquake maps now cover the recent period including the deadly Banda Aceh event. The topography/bathymetry map now has global coverage and uses ice-free elevations, which can, for example, extend to further inquiry about mantle viscosity and loading processes (why are significant portions of the bedrock surface of Greenland and Antarctica below sea level?). The volcanic activity map now differentiates volcano type and primary volcanic lithology, allowing a more elaborate understanding of volcanism at different plate boundaries

  16. Reconstruction of multiple tectonic events in continental margins by integrated tectonostratigraphic and geochronological analysis: the Mesozoic to Paleogene Caribbean-South American interaction in northeastern Colombia

    NASA Astrophysics Data System (ADS)

    Cardona, Agustin; Montes, Camilo; Bayona, German; Valencia, Victor; Ramirez, Diego; Zapata, Sebastian; Lara, Mario; Lopez-Martinez, Margarita; Thomson, Stuart; Weber, Marion

    2013-04-01

    Although the older record and successive tectonic scenarios experienced by a continental margin is commonly fragmentary, integrated field, petrological and geochronological analysis can reconstruct the long term tectonic evolution of continental margins and characterized major controls on the orogenic style. We present new geochronological constraints from igneous and low to very low grade metasedimentary rocks from the Caribbean continental margin of northeastern Colombia (Guajira region) in order to reconstruct the different tectonic events recorded by the margin before, during and following the arc-continent collision with the front of the Caribbean plate. Zircon U-Pb LA-ICP-MS geochronology results from leucogranites associated with garnet amphibolites, tonalites and volcanic rocks that made the continental basement of northeastern Colombia reveals and Early to Middle Mesozoic tectonic activity with peaks at ca. 220-230 Ma and 170-180 Ma. This magmatic record is related to a collisional belt link to the final agglutination of Pangea and was followed by an overimposed far field back-arc setting associated to the subduction of the Pacific (Farrallon) plate under the Pangea supercontinent. Muscovite and biotite Ar-Ar geochronology from basement rocks and low grade Mesozoic metasediments also reveals the existence of Middle Jurassic to Early Cretaceous thermal events link to the final opening of the proto-Caribbean ocean. The South American continental margin was subsequently affected by an arc-continent collisional event with the front of the Caribbean plate. This event is recorded by the growth of a Banda-type collisional melange that mixed South American continental margin sediments with mafic and ultramafic blocks of intra-oceanic arc origin, the formation of a coherent metasedimentary belt also made of South American margin sediments, and the mylonitization of the continental basement. Ar-Ar temporal constraints on the low grade metasedimentary rocks and

  17. Mapping mantle-melting anomalies in Baja California: a combined helium-seismology approach

    NASA Astrophysics Data System (ADS)

    Negrete-Aranda, R.; Spelz, R. M.; Hilton, D. R.; Tellez, M.; González-Yahimovich, O.

    2015-12-01

    In active tectonic settings, the presence of helium in aqueous fluids with 3He/4He ratios greater than in-situ production values (~0.05 RA where RA = air He or 1.4 x 10-6) indicates the contribution of mantle-derived volatiles to the total volatile inventory. This is an indicative of the presence of mantle-derived melts, which act to transfer volatiles from the solid Earth towards the surface. Thus, He has the potential to map regions of the underlying mantle which are undergoing partial melting - a phenomenon which should also be evident in the seismic record. Reports of high 3He/4He in hot springs in Baja California (BC) has prompted us to initiate a survey of the region to assess relationship(s) between He isotopes and geophysical images of the underlying mantle. Previous studies report 3He/4He ratios of 0.54 RA for submarine hot springs (Punta Banda 108oC; Vidal, 1982) and 1.3 RA for spring waters (81oC) at Bahia Concepcion (Forrest et al.,2005). Our new survey of hot springs in northern BC has revealed that all 6 localities sampled to date, show the presence of mantle He with the highest ratio being 1.74RA (21% mantle-derived) at Puertecitos on the Gulf coast. He ratios are generally lower on the Pacific coast with the minimum mantle He contribution being 5% at Sierra Juárez (0.11RA). Thus, preliminary trends are of a west-to-east increase in the mantle He signal across the peninsula. He results presented in this study correlate well with high resolution Rayleigh wave tomography images by Forsythe et al. (2007). Shear velocity variations in the BC crust and upper mantle have been interpreted as low velocity anomalies associated with dynamic upwelling and active melt production. More extensive sampling throughout BC coupled with analysis of other geochemical indicators of mantle degassing (e.g. CO2) will allow more detailed characterization of the extent and distribution of mantle melts in the region, facilitating assessment of the region's geothermal

  18. Contamination of the Convecting Mantle in Eastern Tethyan 'Subduction Factories'

    NASA Astrophysics Data System (ADS)

    Flower, M. F.; Nguyen, T. H.

    2003-04-01

    As subduction gives way to collision at the end of a Wilson Cycle the associated magmatic activity becomes increasingly enriched in potassium and other large-ion lithophile elements. This is usually attributed to the addition of continental crust-derived material to the convecting mantle wedge. Corresponding depletions in high-field strength elements (Ti and Nb) are more commonly explained in terms of accessory phase buffering or protracted reaction of melts with mantle wallrock. It is increasingly apparent that mantle wedge magmatic sources range from 'fertile' (lherzolitic) to 'refractory' (harzburgitic) although the extent to which this corresponds to the LILE and HFSE variation is unclear. Mantle wedge mass balances clearly hold clues to enrichment-depletion histories of the convecting asthenosphere with respect to both the overriding and subducting plates. With a view to better understanding these effects we have used the MELTS algorithm to calculate hypothetical partial melt compositions as a function of source fertility and H2O content, in the pressure range, 0-1.0 GPa as a basis comparison for natural partial melts. Primitive magmas characterizing the Mariana (western Pacific) and Sunda-Banda (Indonesia) arcs, and the northeastern syntaxis of the India-Asia collision suture (Yunnan) appear to resemble calculated equilibrium melts of refractory (basalt-depleted) peridotite, variably enriched in lithophile and light rare earth elements. These comparisons lead to three observations. 1) HFSE and Fe abundances in primitive MORB, calcalkaline, and boninite magmas, and their respective high-potassium variants are consistent with those implied by phase equilibria associated with partial melting and fractionation, suggesting accessory phases, wall-rock reaction, and slab contamination are probably not important as causes of HFSE depletions. 2) Magmatic sources at convergent and colliding margins are typically refractory (basalt-depleted) compared to those yielding

  19. Toward tsunami early warning system in Indonesia by using rapid rupture durations estimation

    NASA Astrophysics Data System (ADS)

    Madlazim, Physics Department, Faculty Mathematics; Sciences of Surabaya State University (UNESA) Jl. Ketintang, Surabaya 60231, Indonesia

    2012-06-01

    Indonesia has Indonesian Tsunami Early Warning System (Ina-TEWS) since 2008. The Ina-TEWS has used automatic processing on hypocenter; Mwp, Mw (mB) and Mj. If earthquake occurred in Ocean, depth < 70 km and magnitude > 7, then Ina-TEWS announce early warning that the earthquake can generate tsunami. However, the announcement of the Ina-TEWS is still not accuracy. Purposes of this research are to estimate earthquake rupture duration of large Indonesia earthquakes that occurred in Indian Ocean, Java, Timor sea, Banda sea, Arafura sea and Pasific ocean. We analyzed at least 330 vertical seismogram recorded by IRIS-DMC network using a direct procedure for rapid assessment of earthquake tsunami potential using simple measures on P-wave vertical seismograms on the velocity records, and the likelihood that the high-frequency, apparent rupture duration, Tdur. Tdur can be related to the critical parameters rupture length (L), depth (z), and shear modulus (μ) while Tdur may be related to wide (W), slip (D), z or μ. Our analysis shows that the rupture duration has a stronger influence to generate tsunami than Mw and depth. The rupture duration gives more information on tsunami impact, Mo/μ, depth and size than Mw and other currently used discriminants. We show more information which known from the rupture durations. The longer rupture duration, the shallower source of the earthquake. For rupture duration greater than 50 s, the depth less than 50 km, Mw greater than 7, the longer rupture length, because Tdur is proportional L and greater Mo/μ. Because Mo/μ is proportional L. So, with rupture duration information can be known information of the four parameters. We also suggest that tsunami potential is not directly related to the faulting type of source and for events that have rupture duration greater than 50 s, the earthquakes generated tsunami. With available real-time seismogram data, rapid calculation, rupture duration discriminant can be completed within 4-5 min

  20. Gravity field and structure of the Sorong Fault Zone, eastern Indonesia

    NASA Astrophysics Data System (ADS)

    Sardjono

    free-air gravity were observed in south of Mangole (about 13 mGal/km) and west of Obi (about 15 mGal/km) but elsewhere were gentler. Analyses of gravity data along the Sorong Fault Zone in the region of Barggal-Sula Islands controlled in part by geological, reflection seismic and sidescan sonar data, have produced four models which suggest that the crustal structures beneath the zone consist predominantly of attenuated continental fragments, juxtaposed to thick layer of tectonic melange and anomalous oceanic crusts. The continental fragments appear to be severely attenuated and limited in extent in the east but thicker and wider towards the west. The tectonic melange is underlain by deep seated oceanic crust in the Molucca Sea region. The anomalously thin North Banda Sea crust appears to underlie a very thin layer of sediments and to have suffered some degree of arching. The deep seated oceanic crust and the thick layer of tectonic melange are interpreted as the result of the sinking of the lithospheric plate of the Molucca Sea. The descent of this plate may have produced bending forces which may have initiated flexure which propagates through the surrounding region. Depending on the rigidity of the crustal slab, arching and fracturing may have occurred in the crustal rocks. The arching of the oceanic crust of the North Banda Sea may have been one result of this process. The continental fragments of the Banggai-Sula region appear to dip northwards and this may, in addition to the effect of shear tectonics along the Sorong Fault Zone, also be interpreted as the response of the continental fragments to the sinking of the lithospheric plate of the Molucca Sea. In the Obi region, the gravity data suggest that most of the island is underlain by peridotitic and basaltic rocks. Continental crust appears to form the basement in the south and extend offshore south of the island and juxtaposed to oceanic rock. The ultramafic and basic rocks appear to be emplaced on Obi by a high

  1. Elastoplasticidad anisotropa de metales en grandes deformaciones

    NASA Astrophysics Data System (ADS)

    Caminero Torija, Miguel Angel

    El objetivo de este trabajo es el desarrollo de modelos y algoritmos numericos que simulen el comportamiento del material bajo estas condiciones en el contexto de programas de elementos finitos, dando como resultado predicciones mas precisas de los procesos de conformado y deformacion plastica en general. Para lograr este objetivo se han desarrollado diversas tareas destinadas a mejorar las predicciones en tres aspectos fundamentales. El primer aspecto consiste en la mejora de la descripcion del endurecimiento cinematico anisotropo en pequenas deformaciones, lo cual se ha realizado a traves de modelos y algoritmos implicitos de superficies multiples. Ha sido estudiada la consistencia de este tipo de modelos tanto si estan basados en una regla implicita similar a la de Mroz o en la regla de Prager. Ademas se han simulado los ensayos de Lamba y Sidebottom, obteniendo, en contra de la creencia general, muy buenas predicciones con la regla de Prager. Dichos modelos podrian ser extendidos de forma relativamente facil para considerar grandes deformaciones a traves de procedimientos en deformaciones logaritmicas, similares a los desarrollados en esta tesis y detallados a continuacion. El segundo aspecto consiste en la descripcion de la anisotropia elastoplastica inicial. Esto se ha conseguido mediante el desarrollo de modelos y algoritmos para plasticidad anisotropa en grandes deformaciones, bien ignorando la posible anisotropia elastica, bien considerandola simultaneamente con la anisotropia plastica. Para ello ha sido necesario desarrollar primero un nuevo algoritmo de elastoplasticidad anisotropa en pequenas deformaciones consistentemente linealizado y sin despreciar ningun termino, de tal forma que se conserve la convergencia cuadratica de los metodos de Newton. Este algoritmo en pequenas deformaciones ha servido para realizar la correccion plastica de dos algoritmos en grandes deformaciones. El primero de estos algoritmos es una variacion del clasico algoritmo de

  2. Analysis and Synthesis of Leaky-Wave Devices in Planar Technology

    NASA Astrophysics Data System (ADS)

    Martinez Ros, Alejandro Javier

    The work developed along this doctoral thesis has been focused on the analysis and synthesis of microwave devices in planar technology. In particular, several types of devices based on the radiation mechanism of leaky waves have been studied. Typically, the radiation properties in leaky-wave devices are determined by the complex propagation constant of the leaky mode, wherein the phase constant is responsible for the pointing angle and the leakage rate for the intensity of the radiated fields. In this manner, by controlling both amplitude and phase of the leaky mode, an effective control over the device's radiation diagram can be obtained. Moreover, with the purpose of efficiently obtaining the leaky mode's radiation properties as function of the main geometrical parameters of the structure, several modal tools based on the transverse resonance analysis of the structure have been performed. In order to demonstrate this simultaneous control over the complex propagation constant in planar technology, several types of leaky-wave devices, including antennas (LWAs), multiplexors and near-field focusing systems, have been designed and manufactured in the technology of substrate integrated waveguide (SIW). This recently proposed technology, allows the design of devices based on classical waveguide technology with standard manufacturing techniques used for printed circuit board (PCB) designs. In this way, most of the parts that form a communication system can be integrated into a single substrate, thus reducing its cost and providing a more robust and compact device, which has less losses compared to other planar technologies such as the microstrip. El trabajo llevado a cabo durante la realizacion de esta tesis doctoral, se ha centrado en el analisis y sintesis de dispositivos de microondas en tecnologia planar. En concreto, se han estudiado diferentes tipos de dispositivos basados en radiacion por ondas de fuga "leaky waves", en los cuales las propiedades de radiacion

  3. Compliance of nutritional recommendations of Spanish pregnant women according to sociodemographic and lifestyle characteristics: a cohort study.

    PubMed

    Villar-Vidal, María; Amiano, Pilar; Rodríguez-Bernal, Clara; Santa Marina, Loreto; Mozo, Imanol; Vioque, Jesús; Navarrete-Muñoz, Eva María; Romaguera, Dora; Valvi, Damaskini; Fernández Samoano, Ana; Tardón, Adonina; Ibarluzea, Jesús

    2015-04-01

    Objetivo: Estudiar las ingesta dietética y cumplimiento de las recomendaciones nutricionales de una población de mujeres embarazadas, de acuerdo a sus características sociodemográficas y hábitos de vida. Métodos: se trata de un estudio prospectivo basado en datos de la cohorte española INMA (Infancia y Medioambiente). Se han reclutado 2.585 mujeres embarazadas entre los años 2003 y 2008 en cuatro regiones diferentes de España. La ingesta dietética ha sido recogida mediante Cuestionarios de Frecuencia Alimentaria (CFA) y la información antropométrica, sociodemográfica y de estilos de vida a través de cuestionarios generales. La ingesta de grupos de alimentos y de vitaminas A, C y E y carotenoides fueron comparadas con las ingestas dietéticas de referencia de las guías Española y Americana. Resultados: El porcentaje de mujeres embarazadas que no cumplían las recomendaciones de cereales y legumbres (3-4 raciones /día) fue del 70 %, de frutas (2-3 raciones /día) el 39,2%, de verduras (2-4 raciones /día) fue del 47,3% y de lácteos (3-4 raciones /día) el 51,6%. La ingesta de frutas y verduras fue mayor en mujeres extranjeras y aumento con la edad, con el nivel de estudios y en mujeres con mayor actividad física (p.

  4. [Sarcopenic obesity and physical fitness in octogenarians: the multi-center EXERNET Project].

    PubMed

    Muñoz-Arribas, Alberto; Mata, Esmeralda; Pedrero-Chamizo, Raquel; Espino, Luis; Gusi, Narcis; Villa, Gerardo; Gonzalez-Gross, Marcela; Casajús, José Antonio; Ara, Ignacio; Gómez-Cabello, Alba

    2013-11-01

    Objetivo: El objetivo de este estudio fue analizar la utilidad de diferentes test de condición física para detectar el riesgo de sufrir obesidad sarcopénica (OS) en octogenarios. Métodos: 306 sujetos (76 hombres, 230 mujeres) con una media de edad de 82,5±2,3 años, del total de la muestra del Proyecto Multi-céntrico EXERNET cumplieron con los criterios de inclusión. La composición corporal se evaluó en todos los sujetos mediante impedancia bioeléctrica. Se crearon 4 grupos basados en el porcentaje de masa grasa y masa muscular: 1) normal, 2) elevada masa grasa, 3) baja masa muscular y 4) OS. La condición física fue evaluada utilizando 8 test diferentes adaptados de las baterías “Senior Fitness Test” y “Eurofit” (batería EXERNET). La probabilidad de padecer OS en función del nivel de condición física se estudió mediante regresión logística. Resultados: Entre las pruebas de condición física estudiadas, los test que mejor predecían el riesgo de sufrir OS fueron la falta de fuerza de piernas, fuerza de brazos, agilidad, velocidad y equilibrio en hombres; 95% CI [(0,606-0,957); (0,496-0,882); (1,116-3,636); (1,060-1,825); (0,913-1,002); todos p.

  5. [Psychopedagogical intervention in attention deficit hyperactivity disorder].

    PubMed

    Abad-Mas, Luis; Ruiz-Andrés, Rosalía; Moreno-Madrid, Francisca; Herrero, Raquel; Suay, Enrique

    2013-09-01

    Introduccion. Los niños con trastorno por deficit de atencion/hiperactividad (TDAH) presentan alteraciones en los mecanismos atencionales y en los procesos de control inhibitorio (impulsividad e hiperactividad), que afectan de distinta manera a su rendimiento academico, socioemocional y conductual, por lo que es fundamental la consideracion de estrategias de intervencion en el ambito psicopedagogico que puedan incidir de forma favorable en el curso evolutivo de los afectados. Objetivo. Revisar las bases psicopedagogicas en la intervencion sobre el TDAH, considerando la relacion de la anatomia funcional con la sintomatologia clinica y los correspondientes programas de intervencion. Desarrollo. Se destacan los tres sindromes preferentes: orbitofrontal, dorsolateral y en el cingulo a nivel medial. Las fases de la intervencion psicopedagogica deben abarcar tanto al niño como a la familia y el colegio. El entrenamiento neurocognitivo se centra en el niño, basado en programas de entrenamiento de las funciones ejecutivas y en las actuaciones sobre el ambito academico, conductual y socioafectivo. Los programas de modificacion de conducta son complementarios y en muchas ocasiones mejoran el comportamiento comprometido en los niños con TDAH. Las orientaciones psicopedagogicas en la escuela deben considerarse necesarias para una intervencion eficaz en el entorno academico. Conclusiones. La intervencion psicopedagogica de los niños con TDAH debe contemplar la individualizacion del tratamiento dentro de una metodologia multidisciplinar, teniendo en cuenta todos los contextos en los que se desarrolla el niño, su rendimiento cognitivo y las intervenciones farmacologicas apropiadas en cada caso.

  6. Prevalence and determinants of the dual burden of malnutrition at the household level in Puna and Quebrada of Humahuaca, Jujuy, Argentina.

    PubMed

    Bassete, M N; Romaguera, D; Giménez, M A; Lobo, M O; Samman, N C

    2014-02-01

    El objetivo del presente estudio fue identificar los hogares en los que coexisten el sobrepeso y bajo peso (doble carga de malnutrición) y explorar los factores que podrían contribuir a la doble carga de malnutrición en los hogares de esta población. Después de aplicar los criterios de exclusión, se incluyeron 136 hogares. Las madres fueron clasificadas como de peso normal o con sobrepeso/ obesidad basado en puntos de corte del índice de masa corporal (IMC), los niños y adolescentes fueron clasificados según z–score de la talla para la edad, si tenían o no retraso en el crecimiento (Stunted). Los hogares con una madre obesa y niños o adolescentes con retraso en el crecimiento fueron clasificados como hogares de doble carga. La prevalencia de hogares con doble carga fue del 12 %. En comparación con los otros hogares, en los hogares con doble carga de malnutrición habitan un mayor número de personas en la casa, y el nivel de educación del jefe de familia fue menor. Las personas que viven en hogares de doble carga mostraron ingestas de energía global más bajas y eran más propensos a tener una ingesta insuficiente de calcio y hierro. Una de las principales causas de la doble carga de malnutrición observada en esta comunidad podría ser la transición nutricional. Los resultados presentados aquí indican la necesidad de considerar a los programas que se centran en un solo tipo de problema nutricional y que en realidad podrían exacerbar el otro.

  7. [Psychomotor skills assessment in basic procedures of laparoscopic surgery in undergraduate medical students at the School of Medicine of the University of Colima].

    PubMed

    Prieto-Díaz-Chávez, Emilio; Medina-Chávez, José Luís; Martínez-Lira, Rafael; Millán-Guerrero, Rebeca; Vázquez-Jiménez, Clemente; Trujillo-Hernández, Benjamín

    2014-01-01

    Antecedentes: la educación basada en competencias señala que el estudiante debe dominar tres rubros: saber, saber hacer y ser. El primero se refiere al conjunto de conocimientos teórico-prácticos, el segundo a las habilidades psicomotrices y el tercero al comportamiento profesional. El estudiante de Medicina adquiere las primeras destrezas en cirugía laparoscópica a través de modelos animales y simuladores virtuales. Sin embargo, no hemos evaluado la trascendencia de esta capacitación. Objetivo: evaluar en alumnos de pregrado las destrezas en cirugía laparoscópica obtenidas después de un curso con un simulador virtual. Material y métodos: estudio de investigación educativa, analíticocomparativo efectuado como parte de las actividades del programa de Aprendizaje Basado en Problemas de la asignatura de Educación y Técnica Quirúrgica de la Facultad de Medicina de la Universidad de Colima. Resultados: todos los participantes alcanzaron en el simulador un mejor nivel durante la tarea 1 después de tres repeticiones (p= 0.001). En la evaluación de la calificación final de los alumnos se observaron diferencias significativas en las medias que fueron más bajas durante la evaluación inicial (8.60 ± 0.76) en comparación con la final (8.96 ± 0.58) p= 0.001. Conclusiones: la adquisición de habilidades en el simulador es más prolongada y al final es superior a la adquisición de habilidades basada en el método tradicional; demuestra que conduce a la adquisición de competencias que favorecen la transferencia de habilidades al entorno quirúrgico.

  8. [Bariatric surgery in adults: variables that facilitate and hinder weight loss from pacients perspective].

    PubMed

    Lecaros-Bravo, Javiera; Cruzat-Mandich, Claudia; Díaz-Castrillón, Fernanda; Moore-Infante, Catalina

    2015-04-01

    Introducción: La obesidad se ha convertido en un problema de salud pública a nivel mundial. Asociado a esto, las cirugías bariátricas han ido en progresivo aumento, dada su efectividad en la baja de peso a corto plazo. Sin embargo, se ha visto que existe un alto porcentaje de reganancia de peso a partir del tercer año post cirugía y existen pocos estudios de seguimiento de estos pacientes. Objetivos: Describir los facilitadores y obstaculizadores de la pérdida de peso, desde la perspectiva de adultos que han sido sometidos a cirugía bariátrica. Métodos: Se utilizó un enfoque cualitativo, descriptivo, basado en la Teoría Fundamentada. Se realizaron entrevistas en profundidad y los datos se analizaron a través de codificación abierta. La muestra estuvo compuesta por 8 mujeres y 3 hombres adultos, intervenidos en clínicas privadas. Resultados: Se generaron cinco categorías de análisis: (1) variables que favorecen la pérdida de peso post cirugía bariátrica, (2) variables que dificultan la pérdida y mantención de peso post cirugía, (3) evaluación de los resultados de la cirugía bariátrica, (4) problematización de la obesidad, y (5) relación con la comida. Discusión: Los principales hallazgos indican que el fracaso y el éxito en la pérdida de peso post cirugía se encuentra asociado a la posibilidad de tener una red de apoyo emocional y social, así como a la posibilidad de comprender y modificar el rol de la comida como mecanismo de regulación emocional.

  9. [Antimicrobial resistance trends in pathogens isolated from nosocomial infections].

    PubMed

    Rincón-León, Héctor A; Navarro-Fuentes, Karla R

    2016-01-01

    Introducción: el tratamiento de las infecciones nosocomiales se dificulta por la tendencia al incremento de la resistencia a antimicrobianos de los gérmenes que las causan. El objetivo fue evaluar las tendencias en la resistencia de las bacterias de aislados de infección nosocomial. Métodos: estudio retrospectivo de 2009 a 2012 en un hospital de tercer nivel en Chiapas. Resultados: fueron obtenidos 1300 gérmenes, 62.3 % bacterias Gram negativas, 22.8 % Gram positivas y 14.9 % levaduras; Pseudomonas aeruginosa pasó del 47.1 al 60.5 % de resistencia a imipenem; Escherichia coli mostró un aumento en la resistencia a aztreonam, cefepime y ceftazidima; Acitenobacter baumannii incrementó su resistencia a amikacina, cefepime, ceftazidima y ciprofloxacino; Klebsiella pneumoniae disminuyó su resistencia a amikacina y piperacilina/tazobactam; la resistencia a vancomicina fue del 3.6 al 25.5 %. Conclusiones: predominaron los gérmenes Gram negativos y mostraron tendencias al incremento en la resistencia antimicrobiana. Hubo un aumento proporcional de la incidencia de infección por E. coli, Candida tropicalis y Staphylococcus haemolyticus. Es indispensable contar con planes y programas para el uso racional y basado en evidencia de antimicrobianos, así como la difusión y el apego a las guías de práctica clínica y la implementación de programas novedosos para la vigilancia y el control de las infecciones hospitalarias, las técnicas de aislamiento y los cuidados generales.

  10. Tratamiento Quirúrgico de los Meningiomas del Foramen Óptico, Técnicay Resultados de una Serie de 18 Pacientes

    PubMed Central

    Goldschmidt, Ezequiel; Ajler, Pablo; Campero, Álvaro; Landriel, Federico; Sposito, Maximiliano; Carrizo, Antonio

    2014-01-01

    Introducción: los meningiomas del foramen óptico producen un rápido deterioro de la función visual aún cuando su tamaño es pequeño, por eso su diagnóstico y manejo difiere del resto de los meningiomas clinoideos. El propósito de este estudio es presentar la técnica y los resultados de nuestro manejo quirúrgico de meningiomas foraminales (MF). Pacientes y Métodos: se llevó a cabo una revisión de las historias clínicas de 47 pacientes con meningiomas primarios intraorbitarios. Se realizaron 52 cirugías en los pacientes con MF. Se empleó una craneotomía fronto-orbitaria, seguida de una descompresión extradural del canal óptico, resección del componente intraorbitario y exploración intradural del nervio óptico. Resultados: de los 12 pacientes con MF que presentaban la visión conservada, la agudeza visual fue preservada en 7 casos, mejoró en 2, y empeoró en 3. En 18 pacientes, el principal síntoma fue exoftalmos y en 35 pacientes ceguera unilateral. Ocurrieron 6 recurrencias, 2 a 10 años después de la resección quirúrgica. Cinco de ellos fueron reoperados. Se indicó radioterapia después de la recurrencia en 3 pacientes. Conclusión: el manejo de los MF continúa siendo controvertido y frecuentemente se propone un tratamiento conservador. Basados en nuestros hallazgos de frecuente extensión intracraneal, proponemos realizar una resección total o subtotal del tumor, preservando el nervio óptico en pacientes con visión prequirúrgica conservada. PMID:25165616

  11. [Cognitive and emotional alterations in chronic insomnia].

    PubMed

    Medrano-Martínez, Pablo; Ramos-Platón, María J

    2016-02-16

    Introduccion. Las alteraciones cognitivas y emocionales asociadas al insomnio cronico son poco conocidas. Desarrollo. Tras revisar la etiologia y fisiopatologia del insomnio cronico, considerando la vulnerabilidad a este y su heredabilidad, se describe el estado actual de conocimientos acerca de los deficits cognitivos y las alteraciones emocionales observados en el insomnio cronico. Conclusiones. La mayoria de los modelos etiologicos incluye factores que predisponen al insomnio, que lo precipitan y que lo mantienen. Los factores predisponentes pueden ser de tipo biologico o psicosocial. Un factor predisponente que desempeña un importante papel es la vulnerabilidad al insomnio, que se relaciona con un modo no adaptativo de afrontar el estres (centrado en la emocion en vez de en el problema) y la internalizacion de las emociones negativas, lo cual favorece un estado de hiperactivacion fisiologica, cognitiva y emocional que altera el sueño y puede desembocar en insomnio. Esta vulnerabilidad es en gran parte hereditaria. Se han descrito dos fenotipos, basados en la duracion objetiva del sueño, que difieren en la gravedad del trastorno. Los insomnes con duracion objetiva del sueño menor de seis horas presentan deficits cognitivos significativos. Estos se manifiestan en tareas que requieren gran cantidad de recursos cognitivos, tareas de atencion complejas, cambio de foco de atencion, proceso de consolidacion de la memoria durante el sueño y memoria operativa. Estos datos sugieren la existencia de una disfuncion prefrontal. Se da una alta comorbilidad entre insomnio y ansiedad-depresion. La ansiedad-depresion provocada por la internalizacion de las emociones predispone al insomnio, y este, a su vez, intensifica la depresion.

  12. [Energy expenditure prediction equations in burn patients; bibliographic review].

    PubMed

    Núñez-Villaveirán, Teresa; Sánchez, Manuel; Millán, Pablo; Martínez-Méndez, Jose Ramón; Iglesias, Carmen; Casado-Pérez, César; García-de-Lorenzo, Abelardo

    2014-06-01

    Introducción: La valoración de las necesidades calóricas del paciente quemado se ha basado en la medición del gasto energético en reposo (GER) mediante calorimetría indirecta, no siempre disponible en las unidades de quemados, o en su estimación mediante el uso de ecuaciones predictivas. Objetivos: analizar la historia y estado del arte del uso de las ecuaciones predictivas de GER en el paciente quemado crítico, y determinar su validez. Métodos: revisión bibliográfica de estudios y revisiones en español y en inglés entre 1989 y 2013. Resultados: Se han diseñado más de 190 ecuaciones para estimar el gasto energético que pueden ser imprecisas por estar basadas en mediciones con metodología heterogénea y en grupos heterogéneos. Describimos los distintos parámetros que aplican las distintas fórmulas predictivas (factores de estrés y de actividad, superficie corporal quemada, tiempo desde la lesión, masa corporal magra), la influencia de la edad en el cálculo de las necesidades calóricas y las fórmulas más utilizadas en el momento actual. También describimos los artículos que evalúan exactitud de las fórmulas cuando se comparan con mediciones mediante calorimetría indirecta. Conclusiones: Las ecuaciones predictivas son poco precisas en general en el paciente quemado. Hasta que se desarrollen ecuaciones predictivas más precisas, recomendamos calcular los requerimientos nutricionales de los pacientes quemados basándose en la medición del gasto energético por calorimetría indirecta.

  13. [Carcinosarcoma of the breast a rare entity with fatal prognosis. One case report].

    PubMed

    Villalón-López, José Sebastián; Souto-del Bosque, Rosalía; Alonso-Briones, Marco Vinicio; Trujillo-de Anda, Ana Patricia

    2013-01-01

    Antecedentes: los carcinomas metaplásticos de la glándula mamaria son un grupo heterogéneo de neoplasias con pobre pronóstico en comparación con el carcinoma ductal invasor. Corresponden a menos de 1% del total de las neoplasias malignas de la glándula mamaria. Casi siempre se manifiestan como tumores de alto grado con menor índice de metástasis ganglionares y menor expresión de receptores de estrógeno y progesterona, Her2 y mayor expresión de Her1 y Ki-67. Caso clínico: se reporta el caso de una mujer de 52 años de edad con carcinosarcoma mamario que se manifiesta con un tumor mamario izquierdo, fungado, ulcerado, polipoide, de 18 cm de diámetro, con metástasis ganglionares al momento del diagnóstico. Recibió tratamiento multimodal con quimioterapia neoadyuvante seguida de mastectomía y quimioterapia complementaria; evolucionó con metástasis pulmonares y recurrencia local masiva. Falleció por complicaciones derivadas de la enfermedad.Conclusiones: los carcinomas metaplásticos de la glándula mamaria son padecimientos sumamente raros. Debido a la naturaleza de la enfermedad y su forma de presentación el pronóstico es pobre. Existen varios subtipos histológicos basados en estudios de hematoxilina y eosina o tinciones de inmunohistoquímica. El tratamiento debe ser multimodal (cirugía, radioterapia y quimioterapia) para obtener mejores resultados.

  14. [Characterisation of the paediatric population of Costa Rica with tuberous sclerosis and a description of the behaviour of the associated epilepsy].

    PubMed

    Ulate-Campos, Adriana; Benavides-Lara, Adriana; Hernández, Laura

    2013-12-01

    Introduccion. La esclerosis tuberosa (ET) es una patologia autosomica dominante debida a un trastorno en la diferenciacion y proliferacion celular que produce hamartomas en diferentes organos. Afecta de forma variable el sistema nervioso central, los riñones, la piel y otros organos. No existen estudios de su prevalencia ni de su comportamiento en la poblacion pediatrica de Costa Rica. Objetivos. Caracterizar la poblacion pediatrica costarricense con ET y describir el comportamiento de su epilepsia. Pacientes y metodos. Estudio de prevalencias basado en la revision de expedientes clinicos de todos los pacientes menores de 18 años con diagnostico de ET seguidos en el Hospital Nacional de Niños durante el periodo 2000-2010. Resultados. Durante el periodo de estudio se incluyeron 37 pacientes para una prevalencia de 3,09 por 100.000 nacidos vivos (intervalo de confianza al 95% = 1,88-4,31). No se presentaron diferencias significativas por sexo. La mediana de edad al diagnostico fue de 14 meses. Los criterios mayores mas frecuentes fueron manchas hipomelanoticas (97,3%), angiofibromas faciales (56%) y tuberomas corticales (54,1%). Treinta y cinco pacientes presentaron convulsiones (95%). Los tratamientos que lograron reduccion de al menos un 50% de las crisis convulsivas fueron la vigabatrina (16,2%) y la cirugia de epilepsia (16,2%). Conclusiones. En todo paciente con epilepsia debe realizarse una valoracion minuciosa de la piel, ya que las lesiones en la piel son un hallazgo muy frecuente en la ET. La epilepsia en la ET es farmacorresistente en un elevado numero de pacientes y la vigabatrina debe valorarse como tratamiento farmacologico de primera linea.

  15. Persistence to single-tablet regimen versus less-drug regimen in treatment experienced HIV-infected patients on antiretroviral therapy.

    PubMed

    Jiménez-Galán, Rocio; Cantudo Cuenca, Maria-Rosa; Robustillo-Cortés, María Aguas; Borrego Izquierdo, Y; Almeida-Gonzalez, Carmen Victoria; Morillo-Verdugo, Ramón

    2016-06-01

    Objetivos: Analizar y comparar la persistencia entre las estrategias basadas en Single-Tablet Regimen (STR) y Less Drug Regimen (LDR) en pacientes VIH+. El objetivo secundario del estudio fue determinar factores predictores de persistencia. Material y métodos: Estudio observacional retrospectivo que incluyo los siguientes criterios: pacientes VIH+ con tratamiento antirretroviral (TAR) con un regimen basado en STR o LDR. Se recogieron variables demograficas, factores de riesgo de adquisicion, consumo de drogas, presencia de algun trastorno psiquiatrico y coinfeccion por el virus de la hepatitis B o C. Para comparar la persistencia entre ambas estrategias se realizo un analisis de supervivencia de Kaplan-Meir y se aplico el metodo de log-rank. Se realizo un analisis de regresion de Cox para identificar los factores predictores de persistencia. Resultados: Se incluyeron 244 pacientes, 176 con STR y 68 con LDR. El 34,1% (n = 60) de los pacientes que recibieron un regimen STR abandonaron y en el LDR el 19,1% (n = 13). Los efectos adversos fueron la principal causa de abandono del tratamiento en los pacientes que recibieron STR y el fallo virologico en el regimen LDR. La persistencia de las estrategias STR y LDR fue similar, no encontrandose diferencias estadisticamente significativas entre ambas. El consumo de drogas fue el unico factor predictivo asociado con una menor persistencia (HR = 2,59; p = 0,005). Conclusiones: La persistencia entre los regimenes STR y LDR fue similar, no detectandose diferencias significativas entre ambos. El consumo de drogas fue el unico factor independiente asociado con una menor persistencia del tratamiento antirretroviral.

  16. Detección automática de NEOs en imágenes CCD utilizando la transformada de Hough

    NASA Astrophysics Data System (ADS)

    Ruétalo, M.; Tancredi, G.

    El interés y la dedicación por los objetos que se acercan a la órbita de la Tierra (NEOs) ha aumentado considerablemente en los últimos años, tanto que se han iniciado varias campañas de búsqueda sistemática para aumentar la población identificada de éstos. El uso de placas fotográficas e identificación visual está siendo sustituído, progresivamente, por el uso de cámaras CCD y paquetes de detección automática de los objetos en las imágenes digitales. Una parte muy importante para la implementación exitosa de un programa automatizado de detección de este tipo es el desarrollo de algoritmos capaces de identificar objetos de baja relación señal-ruido y con requerimientos computacionales no elevados. En el presente trabajo proponemos la utilización de la transformada de Hough (utilizada en algunas áreas de visión artificial) para detectar automáticamente trazas, aproximadamente rectilíneas y de baja relación señal-ruido, en imágenes CCD. Desarrollamos una primera implementación de un algoritmo basado en ésta y lo probamos con una serie de imágenes reales conteniendo trazas con picos de señales de entre ~1 σ y ~3 σ por encima del nivel del ruido de fondo. El algoritmo detecta, sin inconvenientes, la mayoría de los casos y en tiempos razonablemente adecuados.

  17. How Do Management Fees Affect Retirement Wealth under Mexico's Personal Retirement Accounts System?

    PubMed Central

    Aguila, Emma; Hurd, Michael D.; Rohwedder, Susann

    2014-01-01

    In 1997, Mexico transformed its pay-as-you-go social security system to a fully funded system with personal retirement accounts, including management fees. This article examines changes in retirement wealth resulting from this new system. It shows that management fees have drained a significant proportion of individuals' retirement wealth and have increased the number of persons claiming a government-subsidized minimum pension, particularly from the time the system was introduced in 1997 until adjustment to management fees in 2008. Since 2008, retirement wealth accumulation has been similar to that of the previous system. En 1997, México transformó su sistema de pensiones basado en cotizaciones individuales a uno de ahorro para el retiro que incluyen cuotas por la administración de las cuentas. El presente estudio examina los cambios en el monto de las pensiones como resultado de la introducción del nuevo sistema. Los resultados muestran que las cuotas de administración han drenado una proporción significativa del ahorro para el retiro de los individuos por lo que ha aumentado el número de personas que solicita la pensión mínima garantizada subsidiada por el gobierno desde que se introdujo el sistema en 1997 hasta que se hicieron ajustes en las cuotas de administración de los fondos de pensiones en 2008. A partir de 2008, la acumulación del ahorro para el retiro ha sido similar que la del sistema anterior. PMID:25601893

  18. The effectiveness of intervention programs in the prevention and control of obesity in infants: a systematic review.

    PubMed

    Pitangueira, Jacqueline Costa Dias; Rodrigues Silva, Luciana; Costa, Priscila Ribas de Farias

    2015-04-01

    Objetivo: Este trabajo pretende realizar una revisión de literatura para evaluar la efectividad de programas de intervención en la prevención y en el control del exceso de peso infantil y hacer el mapeamiento de los sitios donde los estudios fueron hechos. Métodos: Estudio de revisión sistemática utilizando las bases de datos de PUBMED/MEDLINE y LILACS para rastrear la literatura publicada sobre programas de intervenciones para prevención y control de exceso de peso entre el período de enero de 2004 a octubre de 2013. La búsqueda inicial fue realizada utilizando los términos “body mass index” and “Intervention” and “children” or “adolescent” y fueron seleccionados apenas los artículos publicados en Inglés, español y portugués. Resultados: se observó que intervenciones pautadas unicamente en el aconsejamiento presentaron resultados modestos para identificar alteraciones en los indicadores antropométricos de niños y adolescentes a lo largo del tiempo, aunque parezcan ser efectivos para realizar cambios positivos en los hábitos alimentares de esa población. Entre los estudios identificados, 77.8% fueron realizados en países con renta alta, 22.2% en los países con renta media-alta y no hay estudios de intervención en países con renta media-baja y baja. Conclusión: Los programas de intervenciones basados solamente en el aconsejamiento son efectivos para promover cambios en la calidad alimentar, pero presentan insignificantes resultados en la alteración de los parámetros antropométricos de niños y adolescentes.

  19. [Cost-effectiveness analysis of etanercept compared with other biologic therapies in the treatment of rheumatoid arthritis].

    PubMed

    Salinas-Escudero, Guillermo; Vargas-Valencia, Juan; García-García, Erika Gabriela; Munciño-Ortega, Emilio; Galindo-Suárez, Rosa María

    2013-01-01

    Objetivo: analizar la relación costo-efectividad del etanercept en comparación con otras terapias biológicas para tratar la artritis reumatoide moderada o severa en pacientes con falla previa a fármacos antirreumáticos modificadores de la enfermedad. Métodos: se empleó un modelo farmacoeconómico basado en el análisis de decisiones para valorar la evolución clínica con etanercept, infliximab, adalimumab o tocilizumab para tratar artritis reumatoide moderada o severa. Los parámetros de efectividad fueron las tasas de mejoría igual o superior a 20 % (ACR 20) y de mejoría igual o superior a 70 % (ACR 70). Resultados: etanercept tuvo la mayor efectividad terapéutica: en 79.7 % de los pacientes se observó una ACR 20 y en 31.4 %, una ACR 70. También tuvo el menor costo asociado ($149 629.1 por paciente) y fue más costo-efectiva ($187 740.4 por éxito clínico para obtener ACR 20 y $476 525.8 por éxito clínico para obtener ACR 70) que las demás terapias biológicas. Conclusiones: el etanercept fue el fármaco más efectivo y menos costoso, por lo que resulta la opción terapéutica más eficiente, desde el punto de vista de la relación costo-efectividad media y en términos incrementales para el tratamiento de la artritis reumatoide.

  20. Desarrollo de la Escala sobre el Estigma Relacionado con el VIH/SIDA para Profesionales de la Salud mediante el uso de métodos mixtos123

    PubMed Central

    Varas-Díaz, Nelson; Neilands, Torsten B.; Guilamo-Ramos, Vincent; Cintrón Bou, Francheska N.

    2009-01-01

    El estigma relacionado con el VIH/SIDA continúa siendo un obstáculo para la prevención primaria y secundaria del VIH. Las consecuencias para las personas que viven con la enfermedad han sido muy documentadas y continúan siendo una gran preocupación para las personas que proveen servicios de salud y para aquellas que investigan el tema. Estas consecuencias son preocupantes cuando el estigma emana de profesionales de la salud porque se puede limitar el acceso a los servicios. Uno de los principales obstáculos para la investigación del estigma relacionado con el VIH en Puerto Rico es la falta de instrumentos cuantitativos para evaluar las manifestaciones del estigma entre profesionales de la salud. El objetivo principal de este estudio fue desarrollar y probar las propiedades psicométricas de una escala sobre el estigma relacionado con el VIH/SIDA culturalmente apropiada para personas que proveen servicios de salud puertorriqueñas y desarrollar una versión corta de la escala que pudiera usarse en escenarios clínicos con tiempo limitado. El instrumento desarrollado estuvo basado en evidencia cualitativa recopilada entre profesionales y estudiantes de profesiones de la salud puertorriqueños/as (n=80) y administrado a una muestra de 421 profesionales de la salud en adiestramiento. La escala contenía 12 dimensiones del estigma relacionado con el VIH/SIDA. El análisis cuantitativo corroboró 11 de ellas, teniendo como resultado un instrumento con validez y confiabilidad satisfactoria. Estas dimensiones, a su vez, fueron subcomponentes de un factor de estigma general superior. PMID:20333258

  1. [Perceptions of adolescents Jalisco campaign on breast cancer].

    PubMed

    Tapia-Curiel, Amparo; Nuño-Gutiérrez, Bertha Lidia; Flores-Padilla, Luis; Villaseñor-Farías, Martha; López-López, José Luis; Covarrubias-Bermúdez, María de los Ángeles

    2015-01-01

    Introducción: las campañas sobre cáncer de mama (CaMa) y las estrategias de sensibilización tienen limitada evidencia sobre su efectividad en jóvenes. La percepción referente conductual que da cuenta cómo individuos seleccionan, organizan e interpretan información. Este estudio muestra la percepción de adolescentes jaliscienses sobre campañas de CaMa. Métodos: estudio cualitativo, exploratorio, transversal, basado en las teorías construccionista y asociacionista de la percepción. Entrevista con consentimiento informado a 13 grupos focales, 129 hombres y mujeres de 12 a 19 años, escolarizados, residentes de 6 regiones de Jalisco, muestreo: técnica bola de nieve. Entrevistas transcritas y procesadas en Atlas Ti 4.1, análisis por codificación abierta. Resultados: se identificaron 10 campañas, la percepción de ellas mostró 3 procesos: 1) Selección: permeada por elementos del diseño de las campañas; 2) Organización: influenciada por significados pre estructurados sobre el color rosa, alcances y limitaciones de las campañas, y 3) Interpretación: mostró juicios referentes a visibilización del CaMa, accesibilidad al conocimiento y recursos, permeabilización de pautas y códigos culturales positivos y no cobertura a expectativas. Conclusiones: se evidenció alta sensibilización de adolescentes ante el CaMa y amplia necesidad de información y servicios. Recomendamos generar estrategias en educación formal en la adolescencia sobre salud mamaria.

  2. Agregación de para-H2 en chorros supersónicos: del dímero al sólido

    NASA Astrophysics Data System (ADS)

    María Fernández, José

    En este trabajo se mostrarán los estudios de expansiones supersónicas de para-H2 desde toberas criogénicas, realizados en el laboratorio de Fluidodinámica Molecular del IEM. Hemos registrado los espectros Raman de dichas expansiones en el intervalo de frecuencias de 4145 a 4162 cm-1, próximo a la línea Q(0) del monómero no rotante H2, a 4161.18 cm-1. En el espectro Raman, además de la línea Q(0) del monómero, se observan unos picos débiles, que, por su comportamiento con la temperatura de la tobera y la distancia a la misma, asignamos a la transición homóloga en agregados de p-H2. Dependiendo de las condiciones, se observan agregados pequeños (de 2 a 13 moléculas de p-H2), agregados medios y masivos, y se llega incluso al líquido y al sólido. Las asignaciones se apoyan en un modelo sencillo, basado en la perturbación, debida al potencial intermolecular, de los estados vibracionales v=0 y v=1 en los agregados de p-H2. Se mostrarán detalles de la instalación experimental, ejemplos de los espectros obtenidos en diversas condiciones, y detalles de la interpretación cuantitativa.

  3. [Early detection and stability of diagnosis in autism spectrum disorders].

    PubMed

    Canal-Bedia, R; Magan-Maganto, M; Bejarano-Martin, A; De Pablos-De la Morena, A; Bueno-Carrera, G; Manso-De Dios, S; Martin-Cilleros, M V

    2016-01-01

    Introduccion. La intervencion temprana en los niños con un trastorno del espectro autista (TEA) depende de una deteccion precoz y fiable. Aunque de manera general se habla de un diagnostico estable, se ha evidenciado la necesidad de profundizar mas en los factores que influyen en dicha estabilidad. Pacientes y metodos. Los participantes de la muestra fueron 142 menores con TEA (118 varones y 24 mujeres), con una mediana de 33 meses y un recorrido intercuartilico de 12 en la primera evaluacion, y con una mediana de 47 meses y un recorrido intercuartilico de 29 en el seguimiento. Los diagnosticos se realizaron con las siguientes pruebas: escala Merrill-Palmer revisada, escala de Leiter revisada, escala de inteligencia de Wechsler para preescolar y primaria III y escala de inteligencia de Wechsler para niños revisada y IV; ademas de la escala Vineland y la escala de observacion diagnostica del autismo generica (ADOS-G), basandose el diagnostico clinico en los criterios diagnosticos del Manual diagnostico y estadistico de los trastornos mentales, cuarta edicion, texto revisado (DSM-IV-TR), y quinta edicion (DSM-5). Para la evaluacion de la estabilidad diagnostica, se realizaron tablas de contingencia para las valoraciones del diagnostico en funcion del juicio clinico y los resultados de la ADOS-G. Resultados. El diagnostico clinico basado en los criterios del DSM-IV-TR, el DSM-5 y el juicio clinico se mantiene estable a traves del tiempo en un 96% de los casos. Si se valora la estabilidad diagnostica teniendo en cuenta los resultados del ADOS-G (n = 30), el 87% de los casos mantiene el diagnostico. El ANOVA muestra diferencias estadisticamente significativas para las medidas del factor intrasujeto del cociente intelectual y la edad social global, pero no para el diagnostico. Conclusiones. La estabilidad diagnostica se beneficia de un uso informado del criterio clinico y de la participacion de un equipo multidisciplinar.

  4. Creation and design of a test for the Evaluation of Upper Limb Apraxia (EULA) based on a cognitive model: a pilot study.

    PubMed

    Perez-Marmol, José Manuel; Lopez-Alcalde, Samuel; Carnero-Pardo, Cristóbal; Canadas-De la Fuente, Guillermo A; Peralta-Ramirez, M Isabel; Garcia-Rios, M Carmen

    2015-01-16

    Introduccion. La apraxia es un trastorno neurologico caracterizado por la dificultad en la ejecucion de habilidades gestuales aprendidas a pesar de tener preservados los sistemas motores y sensoriales, la coordinacion y la comprension, asi como de una adecuada colaboracion. Actualmente, existen pocas herramientas validadas que evaluen este sindrome de manera global. En el presente estudio, se ha creado y diseñado un test para la evaluacion de la apraxia de los miembros superiores (EULA), basado en modelos teoricos. Sujetos y metodos. Se selecciono una poblacion de 57 pacientes con quejas subjetivas de deterioro cognitivo y 39 personas sin quejas ni deterioro cognitivo, a las cuales se les administro el test EULA, entre otros tests. Se realizo un analisis factorial de componentes principales y un calculo tanto de la fiabilidad como de la validez de dicho instrumento. Resultados. El analisis factorial agrupo en nueve factores todos los items de la prueba, con una varianza total explicada del 69,91%. El test ha mostrado una alta fiabilidad, con un alfa de Cronbach de 0,929 y un coeficiente de Guttman de 0,870 con el metodo de las dos mitades. El test tambien mostro tener una adecuada validez de constructo, al existir correlacion significativa entre seis factores del test y dos subtests de apraxia. Conclusiones. El test EULA, surgido de las propuestas de evaluacion a nivel teorico desarrolladas por diferentes autores, muestra una puntuacion superior en personas sanas respecto a personas con manifestaciones subjetivas de deterioro cognitivo, ademas de tener una alta fiabilidad y validez de constructo.

  5. NORMATIVE VALUES OF EQ-5D-5L FOR DIABETES PATIENTS FROM SPAIN.

    PubMed

    Collado Mateo, Daniel; García Gordillo, Miguel A; Olivares, Pedro R; Adsuar, José C

    2015-10-01

    Introducción: la diabetes es una enfermedad metabólica que puede conllevar una reducción de la calidad de vida relacionada con la salud. El EQ-5D es un cuestionario genérico de calidad de vida relacionada con la salud basado en preferencias sociales. Este cuestionario ha sido muy utilizado en pacientes con diabetes. Objetivo: el objetivo del presente artículo es informar sobre los valores normativos del cuestionario EQ-5D-5L en personas españolas con diabetes. Métodos: se utilizaron datos de la Encuesta Española de Salud (2011/2012). Un total de 1.857 personas con diabetes participaron en la encuesta. La puntuación del EQ-5D-5L se ha reflejado en función del sexo, región (incluyendo las 17 comunidades autónomas y las 2 ciudades autónomas de España), y 8 grupos de edad. Resultados: la media del índice de utilidad para toda la muestra fue de 0,742. Esta fue mejor para hombres (0,826) que para mujeres (0,673). Resultados similares se observaron en la Escala Visual Analógica. El efecto techo fue mucho mayor en hombres (44,83%) que en mujeres (24,41%). Conclusiones: el presente estudio recoge datos normativos representativos del EQ-5D-5L en España de personas con diabetes.

  6. The "SABEIS" Project: Warning systems based on earthquake and tsunamis-induced ionospheric effects.

    NASA Astrophysics Data System (ADS)

    Rodriguez-Bouza, Marta; Sánchez-Dulcet, Francisco; Herraiz, Miguel; Rodríguez-Caderot, Gracia; Altadill, David; Blanch, Estefania; Santoyo, Miguel Angel

    2016-04-01

    The study of a possible lithosphere-atmosphere-ionosphere coupling (LAI) is mainly focused on the analysis and comprehension of atmospheric and ionospheric anomalies caused by extreme lithospheric events. In this context, earthquakes are considered as possible sources of atmosphere-ionosphere anomalies. The goal of the two-year long project SABEIS (Sistemas de Alerta Basados en Efectos de terremotos y tsunamis en la IonoSfera) granted by the Spanish Ministry of Economy and Competitiveness, is to analyze the disturbances caused by earthquakes and tsunamis and their possible contribution to warning systems. These topics are receiving increased attention in the scientific community and their correct understanding can meaningfully contribute to the protection of people and economic assets in areas subject to seismic threat. The project is based on the analysis of Total Electron Content (TEC) obtained from signals of Global Navigation Satellite Systems (GNSS) and anomalies of the ionospheric F2 layer observed in ionograms. This methodology was partially applied in a previous study of the Mw6.1 earthquake in Greece occurred on January 26, 2014. In that case two TEC disturbances were detected the days prior the earthquake. The first one, four days before, was registered by the majority of the stations analyzed over Europe and after studying its temporal variation, was considered unrelated to the earthquake. The second one occurred the day before the earthquake. This anomaly appeared only at stations close to the epicenter and their temporal proximity to the earthquake point to a possible connection with the earthquake preparation process. In the SABEIS project possible anomalies caused by earthquakes in Mexico and Peru with magnitude ranging from 5.5 to 8.2, will be studied. If the results confirm the influence of seismic events on the ionosphere, the possibility of incorporating this type of analysis in a seismic alert network for the Gulf of Cadiz (southern Iberian

  7. Simple predictive model for Early Childhood Caries of Chilean children.

    PubMed

    Fierro Monti, Claudia; Pérez Flores, M; Brunotto, M

    2014-01-01

    Introducción: Las caries temprana de la infancia (CTI), a pesar de ser una enfermedad prevenible, permanece como uno de los problemas de salud pública, tanto en países industrializados como en los que están en vías de desarrollo, afectando principalmente a poblaciones vulnerables. Objetivo: el objetivo de este trabajo fue generar un modelo sencillo basado en factores de riesgo que sea predictivo del riesgo de CTI en niños de 3-5 años de edad a fin de mejorar las estrategias preventivas a nivel de salud pública. Métodos: Se recolectaron datos clínicos, del hogar y psico-socio-cultural de niños (n=250) de ambos sexos que concurren a centros de salud en la región del Bio Bio – Chile mediante historia clínica y encuesta de comportamiento. Resultados: 24% de los niños presentó problemas de comportamiento (un comportamiento extraño fue la principal característica observada como problema de comportamiento). Las variables asociadas a ceo ?4 fueron: mal temperamento del niño (OR=2,43 [1,34; 4,40]) y estrés del hogar (OR=3,14 [1,54; 6,41]). Se observe que el modelo estratificado por género masculino fue el que presentó la mayor precisión diagnóstica de CTI (AUC= 78%, p-valor=0.000); además Conclusiones: Proponemos un modelo donde la higiene oral, el consumo de azúcar, el género masculino y el mal temperamento son los principales factores de predictivos de CTI. Este modelo podría ser una herramienta promisoria para el costo-efectividad del control de caries temprana.

  8. A strategy for weight loss based on healthy dietary habits and control of emotional response to food.

    PubMed

    Pontes Torrado, Yolanda; García-Villaraco Velasco, Ana; Hernández Galiot, Ana; Goñi Cambrodón, Isabel

    2015-06-01

    Introducción: el sedentarismo y los hábitos alimentarios poco saludables son las principales causas de un balance energético negativo y un exceso de peso corporal. El estilo de vida del patrón de dieta mediterránea reduce significativamente los factores de riesgo de enfermedades no transmisibles. Por otra parte, las emociones tienen un poderoso efecto en el comportamiento alimentario. Existe una relación directa entre la elección de alimentos, las emociones y el aumento de la ingesta energética. Objetivo: conocer el comportamiento emocional de los individuos para facilitar el establecimiento de pautas dietéticas personalizadas basadas en hábitos alimentarios saludables y aumentar la fidelidad del paciente hasta conseguir el peso deseado. Material y métodos: 99 personas adultas con sobrepeso fueron sometidos a un programa de reducción de peso basado en establecer unos hábitos alimentarios y un estilo de vida saludables. La adhesión al patrón de dieta Mediterránea y el efecto de las emociones en la elección de alimentos se determinaron utilizando los cuestionarios MEDAS (Mediterranean Diet Adherence Screener) y EEQ (Emocional Eater Questionnaire), respectivamente. Resultados: la población estudiada era sedentaria, consumía una dieta poco saludable y su conducta alimentaria era dependiente de las emociones. La mayoría de los participantes (66% mujeres y 71% hombres) fueron clasificados como comedores emocionales. Durante el programa de tratamiento, los participantes modificaron sus hábitos alimentarios y su estilo de vida, consiguiendo reducir el peso corporal en al menos un 10% respecto al peso inicial. Conclusión: conocer la relación entre la ingesta de alimentos y las emociones permite personalizar la estrategia dietética para disminuir el peso corporal y la tasa de abandono.

  9. [Nutritional characteristics of school lunch menus in Biscay (Basque Country, Spain) in 2012/2013].

    PubMed

    Sancho Uriarte, Patricia; Cirarda Larrea, Francisco Borja; Valcárcel Alonso, Santiago

    2014-09-28

    Introducción: Uno de los elementos abordados desde la Estrategia para la Nutrición, Actividad física y prevención de la Obesidad y Salud (NAOS) es la alimentación en el medio escolar. Objetivo: Evaluar, tomando como referencia el conjunto mínimo de indicadores y recomendaciones de la Estrategia NAOS, una muestra de menús distribuidos en varios comedores escolares de Bizkaia. Métodos: Estudio descriptivo transversal basado en la revisión teórica de los menús basales distribuidos por siete cocinas centrales que abastecen a 324 centros escolares (80.969 alumnos). Se determinó y valoró la frecuencia semanal de varios grupos de alimentos; los documentos de referencia fueron “Evaluación y Seguimiento de la Estrategia NAOS: Conjunto de Indicadores” y las recomendaciones del “Documento de Consenso sobre la alimentación en los centros educativos”. Resultados y discusión: El 100% de los comedores cumple con los mínimos relativos a legumbres, pescados y precocinados y con las recomendaciones relativas a carne y productos cárnicos. Si bien se aproximan bastante, ninguno cumple con los mínimos de fruta, verdura o con la información nutricional complementaria. Se han evidenciado diferencias entre las recomendaciones de La Estrategia NAOS y las condiciones exigidas por el Departamento de Educación, así como dificultades en la cuantificación y clasificación de varios alimentos. Conclusiones: Se recomienda incrementar el contenido en frutas, verduras, huevos y pescado azul de los menús escolares, así como ofrecer a las familias una información de los menús más detallada.

  10. Comparison between the Coastal Impacts of Cyclone Nargis and the Indian Ocean Tsunami

    NASA Astrophysics Data System (ADS)

    Fritz, H. M.; Blount, C.

    2009-12-01

    penetrated more than 50 km inland along the Ayeyarwady delta while the maximum inundation of the Indian Ocean tsunami was 7 km at Banda Aceh. The extent of affected coast lines differs with 2 m storm surge thresholds of cyclone Nargis spanning 200 km of coastline, whereas East Africa was severely affected by the Indian Ocean tsunami at 5000 km from the epicenter. The available time window for dissemination of warnings and evacuations are significantly shorter for tsunamis than cyclones. Coastal protection in the Indian Ocean must be approached with community-based planning, education and awareness programs suited for a multi-hazard perspective. Ayeyarwady delta in Myanmar after cyclone Nargis: (a) Deforestation of mangroves for use as charcoal and land use as rice paddies; (b) Drinking water wells scoured in surf zone at Aya highlighting more than 100 m land loss due to coastal erosion.

  11. Hydrography of Bahia Todos Santos, Baja California: Results of more than twenty five years of investigations.

    NASA Astrophysics Data System (ADS)

    Bustos-Serrano, H.; Canino-Herrera, S. R.; Morales-Chavez, R.; Martinez-Garcia, G. M.

    2007-05-01

    The first study of Bahia Todos Santos (BTS) was reported by Walton in 1955. We conducted oceanographic studies in BTS since 1979. The BTS has a connection with a coastal lagoon named Estero de Punta Banda (EPB), two islands at the western portion and the Port of Ensenada. The general hydrographic characteristics are: In winter the water became homogeneous, less saline (<33.4) and with low stability. During spring and summer a hydrographic structure of three layers is noticed. The deepest layer is composed of the southern California water mass with a relatively high salinity (>33.6) low temperature (13°C), low oxygen (~3mL L-1) and rich in nutrient concentration. The isothermal top layer has relatively high temperature (>17°C) and oxygen concentration (>6mL L-1). The intermediate transition layer (seasonal thermocline) has minimum salinity, maximum oxygen and high stability. During fall there is distribution of heat from the surface layer to the entire water column. The thermic waves propagate with decrease amplitude in ~3 months, from surface to bottom water. The California Current flow generally southward off the western United States and northern Mexico and is one of the major coastal upwelling of the word oceans. The upwelling events in BTS appear regularly at the SW portion and were typically characterized by an increase in pCO2, decrease of O2, increase of nutrients and a lower temperature. Upwelling activity increases surface nutrient availability causing rise in the primary productivity and hence increased zooplankton biomass. The annual upwelling event which had a maximum strength on May, the seasonal warming and cooling, and the water advection were the dominant modifying processes for the variability of seawater characteristics. Higher salinities are located close to the coastline and lower off the bay. The levels of oxygen, alkalinity, pH and chlorophyll indicate that the maximum concentration of phytoplankton is located at the center of the bay. The

  12. População estelar jovem em galáxias irregulares próximas

    NASA Astrophysics Data System (ADS)

    Guimarães, T. A.; Telles, E.

    2003-08-01

    A análise do conteúdo estelar de galáxias próximas através da fotometria das suas estrelas resolvidas nos fornece informações importantes sobre a história de formação estelar e os processos de formação estelar em galáxias, que estão diretamente ligados ao estudo de evolução de galáxias. Quando nenhuma estrela puder ser resolvida o método mais poderoso consiste na análise do conteúdo estelar integrado das galáxias através das suas cores integradas em conjunto com informação espectroscópica que combinados com modelos de síntese evolutiva podem restringir simultaneamente a função de massa inicial (IMF) e a taxa de formação estelar (SFR). Nesse contexto, galáxias do tipo tardio, em particular, irregulares, são relevantes por várias razões: elas são objetos relativamente simples, com alta atividade de formação estelar e são objetos relativamente jovens (geralmente apresentam baixas abundâncias de elementos pesados e grande quantidade de gás). Apresentamos uma análise fotométrica de uma amostra de 7 galáxias do tipo tardio do universo local (NGC 2366, NGC 4395, NGC 4656, NGC 4214, NGC 4236, HOII, IC2574) que foram observadas com uma boa resolução espacial nas bandas B, V e R no telescópio Isaac Newton de 2.5m de Roque de los Muchachos nas Ilhas Canárias, Espanha. A distribuição espacial da população estelar jovem dessas galáxias é discutida sobre os pontos de vista dos íindices de cor integrados e dos seus diagramas cor magnitude, que comparados com isócronas teóricas, nos fornecem informações sobre os eventos de formação estelar, como por exemplo, indicações sobre a idade dos mesmos. As principais conclusões do trabalho podem ser resumidas em: (i) As galáxias irregulares possuem formação estelar recente (FE) espalhada ocorrendo nos últimos 50 Manos; (ii) A formação estelar em galáxias irregulares não é auto-propagante em escalas globais ( > 100 pc) ; (iii) A FE pode ser auto-regulável em escalas

  13. Cosmic airburst debris, climate anomalies and societal reactions at 4.2kyr BP: from North Syria to Adelie Land

    NASA Astrophysics Data System (ADS)

    Coqueugniot, E.; Courty, M. M.

    2012-12-01

    The linkages established between dust spikes, unprecedented drought and societal disruption at 4.2 kyr BP have yet failed elucidating the marked increase in aerosol. The volcanic dust component or the erratic spatial pattern are among other puzzling anomalies for a global climate event. We examine here the 4.2 kyr BP debris records from high quality sedimentary archives across the two hemispheres: (1) at Tell Dja'de (Syria), a carbonaceous surface sealed by a EB III/IV Bronze age cemetery; (2) at Tell Ahmar (Syria), the nearly intact collapsed wood frame of the Akkad palace sandwiched between the last 3rd millennium BC plastered floors and massive destruction layers of the monumental buildings; (3) debris accumulation from human processed slags in late Akkaddian contexts at Tell Leilan, Tell Chuera, Tell Beydar, Tell Brak (North Syria) and in an EB III/IV one at Umbaschi (South Syria); (4) a tsunami layer at Banda Aceh (Sumatra); (5) deep sea cores from the Mediterranean and Caspian seas, the Indian and Austral oceans. Using an in situ multi-analytical protocol, we focus on the carbonaceous polymorphs and the composite elements that we formerly defined to tracing hypervelocity cosmic airbursts. A meticulous control of their spatial pattern and structural characteristics at meso to nano-scales has helped to distinguishing the intact debris fall of airburst origin from their human processed-byproducts. The later trace the occurrence in the debris airbursts of highly valuable resources, i.e. fossil combustible with singular properties, that have been exploited since the prehistoric time. Evidence for an oceanic impact at 4.2 kyr BP in the Austral ocean are provided by the 3 m record in the Adelie land high resolution marine core (MD03-2601) showing sudden discharge of ice rafted fine debris with impact features. Their fresh fingerprints in the high to low latitude records from the southern hemisphere indicate massive dispersion of impact debris by air and surface

  14. Tsunami damages assessment: vulnerability functions on buildings based on field and earth observation survey.

    NASA Astrophysics Data System (ADS)

    Gauraz, A. L.; Valencia, N.; Koscielny, M.; Guillande, R.; Gardi, A.; Leone, F.; Salaun, T.

    2009-04-01

    The assessment of damages caused by tsunami scenarios on coastal buildings requires using vulnerability matrixes or functions to carry out a relation between the magnitude of the phenomena and the damage expected. These functions represent the probability for a building belonging to a class of vulnerability to suffer from a mean damage level. The physical vulnerability of buildings depends on two parameters: the solicitation level applied by the tsunami on buildings and their resistance capacity. According to the authors after post-tsunami observations (Reese et al. 2007; Ruangrassamee et al. 2006; Leone et al. 2006; Peiris 2006), the level of damage is clearly linked to the water elevation of the inundated areas and the type of observed buildings. Very few works propose relations based on velocity or hydrodynamic pressure of the waves. An approach developed for the estimation of the building vulnerability consists in deriving empirical damage functions starting from field observations. As part of the SCHEMA European Project on the vulnerability assessment for tsunami hazards in the Atlantic and Mediterranean area, vulnerability functions have been elaborated for different classes of buildings in order to produce vulnerability maps for exposed areas with emphasis on extraction of building characteristics using remote sensing data. The damage detection has been carried out by field data collected after the 24 December 2006 tsunami event on the southwest area of Banda Aceh (Sumatra, Thailand) completed by photo-interpretation of satellite images to get representative functions with large population of samples. The building classes consist in several categories depending mainly on the type of construction material (timber/bamboo, traditional brick, reinforced concrete …), the type of structure (beam, pillars, etc) and the number of storeys. The level of damage has been also classified in five categories, from D0 (no damage) to D5 (total destruction). Vulnerability

  15. Tectonic evolution and crustal structure of the central Indonesian region from geology, gravity and other geophysical data

    NASA Astrophysics Data System (ADS)

    Guntoro, Agus

    Bone Bay, the Makassar Strait, the Central Java Sea, the East Java Sea and the Flores Sea provinces. Each province is examined and their stratigraphy, structural and tectonic styles correlated in order to have a complete understanding of their evolution. Variations in gravity values and models demonstrate that the continental crust in the CIR was attenuated by subduction roll-back and then subjected to rifting by extensional forces. The extension in the Makassar Strait, Central Java Sea and East Java Sea took place in the Eocene, forming marginal basins. Bone Bay opened due to collision between the Banggai- Sula microcontinent and Sulawesi in the Middle Miocene and was followed by clockwise rotation of Java, Sumbawa and Flores which cause the opening of the Flores Sea. The present configuration of the CIR is influenced by the collision between the Indo-Australian Plate and the Banda-Sunda arcs.

  16. The Lesser Antilles: a case study for melt-dehydration processes in arcs

    NASA Astrophysics Data System (ADS)

    Chauvel, C.; Labanieh, S.; Carpentier, M.

    2011-12-01

    The nature and the proportion of subducted material involved in the genesis of island arcs depends on the amount and type of subducted sediments, the input from basaltic crust, the mechanism of chemical transfer and the speed and angle of the subducting plate. Here we present a compilation of geochemical features along the Lesser Antilles arc which is famous for having the most "continental crust-like" geochemical characteristics of all island arcs. We show that beneath the southern part of the Lesser Antilles arc, where vast amounts of sedimentary material are subducted, sediments melt to produce island arc magmas with elevated La/Yb and low Ba/Th, U/Th, Sr/Th and Pb/Th. Associated with these trace element characteristics are typically crustal isotopic signatures: low 143Nd/144Nd and 176Hf/177Hf and high 87Sr/86Sr and Pb isotopic ratios. In contrast, in the northern part of the arc, where far less sediment enters the trench, La/Yb is low and associated to high Ba/Th, U/Th, Sr/Th and Pb/Th in all lavas, and radiogenic isotope ratios are near those of MORB. In this part of the island arc, dehydration of altered basalt is responsible for the enrichment in fluid-mobile elements (Ba, U, Sr, Pb etc..) and the subducted sediments are barely involved. On Martinique in the middle of the arc, both types of lavas exist but not in the same place. On the west side of the island, sediment melting dominates while dehydration of basalt controls the volcanism closer to the trench. This dichotomy between sediment melting and slab dehydration appears a worldwide feature: in Sunda, Luzon and Banda arcs, subducted sediment melts to produce lavas with high La/Yb, low Ba/Th, U/Th, Sr/Th and Pb/Th and "crust-like" radiogenic isotopic characteristics. In contrast, in Izu-Bonin-Mariana, Tonga and Kermadec arcs, fluid migration leading to high mobile/immobile trace element ratios and "mantle-like" isotopes controls element transport from the subducted slab. The only arcs similar to the

  17. Geochemical Interpretation of Collision Volcanism

    NASA Astrophysics Data System (ADS)

    Pearce, Julian

    2014-05-01

    Collision volcanism can be defined as volcanism that takes place during an orogeny from the moment that continental subduction starts to the end of orogenic collapse. Its importance in the Geological Record is greatly underestimated as collision volcanics are easily misinterpreted as being of volcanic arc, extensional or mantle plume origin. There are many types of collision volcanic province: continent-island arc collision (e.g. Banda arc); continent-active margin collision (e.g. Tibet, Turkey-Iran); continent-rear-arc collision (e.g. Bolivia); continent-continent collision (e.g. Tuscany); and island arc-island arc collision (e.g. Taiwan). Superimposed on this variability is the fact that every orogeny is different in detail. Nonetheless, there is a general theme of cyclicity on different time scales. This starts with syn-collision volcanism resulting from the subduction of an ocean-continent transition and continental lithosphere, and continues through post-collision volcanism. The latter can be subdivided into orogenic volcanism, which is related to thickened crust, and post-orogenic, which is related to orogenic collapse. Typically, but not always, collision volcanism is preceded by normal arc volcanism and followed by normal intraplate volcanism. Identification and interpretation of collision volcanism in the Geologic Record is greatly facilitated if a dated stratigraphic sequence is present so that the petrogenic evolution can be traced. In any case, the basis of fingerprinting collision terranes is to use geochemical proxies for mantle and subduction fluxes, slab temperatures, and depths and degrees of melting. For example, syn-collision volcanism is characterized by a high subduction flux relative to mantle flux because of the high input flux of fusible sediment and crust coupled with limited mantle flow, and because of high slab temperatures resulting from the decrease in subduction rate. The resulting geochemical patterns are similar regardless of

  18. SE Asian-West Pacific Tectonics and Mantle Structure

    NASA Astrophysics Data System (ADS)

    Hall, Robert

    2010-05-01

    zones. This long term, but not continuous, subduction resulted in a weak and thin lithosphere, which is very responsive to changing forces at plate boundaries and contributed to a hot and weak lower crust that can flow due to tectonic and sedimentary loading. During the Cenozoic there were unusually rapid vertical motions (both subsidence and uplift), with gravity-driven movements of the upper crust, accompanied by exceptionally high rates of erosion, and by massive movements of sediment. The magnitude of these motions is probably far greater than dynamic topographic effects within SE Asia although mantle-driven vertical movements may be detectable in stronger continental parts of the region and in some of the marginal oceanic basins. Back-arc basins such as those of the Philippine and Banda Seas appear to have formed by rollback driven by the great age of the subducting lithosphere, mainly in intra-oceanic settings at plate margins. Other marginal basins within continental crust, such as the South China Sea, are more easily explained by slab-pull forces. Back-arc basins of Mesozoic age are not obvious, although ophiolite and arc remnants in Indonesia, the Philippines and New Guinea suggest that they formed at intra-oceanic margins of Pacific plates and perhaps not at the continental margins of SE Asia.

  19. Plate tectonic reconstruction of South and East Asia since 43 Ma using seismic tomographic constraints: role of the subducted ';East Asia Sea' (Invited)

    NASA Astrophysics Data System (ADS)

    Wu, J. E.; Suppe, J.; Renqi, L.; Kanda, R. V.

    2013-12-01

    Lithosphere that subducts at convergent plate boundaries provides a potentially decipherable plate tectonic record. In this study we use global seismic tomography to map subducted slabs in the upper and lower mantle under South and East Asia to constrain plate reconstructions. The mapped slabs include the Pacific, the Indian Ocean and Banda Sea, the Molucca Sea, Celebes Sea, the Philippine Sea and Eurasia, New Guinea and other lower mantle detached slabs. The mapped slabs were restored to the earth surface and used with Gplates software to constrain a globally-consistent, fully animated plate reconstruction of South and East Asia. Three principal slab elements dominate possible plate reconstructions: [1] The mapped Pacific slabs near the Izu-Bonin and the Marianas trenches form a subvertical slab curtain or wall extending down to 1500 km in the lower mantle. The ';slab curtain' geometry and restored slabs lengths indicate that the Pacific subduction zone has remained fixed within +/- 250 km of its present position since ~43 Ma. In contrast, the Tonga Pacific slab curtain records at least 1000 km trench rollback associated with expansion of back-arc basins. [2] West of the Pacific slab curtain, a set of flat slabs exist in the lower mantle and record a major 8000km by 2500-3000km ocean that existed at ~43 Ma. This now-subducted ocean, which we call the ';East Asian Sea', existed between the Ryukyu Asian margin and the Lord Howe hotspot, present-day eastern Australia, and fills a major gap in Cenozoic plate reconstructions between Indo-Australia, the Pacific Ocean and Asia. [3] An observed ';picture puzzle' fit between the restored edges of the Philippine Sea, Molucca Sea and Indian Ocean slabs suggests that the Philippine Sea was once part of a larger Indo-Australian Ocean. Previous models of Philippine Sea plate motions are in conflict with the location of the East Asian Sea lithosphere. Using the mapped slab constraints, we propose the following 43 Ma to 0 plate

  20. 2011 Tohoku tsunami hydrographs, currents, flow velocities and ship tracks based on video and TLS measurements

    NASA Astrophysics Data System (ADS)

    Fritz, Hermann M.; Phillips, David A.; Okayasu, Akio; Shimozono, Takenori; Liu, Haijiang; Takeda, Seiichi; Mohammed, Fahad; Skanavis, Vassilis; Synolakis, Costas E.; Takahashi, Tomoyuki

    2013-04-01

    The March 11, 2011, magnitude Mw 9.0 earthquake off the Tohoku coast of Japan caused catastrophic damage and loss of life to a tsunami aware population. The mid-afternoon tsunami arrival combined with survivors equipped with cameras on top of vertical evacuation buildings provided fragmented spatially and temporally resolved inundation recordings. This report focuses on the surveys at 9 tsunami eyewitness video recording locations in Myako, Kamaishi, Kesennuma and Yoriisohama along Japan's Sanriku coast and the subsequent video image calibration, processing, tsunami hydrograph and flow velocity analysis. Selected tsunami video recording sites were explored, eyewitnesses interviewed and some ground control points recorded during the initial tsunami reconnaissance in April, 2011. A follow-up survey in June, 2011 focused on terrestrial laser scanning (TLS) at locations with high quality eyewitness videos. We acquired precise topographic data using TLS at the video sites producing a 3-dimensional "point cloud" dataset. A camera mounted on the Riegl VZ-400 scanner yields photorealistic 3D images. Integrated GPS measurements allow accurate georeferencing. The original video recordings were recovered from eyewitnesses and the Japanese Coast Guard (JCG). The analysis of the tsunami videos follows an adapted four step procedure originally developed for the analysis of 2004 Indian Ocean tsunami videos at Banda Aceh, Indonesia (Fritz et al., 2006). The first step requires the calibration of the sector of view present in the eyewitness video recording based on ground control points measured in the LiDAR data. In a second step the video image motion induced by the panning of the video camera was determined from subsequent images by particle image velocimetry (PIV) applied to fixed objects. The third step involves the transformation of the raw tsunami video images from image coordinates to world coordinates with a direct linear transformation (DLT) procedure. Finally, the

  1. [Type 2 Diabetes Mellitus, Depression and Eating Disorders in Patients Submitted to Bariatric Surgery].

    PubMed

    Brandão, Isabel; Marques Pinho, Ana; Arrojado, Filipa; Pinto-Bastos, Ana; Maia da Costa, José; Coelho, Rui; Calhau, Conceição; Conceição, Eva

    2016-03-01

    Introdução: A obesidade associa-se a um elevado número de comorbilidades, entre as quais a diabetes mellitus tipo 2 e a patologia psiquiátrica. A cirurgia bariátrica tem demonstrado ser a melhor solução para a perda de peso e a melhoria das complicações nos casos de obesidade mórbida. O objetivo deste estudo é o de analisar a evolução da diabetes mellitus tipo 2 e de variáveis psicopatológicas antes e depois da cirurgia bariátrica e verificar o seu impacto na perda de peso. Material e Métodos: É um estudo longitudinal, que avalia 75 indivíduos antes e depois de serem submetidos a cirurgia bariátrica (47 - banda gástrica; 19 - bypass Roux-en-Y gástrico; 9 - sleeve gástrico), com tempo de follow-up entre 18 e 46 meses. Os instrumentos de avaliação foram a entrevista clínica e os questionários Eating Disorder Examination questionnaire - EDE-Q e Beck Depression Inventory - BDI. Resultados: Verificou-se melhoria relativamente à variável dicotómica diabetes mellitus tipo 2 após a cirurgia (X(1) = 26,132, p < 0,001). Não ocorreu melhoria significativa em termos de patologia psiquiátrica quando a análise foi controlada para o tipo de cirurgia. Encontrámos uma associação significativa entre as variáveis em estudo no pós-cirúrgico e a perda de peso. Este modelo explica 27% da variação do peso após a cirurgia (R2 = 0,265) e é significativo F (3,33) = 2,981, p = 0,038. Discussão: A diabetes mellitus tipo 2, patologia depressiva ou do comportamento alimentar mostraram estar relacionados com a perda de peso. Não ficou esclarecido em que sentido esta relação é estabelecida, nem a relação que estas variáveis metabólicas e psicológicas possam ter entre si ao longo do período pós cirurgia bariátrica. Conclusão: A diabetes mellitus tipo 2 evoluiu favoravelmente após a cirurgia. Diabetes mellitus tipo 2, depressão e patologia alimentar no período pós-cirúrgico associaram-se a menor perda de peso. As variáveis estudadas no

  2. Condições físicas do disco de acréscimo da nova-anã V4140 SGR

    NASA Astrophysics Data System (ADS)

    Borges, B.; Baptista, R.

    2003-08-01

    Discos de acréscimo são aparatos cósmicos que permitem que matéria seja eficientemente acrescida sobre uma fonte compacta pela remoção de momento angular via tensões viscosas enquanto transforma a energia potencial gravitacional em calor e, posteriormente, em radiação. Sistemas binários semi-ligados, como Variáveis Cataclísmicas (VCs) não-magnéticas, são talvez os melhores ambientes encontrados para o estudo da física desses discos de acréscimo. O desenvolvimento de técnicas de imageamento indireto, como o mapeamento por eclipses (MME) e a tomografia Doppler, permitiu avanços importantes na compreensão da física dos processos de acréscimo desses sistemas. V4140 Sagitarii é uma VC eclipsante de curto período orbital (~ 90 min) que não havia sido classificada como nova-anã ou polar. Neste trabalho apresentamos a análise do mapeamento por eclipse feito com dados de fotometria CCD nas bandas B, V e R de V4140 Sgr realizada no LNA. O objeto foi observado no declínio de erupção em julho de 1992 e em erupção em julho de 2001, isso indicou a classificação do sistema como uma nova-anã. A análise, feita sobre os mapas já apresentados em trabalho anterior, apresenta (i) diagrama cor-cor, que indica uma emissão opticamente espessa nas partes internas do disco em quiescência (R < RL1); (ii) diagrama cor-magnitude, usado para inferir uma distância de 600 +/- 10 pc ao sistema; (iii) a distribuição radial de temperatura observada que concorda com a lei de disco espesso em estado estacionário TµR-3/4, com temperaturas em torno de 10000 K e 3000 K ns partes internas e externas do disco em quiescência, respectivamente; (iv) a evolução da distribuição de temperatura no declínio de erupção; (v) estimativa da transferência de massa de 109.9+/-0.1 M¤/ano em quiescência, similar àquelas observadas em novas-like. O sistema é comparado à outras novas-anãs (e.g. OY Car e Z Cha) em quiescência e erupção, mostrando-se tratar um

  3. Continental crustal history in SE Asia: Insights from zircon geochronology

    NASA Astrophysics Data System (ADS)

    Sevastjanova, I.; Hall, R.; Gunawan, I.; Ferdian, F.; Decker, J.

    2012-12-01

    Cenozoic. All these populations are complex and suggest multiple episodes of magmatism for each. Permian-Triassic detrital zircons were derived from two distinct source areas, the SE Asian tin belt and eastern Indonesia (Banggai-Sula and West Papua). It is notable that in both these areas zircon ages show a gap in magmatism around 260-250 Ma. In West Papua, North Banda and Sulawesi, detrital Triassic zircons are present in many metamorphic rocks, suggesting Triassic or post-Triassic metamorphism in these areas, in rocks previously thought to be Paleozoic or older metamorphic basement. Cretaceous zircons are common in Sumatra, Borneo, Vietnam, Malaysia, Thailand, on the Sunda shelf, and in Sulawesi. They were produced during multiple magmatic events that are unlikely to have a common cause. Cretaceous zircons have also been found in all metamorphic rocks from SW Borneo previously suggested to be Palaeozoic or older. Cenozoic zircons were largely derived from subduction volcanism and are widely distributed, but are a relatively small proportion of the total data set, reflecting a combination of natural, sampling and analytical reasons. Zircon age data suggest that SE Asia records crustal growth mainly by re-assembly of continental fragments rather than by creation of significant new crust.

  4. A estabilidade dos PAHS em função da energia da radiação interestelar nas faixas UV e raios-X

    NASA Astrophysics Data System (ADS)

    Pinotti, R.; Costa, R. K.; Boechat-Roberty, H. M.; Lago, A.; Souza, G. B.

    2003-08-01

    A nebulosa CRL 618, uma proto-nebulosa planetária cuja nuvem molecular espessa envolve uma estrela B0, contém uma grande quantidade de C2H2 e CH4. Estas moléculas são consideradas os tijolos da criação de grandes moléculas carbonadas como os Hidrocarbonetos Policíclicos Aromáticos (PAHs). Esta nebulosa, por estar exposta a intensos campos de UV e Raios-X, é uma região de fotodissociação molecular que propicia a formação de novas moléculas, confirmada pela presença de C4H2 e C6H6 (Benzeno), que é a unidade básica dos PAHs. Atribui-se a esta família de moléculas orgânicas duas propriedades fundamentais, a resistência para sobreviver ao campo de radiação UV interestelar e a geração das bandas de emissão não identificadas (UIR) observadas no infravermelho. No entanto, alguns autores questionam a resistência dos PAHs ao campo de radiação UV interestelar. Empregando a técnica de Espectrometria de Massas por Tempo de Vôo, no modo de coincidência fotoelétron-fotoíon, estudamos a ionização e fragmentação das seguintes moléculas: Benzeno, Benzeno deuterado, Naftaleno, Antraceno e Fenantreno. Utilizamos uma fonte de Hélio monocromática em 21,21 eV (584,5 Å) e a radiação Síncroton do Laboratório Nacional de Luz Síncroton (LNLS) em diferentes energias nas proximidades da borda do C 1s ( 290 eV). Comprovamos a estabilidade dos PAHs sob ação de UV (21,21 eV), onde eles apresentam um baixo nível de fotodissociação, produzindo fragmentos ionizados com rendimento total na ordem de 5 por cento em relação ao íon molecular pai. Entretanto, em altas energias, na faixa de Raios-X, a quebra destas moléculas torna-se mais intensa, com a produção de muitos fragmentos. Como uma das rotas de fragmentação do Naftaleno é [(C10H8) = > (C6H6+) + (C4H2) + (e-)], e como temos as evidências observacionais da existência do C4H2 e C6H6 na nebulosa CRL 618, sugerimos que este ambiente também possui o Naftaleno.

  5. Composição química, evolução e cinemática de estrelas de tipo solar

    NASA Astrophysics Data System (ADS)

    Silva, R. O.; Porto de Mello, G. F.; Milone, A. C.

    2003-08-01

    A composição química das estrelas de tipo solar é um diagnóstico extremamente valioso da evolução química do disco da Galáxia. Existe alguma evidência de que tal evolução tem sido heterogênea no espaço e ao longo do tempo e que a composição química do Sol pode não ser um padrão representativo de abundâncias. Neste trabalho, foram obtidas as abundâncias dos elementos químicos C, N, Na, Mg, Si, Ca, Sc, Ti, V, Cr, Mn, Fe, Co, Ni, Cu, Zn, Sr, Y, Zr, Ba, La, Ce, Nd e Sm em uma amostra de estrelas de tipo solar na vizinhança solar (distâncias £ 25 pc). A técnica empregada foi a análise espectroscópica diferencial em relação ao Sol, baseando-se em dados de alta resolução (R ~ 46.000) e alta razão sinal/ruído (S/R > 300), obtidos com o espectrógrafo échelle de bancada do telescópio de 1,5 m do CTIO. Adicionalmente, abundâncias de C e N foram obtidas através de síntese de bandas moleculares dos Sistemas Eletrônicos Swan do C2 e Vermelho do CN utilizando-se um programa de síntese espectral. Os parâmetros atmosféricos foram estabelecidos usando cores fotométricas, o equilíbrio de excitação e ionização de linhas do Fe e a análise da temperatura e da luminosidade estelares no diagrama HR. Os resultados de abundâncias químicas obtidos proporcionam uma melhor compreensão da relação das abundâncias conhecidas para o Sol com a das estrelas anãs de tipo G da população local, uma vez que as razões de abundâncias de diversos elementos (em relação ao ferro) obtidas para estrelas de metalicidade semelhante à solar diferem daquelas obtidas para o Sol. Tais resultados também contribuem para um melhor entendimento do processo de evolução química da vizinhança solar e do enriquecimento nucleossintético do disco galáctico.

  6. Um supressor de fundo térmico para a câmara infravermelha CamIV

    NASA Astrophysics Data System (ADS)

    Jablonski, F.; Laporte, R.

    2003-08-01

    O ângulo sólido subtendido pelos pixels na câmara infravermelha do NexGal (CamIV) que operamos no OPD/LNA contém contribuições provenientes do sistema de coleta de fluxo propriamente dito - sendo esta a parte que interessa para as medidas astronômicas - e contribuições da obstrução central, sistema de suporte do espelho secundário e região exterior à pupila de entrada do telescópio. Estas últimas contribuições são devi-das à emissão de corpo negro à temperatura ambiente e aumentam exponencialmente para comprimentos de onda maiores que 2 micra (banda K, no infravermelho próximo). Embora a resultante pode ser quantificada e subtraída dos sinais relevantes, sua variância se adiciona à variância do sinal, e pode ser facilmente a contribuição domi-nante para a incerteza final das medidas, tornando ineficiente o processo de extração de informação e degradando a sensibilidade da câmara. A maneira clássica de resolver esse problema em sistemas ópticos que operam no infravermelho, onde os efeitos da emissão térmica do ambiente são importantes, é restringir o ângulo sólido subtendido pelos pixels individuais exclusivamente aos raios provenientes do sistema óptico. Para tanto, projeta-se uma imagem real, bastante reduzida, da pupila de entrada do sistema óptico num anteparo que transmita para o sistema de imageamento só o que interessa, bloqueando as contribuições das bordas externas à pupila de entrada, obstrução central do telescópio e sistema de suporte. Como a projeção é realizada em ambiente criogênico, a contribuição térmica espúria é efetivamente eliminada. Nós optamos por um sistema do tipo Offner para implementar na prática esta função. Trata-se de um sistema baseado em espelhos esféricos, bastante compacto e ajustado por construção. A opção por espelhos do mesmo material que o sistema de suporte (Alumínio) minimiza a dilatação diferencial, crítica nesse tipo de aplicação. Apresentamos as solu

  7. Poblacion estelar joven embebida en la nube molecular galactica asociada a la fuente IRAS 18236-1205

    NASA Astrophysics Data System (ADS)

    Romero, Ricardo Retes

    2008-06-01

    En esta tesis presento una metodología de seleccion y estudio de la población estelar embebida en la nube molecular galactica asociada a la fuente IRAS 18236-1205. La fuente IRAS posee colores de region Ultra Compacta HII (UCHII) y tiene deteccióon en monosulfuro de carbono (CS), trazador molecular de alta densidad, lo cual da la posibilidad de definir la nube molecular asociada hacia esta region. Lo anterior muestra que esta es buena candidata a región de formación estelar masiva. La metodología de seleccion de la población embebida, est à basada por una parte, en la distribución del gas molecular monoxido de carbono (13CO) asociado a la fuente IRAS, nube molecular seleccionada del mapeo Galactic Ring Survey (GRS) realizado en 13CO. Otros pasos de la seleccion, se basan en los diagramas color-color y color-magnitud con datos del cercano infrarrrojo de 2MASS. Para el estudio de la componente estelar se usaron los catalogos de fuentes puntuales en el cercano, medio y lejano infrarrojo de 2MASS, SPITZER e IRAS, respectivamente. De los diagramas color-color y color-magnitud, usando datos de 2MASS, se construyo un criterio fotométrico para identificar los objetos estelares j ovenes embebidos en la region molecular. Aplicando modelos a la distribución espectral de energía (SED) de algunos ellos, se encontraron parametros estelares de objetos estelares j ovenes embebidos de masa intermedia y alta. Adicionalmente, se encontro un objeto de masa ´ intermedia no identifiado por el catalogo de 2MASS y su efecto sobre el medio interestelar, emision en la banda de [4.5] μm de IRAC-Spitzer asociado a un outflow. Dos de los objetos seleccionados por el criterio fotometrico resultaron ser objetos estelares jovenes de alta e intermedia masa (B1V/B2V y B8V/A0V respectivamente), los cuales deben estar asociados a la emision radiativa responsable de los colores de región UC HII. Otro objeto estelar joven de baja masa (F0V/F5V) fue encontrado en la region de estudio

  8. Quality of life of diabetic patients with medical or surgical treatment.

    PubMed

    Weiner, S; Neugehauer, E A M

    2013-03-01

    Introducción: En general, la mayoría de los estudios coinciden en que la calidad de vida de las personas con diabetes es peor que la calidad de vida de la población general (QoL). Además, estos mismos estudios también han descrito efectos muy positivos sobre la calidad de vida tras cirugía bariátrica. El objetivo de este estudio fue analizar si el impacto sobre la calidad de vida de los pacientes diabéticos después de ser sometidos a cirugía bariátrica según el test (QoL) es el que se supone debería ser. Métodos: Analizamos nuestra colección de datos prospectivos de 524 pacientes diabéticos que se sometieron a cirugía bariátrica entre 2001 y 2005. Todos los pacientes realizaron 3 cuestionarios de calidad de vida antes de la cirugía y después de 1, 3, 6 y 12 meses. Las respuestas se recogieron en una base de datos anual. Todos los pacientes se sometieron a una intervención de banda gástrica ajustable, Bypass Gástrico en-Y-Roux o BPD-Scopinaro. Resultados: En total se obtuvieron los datos completos de 89 pacientes que fueron incluidos en el estudio. 1 año después de la cirugía, la calidad de vida mejoró de manera significativa e independientemente de la remisión de la enfermedad y de la pérdida de peso. La diabetes mejoró en todos los casos. La mejora en la calidad de vida fue superior en los pacientes con remisión de la enfermedad que en los que únicamente mejoraron su estado, pero inferior que en los pacientes que no tenían diabetes antes de la operación. Conclusiones: Tras el análisis de la literatura y de nuestros propios datos prospectivos, podemos concluir que los beneficios que obtienen los pacientes diabéticos tras la cirugía bariátrica son debidos principalmente a la mejora de su diabetes, independientemente del IMC inicial y de la disminución del IMC tras la intervención. Se necesitan más estudios para investigar los resultados del test QoL en diabéticos con bajo índice de masa corporal tras la cirugía bari

  9. Planning Matters: Response Operations following the 30 September 2009 Sumatran Earthquake

    NASA Astrophysics Data System (ADS)

    Comfort, L. K.; Cedillos, V.; Rahayu, H.

    2009-12-01

    Response operations following the 9/30/2009 West Sumatra earthquake tested extensive planning that had been done in Indonesia since the 26 December 2004 Sumatran Earthquake and Tsunami. After massive destruction in Aceh Province in 2004, the Indonesian National Government revised its national disaster management plans. A key component was to select six cities in Indonesia exposed to significant risk and make a focused investment of resources, planning activities, and public education to reduce risk of major disasters. Padang City was selected for this national “showcase” for disaster preparedness, planning, and response. The question is whether planning improved governmental performance and coordination in practice. There is substantial evidence that disaster preparedness planning and training initiated over the past four years had a positive effect on Padang in terms of disaster risk reduction. The National Disaster Management Agency (BNPB, 10/28/09) reported the following casualties: Padang City: deaths, 383; severe injuries, 431, minor injuries, 771. Province of West Sumatra: deaths, 1209; severe injuries, 67; minor injuries, 1179. These figures contrasted markedly with the estimated losses following the 2004 Earthquake and Tsunami when no training had been done: Banda Aceh, deaths, 118,000; Aceh Province, dead/missing, 236,169 (ID Health Ministry 2/22/05). The 2004 events were more severe, yet the comparable scale of loss was significantly lower in the 9/30/09 earthquake. Three factors contributed to reducing disaster risk in Padang and West Sumatra. First, annual training exercises for tsunami warning and evacuation had been organized by national agencies since 2004. In 2008, all exercises and training activities were placed under the newly established BNPB. The exercise held in Padang in February, 2009 served as an organizing framework for response operations in the 9/30/09 earthquake. Public officers with key responsibilities for emergency operations

  10. Cinnabar, arsenian pyrite and thallium-enrichment in active shallow submarine hydrothermal vents at Paleochori Bay, Milos Island, Greece

    NASA Astrophysics Data System (ADS)

    Kati, Marianna; Voudouris, Panagiotis; Valsami-Jones, Eugenia; Magganas, Andreas; Baltatzis, Emmanouil; Kanellopoulos, Christos; Mavrogonatos, Constantinos

    2015-04-01

    -rich grains from the volcaniclastic components of the sediments and resulting in precipitation of pyrite; (b) the iron may also have been derived by the near-neutral reduced hydrothermal brines and precipitate metal sulfides as a result of cooling, mixing with seawaters; the necessary iron content to form sulfides is mostly derived from primary iron-rich components of the basement; (c) biological activity may have resulted in pyrite deposition (e.g. sulfur is provided by a biogenic reduction of marine sulphate). The mineralogy of hydrothermal precipitates considered in the present study resemble hydrothermal products from other shallow water venting areas elsewhere: Lihir and Ambitle Islands, Papua New Guinea, Kraternaya Bight, Kuriles, Russia, Punta Mita and Bahía Concepción, Mexico and Punta Banda at Baja California. The Paleochori vents contain the first documented occurrence of cinnabar on the sea floor in the Aegean area and provide an important link between offshore hydrothermal activity and the mercury-depositing mineralizing system on Milos Island. An interplay between bacterial activity, pH, Eh, temperature, precipitation rate and iron concentration resulted in precipitation of As-pyrite with interlayered cinnabar, hydrous ferric oxides enriched in thallium, alunite-jarosite solid solution and carbonates.

  11. Resolving rock exhumation versus surface uplift during arc-continent accretion on the island of Timor by integrating thermochronology and micropaleontology data

    NASA Astrophysics Data System (ADS)

    Tate, G. W.; McQuarrie, N.; Van Hinsbergen, D. J.; Bakker, R.; Reiners, P. W.; Willett, S.

    2012-12-01

    The emergence of the island of Timor is the result of active accretion of the Banda volcanic arc to the Australian continent. Since collision began in the latest Miocene, a mountain range over 2,900 m in elevation has been raised, much of the Indonesian throughflow linking the Pacific and Indian Oceans has been closed, and the final accretion stages of slab breakoff and subduction polarity reversal may have begun. New thermochronologic and micropaleontological data from Timor-Leste reveal a detailed history of both rock and surface uplift in the central portion of Timor Island. Micropaleontological data is taken from synorogenic basins in Viqueque near the southern coast and in Caiaco, 120 km to the west of Viqueque and farther to the hinterland. These data indicate surface uplift from lower bathyal depth between 5.5 and 4.4 Ma to upper-middle bathyal depth around 3.3 Ma. Uplift is further suggested by a facies change around 4.4 Ma from deep-marine chalk deposits to clay, turbiditic sandstone and debris flow deposits with fossil wood remains, showing nearby emergence. The data suggest a phase of uplift in these basins of up to 1.4 km in about 1 Myr with an uplift rate of about 1.4 mm/yr. Uplift rates since 3.3 Ma may have dropped to less than 0.2 mm/yr. In the central mountain belt between these synorogenics, thermochronologic data show that rapid exhumation was concurrent with and continued after the rapid surface uplift recorded in the basins. Along the northern coast of Timor, zircon (U-Th)/He ages are 4.4 Ma in the east (at Hilimanu) and young to about 1.5 Ma in the west (at Liquica and Ermera). Thermal models suggest exhumation that was possibly as fast as 6.4 mm/yr from as deep as 9 km. To the south and east of the higher grade zircon (U-Th)/He data, apatite (U-Th)/He ages indicate notably less exhumation. Apatite (U-Th)/He ages from the northern and southern foothills in the east (Manatuto district) vary from 3.5 to 5.5 Ma while ages cluster around 2.0 Ma in

  12. [Malnutrition in patients with cancer; four years experience].

    PubMed

    Fernández López, María Teresa; Saenz Fernández, Cecilia Alejandra; de Sás Prada, María Trinidad; Alonso Urrutia, Susana; Bardasco Alonso, María Luisa; Alves Pérez, María Teresa; Rivero Luis, María Teresa; Alvarez Vázquez, Paula; Mato Mato, José Antonio

    2013-01-01

    Objetivo: Analizar la prevalencia y el grado de desnutrición de los pacientes con cáncer remitidos a una consulta específica de Nutrición Oncológica. Material y métodos: Se trata de un estudio transversal, observacional y descriptivo basado en los datos recogidos en la primera consulta de nutrición de todos los pacientes mayores de edad con cáncer evaluados en el período comprendido entre el 1 de marzo de 2008 y el 29 de febrero de 2012. Se incluyeron 997 pacientes, a los que se les realizó la Valoración Global Subjetiva Generada por el Paciente. Resultados: El 69% de los pacientes habían perdido más de un 5% de su peso habitual en los 3 meses previos, siendo esto más frecuente entre los portadores de tumores digestivos. El 81,2% de los pacientes tenían dificultades para alimentarse, el síntoma más frecuente era la anorexia (53,3%) y la mediana de síntomas por paciente 3. La Valoración Global Subjetiva Generada por el Paciente muestra una prevalencia de desnutrición del 72,9% (29,9% desnutrición moderada y 43% desnutrición severa). La desnutrición se relacionó con el tipo de tumor y con el estadío, pero no con la edad, el sexo ni con el Índice de Masa Corporal habitual. Conclusiones: La prevalencia de desnutrición en los pacientes con cáncer evaluados en nuestra consulta es elevada. La valoración nutricional es básica para identificar a aquellos pacientes con desnutrición o riesgo de desnutrición y orientar la necesidad de tratamiento nutricional.

  13. [VALIDATION OF A COMPUTER PROGRAM FOR DETECTION OF MALNUTRITION HOSPITAL AND ANALYSIS OF HOSPITAL COSTS].

    PubMed

    Fernández Valdivia, Antonia; Rodríguez Rodríguez, José María; Valero Aguilera, Beatriz; Lobo Támer, Gabriela; Pérez de la Cruz, Antonio Jesús; García Larios, José Vicente

    2015-07-01

    Introducción: uno de los métodos de diagnóstico de la desnutrición es la albúmina sérica, por la sencillez de su determinación y bajo coste. Objetivos: el objetivo principal es validar e implementar un programa informático, basado en la determinación de albúmina sérica, que permita detectar y tratar precozmente a los pacientes desnutridos o en riesgo de desnutrición, siendo otro objetivo la evaluación de costes por grupos relacionados por el diagnóstico. Métodos: el diseño del estudio es de tipo cohorte, dinámico y prospectivo, en el que se han incluido las altas hospitalarias desde noviembre del año 2012 hasta marzo del año 2014, siendo la población de estudio los pacientes mayores de 14 años que ingresen en los diversos servicios de un Hospital Médico Quirúrgico del Complejo Hospitalario Universitario de Granada, cuyas cifras de albúmina sérica sean menores de 3,5 g/dL, siendo el total de 307 pacientes. Resultados: de los 307 pacientes, 141 presentan desnutrición (sensibilidad del programa: 45,9%). El 54,7% de los pacientes son hombres y el 45,3% mujeres. La edad media es de 65,68 años. La mediana de la estancia es de 16 días. El 13,4% de los pacientes han fallecido. El coste medio de los GRD es de 5.958,30 € y dicho coste medio después de detectar la desnutrición es de 11.376,48 €. Conclusiones: el algoritmo que implementa el programa informático identifica a casi la mitad de los pacientes hospitalizados desnutridos. Es fundamental registrar el diagnóstico de desnutrición.

  14. Late referral for chronic kidney disease patients: nutritional point of view.

    PubMed

    Guerra, Daiane Cristina; Rodrigues Neto Angéloco, Larissa; Furtado, Wander R; Barbosa Coelho, Eduardo; Garcia Chiarello, Paula

    2014-09-12

    La prevalencia de la referencia tardía de los pacientes con enfermedad renal crónica (ERC) es alta y se ha asociado con un pronóstico peor ERC, sin embargo pocos estudios se han llevado a cabo desde una perspectiva nutricional. Objetivo: Caracterizar el estado nutricional de los pacientes con ERC con la primera cita en un servicio de nefrología, con temprana (ER) y la remisión tardía (LR). Metodología: Se realizó un estudio transversal con pacientes mayores de 18 años a que se refiere el servicio de Nefrología del Hospital Universitario. Los grupos de referencia se clasificaron de acuerdo a la tasa estimada de filtración glomerular (TFG) como: LR (TFG 15 ml / min / 1.73m2), basado en la Kidney Disease Outcomes Quality Initiative. Evaluación nutricional incluyó la evaluación subjetiva global (SGA), antropométricas, de laboratorio y los datos de impedancia bioeléctrica. El software de SAS ® se utilizó para el análisis estadístico. Resultados: Fueron evaluados setenta y cinco pacientes, el 29% de ellos pertenece al grupo LR. Este grupo mostró una pérdida mayor de peso anterior (-7,0 ± 3,5 frente a -2,8 ± 7,0 Kg) y los valores más bajos para todas las variables antropométricas y de composición corporal. En general, los resultados de laboratorio del grupo LR también eran peores. De acuerdo con el SGA, todos los pacientes tenían LR algún grado de desnutrición (50% con desnutrición severa contra 28,8% en ER), que muestra resultados significativamente más bajos de la TFG (21,4 + 12,2 ml / min / 1,73 m2), albúmina (3,9 + 0,3 g / dL), bicarbonato sérico (22,8 + 5,1 mmol / L) y ángulo de fase (5.3+ 0,6 ). La función renal se correlacionó positivamente con el porcentaje de adecuación de la circunferencia del brazo (r=0,40; p.

  15. THE ASSOCIATION BETWEEN PRE-PREGNANCY OBESITY AND WEIGHT GAIN IN PREGNANCY, WITH GROWTH DEVIATIONS IN NEWBORNS.

    PubMed

    Camacho-Buenrostro, Dennis; Pérez-Molina, J Jesús; Vásquez-Garibay, Edgar M; Panduro-Barón, J Guadalupe

    2015-07-01

    Introducción: la obesidad en el embarazo se ha relacionado con mayor morbilidad para la madre y el feto. Objetivo: cuantificar la asociación entre obesidad en el embarazo con desviaciones del crecimiento de sus recién nacidos. Métodos: se realizó un estudio de casos y controles, no pareado, basado en el Nuevo Hospital Civil de Guadalajara “Dr. Juan I Menchaca” de 2012 a 2013. Las variables dependientes fueron recién nacido grande (GEG) y pequeño para edad gestacional (PEG), y la independiente obesidad pre-gestacional. Se recabaron datos socioeconómicos y ginecoobstétricos. La asociación entre las variables dependientes con las independientes, se evaluó con regresión logística. Resultados: se estudiaron 143 díadas madre-hijo con desviaciones en el crecimiento de sus RN, y 137 díadas madre-hijo sin desviaciones. La edad de las embarazadas fue 24.7 ± 6.3 vs 24.0 ± 6.0 años, y la edad gestacional 38±1.2 vs 38±1.5. Los factores asociados con desviaciones en el crecimiento fueron: obesidad pre-gestacional (RM 2.65, IC95% 1.29-5.44), ganancia de peso durante el embarazo elevada (RM 1.98, IC95% 1.04-3.76) y enfermedades durante el embarazo (RM 2.62, IC95% 1.05-6.76). Un modelo multivariado, con la variable dependiente GEG, y las covariables asociadas, demostró que la obesidad pregestacional y ganancia de peso gestacional elevada fueron predictores de GEG (RM 2.43, IC95% 1.10- 5.40) y (RM 3.31, IC95% 1.83-5.96). Conclusiones: en una población de mujeres jóvenes de escasos recursos económicos, la obesidad pregestacional y la ganancia de peso durante el embarazo alta, fueron predictores de productos GEG.

  16. [EFFECT OF A HEALTHY EATING AND PHYSICAL ACTIVITY INTERVENTION PROGRAM ON CHILHOOD OBESITY].

    PubMed

    Díaz Martínez, Ximena; Mena Bastías, Carmen; Celis-Moralesl, Carlos; Salas, Carlos; Valdivia Moral, Pedro

    2015-07-01

    Introducción: las intervenciones orientadas a la formación de estilos de vida saludable en edades tempranas podría ser una herramienta eficaz para reducir los niveles de obesidad en escolares. Objetivo: evaluar el efecto de una intervención en alimentación y actividad física (AF) en la reducción de la obesidad en escolares. Métodos: un total de 312 escolares participaron en esta intervención, la cual se aplicó durante cinco meses. Se desarrollaron talleres para la familia y los niños con material educativo basado en guías alimentarias chilenas, en conjunto con 45 minutos diarios de AF. El estado nutricional fue evaluado con el International Obesity Task Force. Los cambios en los hábitos alimentarios y de actividad física fueron evaluados mediante la aplicación de cuestionarios. Resultados: el Índice de Masa Corporal (IMC) disminuyó significativamente post intervención (-0,2 kg.m-2); al analizar estos resultados por sexo, solo los varones presentaron una reducción significativa (-0,3 kg.m-2). Resultados similares fueron observados para el perímetro de la cintura en varones (-0,4 cm). No obstante, al analizar el efecto de la intervención en aquellos escolares con sobrepeso u obesidad preintervención se observaron cambios significativos en el IMC, los cuales fueron asociados a cambios en la alimentación y los niveles de actividad física. Conclusiones: las intervenciones multidisciplinarias aplicadas a escolares del primer ciclo de enseñanza básica son efectivas a la hora de reducir los niveles de IMC e incrementar los niveles de actividad física y la calidad de la alimentación en escolares con sobrepeso u obesidad.

  17. Invertebrate fauna associated with Torpedograss, Panicum repens (Cyperales: Poaceae), in Lake Okeechobee, Florida, and prospects for biological control

    SciTech Connect

    Cuda, J.P.; Dunford, J.C.; Leavengood, J.M. Jr.

    2007-03-15

    realizado como parte de un estudio de factibilidad para determinar si conota es una candidata apropiada para un programa de control biologico clasico. En general, especimenes de aproximadamente unos 4,000 artropodos y unos 400 nematodos fueron recolectados. Muestras recolectadas pasando una red sobre vegetacion mezclada, cortando la vegetacion y tomando centros del suelo fueron dominados por representantes de artropodos de los ordenes de Hemiptera, Hymenoptera, Diptera, y Acari. Nematodos en el genero Pratylenchus, que causan lesiones sobre tejido, fueron asociados regularmente con las raices de conota. Ninguno de los organismos recolectados eran especialistas sobre conota. Aunque el control biologico clasico de la conota es factible basado sobre la magnitud de la infestacion, las perdidas economicas, la resistencia hacia los metodos de control convencionales y el informe en la India de un posible enemigo natural especifico a esta planta, la posicion botanica de este pasto maleza requiere una evaluacion de riesgo economico formal antes de continuar con un programa de control biologico clasico. (author)

  18. [DIETARY HABITS AND FEEDING BELIEFS OF PEOPLE WITH CROHN'S DISEASE].

    PubMed

    García-Sanjuán, Sofía; Lillo-Crespo, Manuel; Sanjuán-Quiles, Ángela; Richart-Martínez, Miguel

    2015-12-01

    Introducción: la enfermedad de Crohn es una enfermedad crónica de etiopatogenia desconocida. Las consecuencias que esta enfermedad provoca a nivel nutricional dependen de varios factores. Sin embargo, poco se sabe sobre las prácticas nutricionales que adoptan estos pacientes una vez diagnosticados. Objetivo: explorar la experiencia de los afectados en relación con la ingesta alimentaria, con el objetivo futuro de comprender dichas experiencias y diseñar intervenciones eficaces y adecuadas. Metodología y sujetos: se empleó un diseño cualitativo basado en el enfoque etnográfico. Se realizaron 19 entrevistas semiestructuradas, hasta conseguir la saturación de la información, a afectados por la enfermedad de Crohn, en la provincia de Alicante y, posteriormente, se realizó el análisis temático. Resultados: cinco categorías con sus respectivas subcategorías de análisis fueron identificadas a partir de los datos sobre la experiencia de alimentación de las personas entrevistadas. 1) Creencias sobre nutrición y EC, 2) Modificación de los hábitos alimentarios, 3) Búsqueda de información sobre alimentación y EC, 4) El papel de los profesionales, 5) Autogestión. Conclusiones: el conocimiento de los hábitos dietéticos de la persona con EC en una población en la que su dieta se presupone que culturalmente es reconocida como saludable, nos puede dar pautas de abordaje o apoyo profesional tanto en materia de prevención, promoción y educación para la salud, así como sobre su nivel organizativo en las instituciones sanitarias, cosas que actualmente no se tienen en cuenta, puesto que el abordaje de la EC es meramente clínico y con enfoque patológico, pero no desde una perspectiva de salud, fomentando hábitos saludables desde la multidisciplinariedad.

  19. [Morning rise in home blood pressure and target organ damage in hypertensive patients].

    PubMed

    Barochiner, Jessica; Aparicio, Lucas S; Cuffaro, Paula E; Rada, Marcelo A; Morales, Margarita S; Alfie, José; Marin, Marcos J; Galarza, Carlos R; Waisman, Gabriel D

    2014-01-01

    El incremento matutino de la presión arterial (IMPA) aumenta el riesgo cardiovascular. Los estudios que evalúan la asociación entre IMPA domiciliaria y daño de órgano blanco son escasos y casi exclusivamente basados en población asiática. Nuestro objetivo fue caracterizar a los pacientes hipertensos con IMPA domiciliaria y establecer una posible asociación con la presencia de hipertrofia ventricular izquierda (HVI). Métodos: se incluyeron hipertensos medicados ≥18 años que realizaron mediciones de PA domiciliaria (4 días de mediciones por duplicado, a la mañana, tarde y noche) y completaron un cuestionario acerca de sus factores de riesgo y antecedentes de enfermedad cardiovascular. Se revisaron las historias clínicas para extraer datos ecocardiográficos. Se definió como IMPA a una diferencia entre el promedio de PA sistólica domiciliaria matutina – vespertina ≥15 mmHg. Se consideró que los pacientes tenían HVI si el índice de masa ventricular era >95 g/m2 en mujeres y >115 g/m2 en varones. Las variables identificadas como predictores relevantes de IMPA fueron introducidos en un modelo multivariado de regresión logística. Resultados: se incluyeron 216 pacientes, con una edad media de 68 (+13,3) años, 69,4% mujeres y 99,1% caucásicos. La prevalencia de IMPA fue de 13,4% y las variables independientemente asociadas fueron HVI (OR 3,5; 95%CI 1,1-11,4), edad (OR 1,05; 95%CI 1,003-1,1) y antecedente de enfermedad cerebrovascular (OR 3,9; 95%CI 1,1-14,2). En conclusión, el IMPA evaluado por monitoreo domiciliario presenta asociación independiente con HVI, edad y antecedentes de enfermedad cerebrovascular, debiendo esclarecerse las implicancias terapéuticas de esta observación en estudios prospectivos a gran escala.

  20. [Pharmaceutical care and home delivery of medication to patients with chronic myeloid leukemia].

    PubMed

    San José Ruiz, Begoña; Gil Lemus, María Angeles; Figuero Echeverria, María Puy

    2015-01-01

    Objetivo: El objetivo de este artículo es describir la puesta en marcha de un modelo de envío domiciliario y atención farmacéutica presencial y no presencial a pacientes con leucemia mieloide crónica en tratamiento con inihibidores de tirosin kinasa. Método: Los pacientes diagnosticados de leucemia mieloide crónica fueron seleccionados como población susceptible de recibir este nuevo modelo de atención. Esta elección respondía a cuatro características: cronicidad de la patología, periodicidad de las consultas médicas, valor del seguimiento farmacéutico y conservación a temperatura ambiente de los medicamentos. Resultados: De 68 pacientes diagnosticados de leucemia mieloide crónica en tratamiento con inhibidores de tirosin kinasa se eligieron 42 por acudir a las consultas médicas de hematología con una periodicidad superior a tres meses. Se les envió una carta de presentación y un cuestionario sobre sus preferencias. Dieciséis expresaron su deseo de participar en el nuevo modelo. El departamento jurídico redactó un contrato para garantizar la confidencialidad, así como un modelo de consentimiento informado. Se estableció un modelo logístico de reparto basado en rutas y horarios definidos. Previo a la inclusión en el programa, se realizó una consulta de atención farmacéutica presencial y se estableció el medio de comunicación para las próximas consultas no presenciales. El envío de medicación tuvo un coste mensual de 13,2€ (con IVA) por paciente. Todos los pacientes que iniciaron el programa continúan en él. Se han realizado hasta la fecha, 5 envíos por paciente. Conclusiones: Es posible instaurar un modelo alternativo de atención farmacéutica con envío domiciliario de medicación, manteniendo la relación farmacéutico-paciente, evitando desplazamientos, garantizando la confidencialidad y racionalizando el stock.

  1. HIGH BODY MASS INDEX AMONG PATIENTS UNDERGOING HEMATOPOIETIC STEM CELL TRANSPLANTATION: RESULTS OF A CROSS-SECTIONAL EVALUATION OF NUTRITIONAL STATUS IN A PRIVATE HOSPITAL.

    PubMed

    Pereira, Andrea Z; Victor, Elivane S; Vidal Campregher, Paulo; Piovacari, Silvia M F; Bernardo Barban, Juliana S; Pedreira, Wilson L; Hamerschlak, Nelson

    2015-12-01

    Introducción: el estado nutricional previo al trasplante de células madre hematopoyéticas (HSCT) afecta al pronóstico: los pacientes con una mejor nutrición necesitan un menor tiempo de injerto, mientras que una nutrición pobre estaría asociada a un aumento de la tasa de mortalidad, complicaciones, costes médicos, mala calidad de vida y hospitalización. Además, los pacientes con bajo peso presentan un mayor riesgo de muerte al principio del periodo post-HSCT, y la tasa de mortalidad sin recaída es mayor en aquellos con bajo peso extremo, sobrepeso y obesidad. La obesidad está relacionada con una toxicidad asociada al tratamiento, una incidencia más alta de enfermedad de injerto-huésped de grado II-IV (GVHD), infecciones y mortalidad. El objetivo de este estudio fue investigar el estado nutricional de pacientes que se sometieron a HSCT entre 2007 y 2013 en un hospital privado, calculando el índice de masa corporal (IMC), para comprobar la prevalencia de posibles desajustes nutricionales, especialmente obesidad. Métodos: en este estudio retrospectivo, basado en informes médicos, analizamos datos de todos los pacientes con enfermedades tumorales y no tumorales que se sometieron a HSCT desde enero de 2007 hasta febrero de 2014 en el Centro de hematología-oncología y trasplante de médula ósea en un gran centro de especialidades médicas en Brasil. Resultados: en el periodo se trató y analizó un total de 257 casos, de los cuales el 79% tenían edades de hasta 65 años. Entre estos, el 56% tenían sobrepeso u obesidad. Observamos una mayor prevalencia de obesidad en pacientes ancianos (P < 0,001). El IMC medio de la muestra total fue 26,4 kg/m2. El IMC fue significativamente diferente entre géneros, con una prevalencia mayor de sobrepeso entre los hombres (P < 0,001). Conclusión: a diferencia de otros estudios, nuestra investigación ha mostrado bajas tasas de tasas de bajo peso y altas tasas de sobrepeso y de obesidad en los hombres y pacientes

  2. [Glycosylated hemoglobin A1c as a diagnostic test for diabetes mellitus in adolescents with overweight and obesity].

    PubMed

    Rivera-Hernández, Aleida; Zurita-Cruz, Jessie Nallely; Garrido-Magaña, Eulalia; Fiorentini-Fayad, Gigliola Margaretta; Nishimura-Meguro, Elisa

    2015-01-01

    Introducción: en 2009 se introdujo un criterio diagnóstico para la diabetes mellitus 2 (DM2) en población adulta, basado en los niveles de hemoglobina glucosilada (HbA1c) mayor o igual a 6.5 %; el punto de corte en población pediátrica podría ser menor. Se buscó determinar la utilidad de este criterio en adolescentes mexicanos con sobrepeso u obesidad. Métodos: se hizo somatometría completa, revisión del estadio de Tanner y presión arterial, glucemia, curva de tolerancia a la glucosa (CTOG) y HbA1c. Se calculó especificidad, sensibilidad, valores predictivos positivos y negativos y curva ROC para el diagnóstico de DM con HbA1c. Resultados: se estudiaron 109 pacientes entre 10 y 16 años referidos por obesidad o sobrepeso más comorbilidades, 58 % mujeres, edad 13 ± 1.74 años, IMC percentil 95.3 y HbA1c 5.73 ± 0.9 %. Se estableció el diagnóstico de DM en 9 casos (8.3 %), prediabetes en 8 (7.3 %) y tolerancia normal a la glucosa en 92 (84.4 %), el promedio de HbA1c fue de 5.6 ± 0.04, 5.7 ± 0.4 y 5.6 ± 0.73 %, respectivamente. La HbA1c mayor o igual a 6.5 % tuvo una sensibilidad de 12.5 %, especificidad de 89.8 %, VPP 10.65 y VPN 14.28. El mejor punto de corte para diagnosticar DM por curva ROC de HbA1c fue de 5.45 %, con sensibilidad de 62.5 % y especificidad de 57.1 %, VPP 2.53 y VPN 33.3. Conclusiones: el nivel de HbA1c mayor o igual a 6.5% tuvo baja sensibilidad y especificidad para diagnosticar DM. Un punto de corte menor es insuficiente para utilizar la HbA1c como criterio diagnóstico.

  3. Effects of exercise on inflammation in cardiac rehabilitation.

    PubMed

    Roca-Rodríguez, María del Mar; Garrido-Sánchez, Lourdes; García-Almeida, Jose Manuel; Ruiz-Nava, Josefina; Alcaide-Torres, Juan; Gómez-González, Adela; Montiel-Trujillo, Angel; Tinahones-Madueño, Francisco

    2015-06-01

    Introducción: a los pacientes con riesgo cardiovascular se les recomiendan programas de pérdida de peso y dieta saludable, pero la eficacia de estos programas a la hora de reducir la mortalidad es controvertida. Objetivo: examinar los efectos agudos y a largo plazo de un programa de rehabilitación cardíaca de dos meses de duración sobre las quemocinas relacionadas con la inflamación en pacientes con enfermedad cardiovascular. Diseño: estudio de cohortes prospectivo. Métodos: se estudiaron 26 pacientes con enfermedad cardiovascular inscritos en un programa de rehabilitación cardíaca basado en intervenciones nutricionales y de ejercicio. Se analizaron el estilo de vida y variables clínicas, metabólicas e inflamatorias. Resultados: 88,5% eran hombres y la edad media fue de 54,9 ± 7,8 años. Al final del programa de rehabilitación cardíaca las variables del perfil glucémico y lipídico descendieron, excepto el colesterol de lipoproteínas de alta densidad, que aumentó. Ácido úrico, interleucina-6, interleucina-1 beta, adiponectina y leptina se mantuvieron estables. Interleucina-6 correlacionó positivamente con proteína C reactiva y negativamente con glucosa en sangre. Interleucina-1 beta correlacionó positivamente con proteína C-reactiva y negativamente con las cifras de presión arterial. Encontramos correlaciones significativas entre los cambios en interleucina-6 e interleucina- 1 beta y los cambios en los equivalentes metabólicos y proteína C-reactiva, antes y después del programa de rehabilitación cardíaca. No se observaron correlaciones significativas con peso, circunferencia de cintura o masa grasa. Conclusiones: la rehabilitación cardiaca mejora las variables antropométricas, las cifras de presión arterial, así como el perfil de lípidos y los resultados de la ergometría. Sin embargo, no se observaron cambios con respecto al estado inflamatorio.

  4. Descripción del coronógrafo a ser instalado en Argentina (MICA)

    NASA Astrophysics Data System (ADS)

    Stenborg, G.; Francile, C.; Schwenn, R.; Epple, A.; Rovira, M.

    El ``Coronógrafo de espejo para Argentina'' es un telescopio solar terrestre a ser colocado en el Observatorio Astronómico Félix Aguilar (El Leoncito), antes de finalizar 1996, como parte de un programa de ciencia bilateral entre Alemania y Argentina. Eclipses fotográficos de alta resolución han revelado que la corona solar es altamente estructurada y variable. De hecho, está contínuamente deformada y moldeada por los movimientos convectivos de los extremos de los arcos magnéticos en la fotosfera, estando, en muchas oportunidades, afectada por explosivas liberaciones de energía. MICA, en conjunción con otros telescopios solares espaciales y terrestres, tratará de contribuir al entendimiento de cuestiones fundamentales de la física solar. Entre ellas: cómo la corona está siendo calentada, dónde y cómo el viento solar es acelerado, qué causa los transitorios coronales, etc. Para ello investigará la distribución de los parámetros del plasma y su evolución con el tiempo, la estructura espacial de la corona en fina y gran escala, procesos que ocurren en los transitorios coronales y factores que los disparan, etc. Para responder a estas cuestiones MICA observará la atmósfera solar por sobre el limbo entre 1.1 y 2 radios solares aproximadamente, usando un nuevo tipo de sistema coronográfico que permite suprimir el brillo del disco solar suficientemente bien, tomando las imágenes con una cámara CCD de 1024x1024 pixels, codificada en 12 bits, pudiendo el mismo ser operado en forma remota. En la presente exposición describiremos las características del instrumento, cómo será controlado y qué esperamos observar basados en las imágenes obtenidas por los telescopios de similares características LASCO C1 a bordo del SOHO y PICO (ubicado en el Observatorio de Pic du Midi, Francia).

  5. Stature estimation using the knee height measurement amongst Brazilian elderly.

    PubMed

    Fogal, Aline Siqueira; Franceschini, Sylvia do Carmo Castro; Priore, Silvia Eloiza; Cotta, Rosângela Minardi M; Ribeiro, Andréia Queiroz

    2014-10-16

    Introducción: La estatura es una variable importante en varios índices del estado nutricional que son aplicables a las personas mayores. Sin embargo, la estatura es difícil o imposible de medir en la edad avanzada, ya que a menudo son incapaces de mantener la posición de pie. Una alternativa es el uso de altura estimada a partir de mediciones de medida de altura de la rodilla. Objetivos: Este estudio tuvo como objetivo evaluar la exactitud de la fórmula propuesta por Chumlea et al. (1985), basado en la altura de la rodilla de una población caucásica para estimar la altura y su aplicación en el cálculo del índice de masa corporal en las personas mayores residentes en la comunidad de Viçosa, Minas Gerais, Brasil. Métodos: La muestra incluyó a 621 adultos mayores de 60 anõs y más, que viven en la comunidad. Se tomaron medidas de peso, talla y altura de la rodilla (AR) y el Índice de Masa Corporal (IMC) se calculó con el peso medido y estimado. Se utilize la prueba T del estudiante para la comparación de las mediciones de altura entre los géneros. Para la comparación de los valores estimados y medidos se utilizó la prueba T pareada y también la metodología propuesta por Bland y Altman para comparar la diferencia entre las mediciones. Para evaluar el acuerdo entre las clasificaciones para el IMC se utilizó el Kappa de Cohen. Resultados: Los valores medios obtenidos a partir de AR fueron más altos que los medidos en la muestra completa y mujeres. Hay subestimación de IMC en mujeres y también en el conjunto. Conclusiones: Los resultados sugieren que la ecuación Chumlea no era adecuado para estimar la altura de la muestra en cuestión, especialmente para las mujeres.

  6. Eficacia de la detección sistemática de la gripe en las fronteras en los viajeros que llegan por vía aérea*

    PubMed Central

    Priest, Patricia C.; Jennings, Lance C.; Duncan, Alasdair R.; Brunton, Cheryl R.; Baker, Michael G.

    2015-01-01

    Objetivos. Se midieron los síntomas y la prevalencia de la gripe (también llamada influenza), así como la eficacia del mecanismo de detección sistemática basado en los síntomas y la temperatura para diagnosticar la gripe en viajeros internacionales que llegaban por vía aérea. Métodos. El presente estudio transversal recopiló datos de viajeros que llegaron al aeropuerto internacional de Christchurch (Nueva Zelandia) en el invierno del 2008 mediante un cuestionario de salud, medición de la temperatura y toma de muestras de las vías respiratorias. Resultados. De los viajeros, 15 976 (68%) entregaron los formularios completos. De ellos, 17% notificaron al menos un síntoma de gripe; los síntomas más comunes fueron rinorrea o congestión nasal (10%) y tos (8%). Se tomaron muestras de las vías respiratorias de 3 769 viajeros. La prevalencia estimada de la gripe fue de 1,1% (4% en las personas sintomáticas, 0,2% en las asintomáticas). La sensibilidad de los criterios de detección varió de 84% para “cualquier síntoma” a 3% para la fiebre de 37,8 °C o mayor. El valor predictivo positivo fue bajo para todos los criterios. Conclusiones. El método de detección sistemática en las fronteras mediante la autonotificación de síntomas y la toma de la temperatura presenta limitaciones para impedir que una gripe pandémica entre en un país. Basarse en criterios como “cualquier síntoma” o la tos haría que se investigara a varias personas no infectadas, mientras que algunas personas infectadas pasarían inadvertidas. Si se usaran criterios más específicos como la fiebre, la mayoría de las personas infectadas entrarían en el país a pesar del mecanismo de detección.

  7. [New technologies in minimally invasive surgery training: what do surgeons demand?].

    PubMed

    Sánchez-Peralta, Luisa Fernanda; Sánchez-Fernández, Javier; Pagador, José Blas; Sánchez-Margallo, Francisco Miguel

    2013-01-01

    Antecedentes: las tecnologías de la información y comunicación pueden aportar beneficios a la formación en cirugía de mínima invasión. Objetivo: determinar la manera más adecuada de incluir las tecnologías de la información y comunicación, en particular una plataforma de e-Learning, en un programa de formación presencial. Material y métodos: se realizó una encuesta en línea entre los asistentes al Centro de Cirugía de Mínima Invasión Jesús Usón, con preguntas relativas a las nuevas tecnologías aplicadas a la formación. Con los datos recopilados se efectuó un estudio descriptivo. Resultados: se enviaron 382 cuestionarios y se recibieron 102 (30%) correctamente respondidos. Los medios para formación teórica más empleados en la actualidad en la población estudiada son: visualización de videos quirúrgicos (85-83.3%) y la asistencia a cursos (77-75.5%). Los usuarios consideran útiles las nuevas tecnologías en formación (4.1 ± 0.9) y sobre todo usarían una plataforma de e-Learning personalizada antes y después de asistir a un curso de formación presencial (80-78.4%). Conclusiones: se propone una metodología de recursos didácticos basados en videos quirúrgicos antes y después que los alumnos asistan a un curso de formación presencial, para que mediante la aplicación de esta metodología se mejore y optimice el tiempo que los cirujanos dedican a su formación.

  8. [CAFFEINE INTAKE AND ITS EFFECT ON THE MAXIMAL AEROBIC SPEED CORRIDORS 800 -METER ATHLETES].

    PubMed

    Rosales Soto, Giovanni; Monsálves Álvarez, Matías; Yáñez Sepúlveda, Rodrigo; Durán Agüero, Samuel

    2015-10-01

    Objetivos: comprobar los efectos de la ingesta de cafeína (3 mg/kg-1) y la mejora del tiempo límite hasta el agotamiento de la velocidad aeróbica máxima que podría modificar los niveles de lactato en sangre en corredores de 800 metros lisos. Material y método: el estudio está basado en un diseño experimental, cruzado, aleatorio y ciego. Se evaluaron 7 sujetos (20 ± 3 años, 63 ± 6 kg y 169,1 ± 7 cm) corredores de 800 metros lisos, que debían estar compitiendo al menos durante tres años y estar entre los diez primeros lugares del ranking nacional. Realizaron una prueba de tiempo límite hasta el agotamiento en cinta rodante a la velocidad aeróbica máxima, donde ingirieron una cápsula que podía contener cafeína (3 mg/kg-1) o placebo (sucralosa). Se midió la concentración de lactato en reposo y al final de cada prueba. Resultados: la ingesta de cafeína reflejó un aumento significativo en la duración del tiempo límite en relación al placebo (376 ± 137 - 457 ± 182 s, respectivamente, p < 0,05). En cuanto al lactato sanguíneo, hay diferencia significativa entre la condición de reposo, el placebo y la ingesta de cafeína (p < 0,05). Conclusiones: la utilización de cafeína como ayuda ergogénica, en dosis de 3 mg/kg-1, incrementa significativamente (p < 0,05) el TLIM de la VAM hasta el agotamiento. Este efecto significa una mejora en el rendimiento de los corredores de 800 metros lisos. A su vez, se aprecia un aumento significativo en las concentraciones de lactato, que podrían hacer referencia al aumento en la intensidad de trabajo posterior a la ingesta de cafeína.

  9. [IMPACT OF DIETARY FATTY ACIDS ON LIPID PROFILE, INSULIN SENSITIVITY AND FUNCTIONALITY OF PANCREATIC β CELLS IN TYPE 2 DIABETIC SUBJECTS].

    PubMed

    Sambra Vásquez, Verónica; Rojas Moncada, Pamela; Basfi-Fer, Karen; Valencia, Alejandra; Codoceo, Juana; Inostroza, Jorge; Carrasco, Fernando; Ruz Ortiz, Manuel

    2015-09-01

    Introducción: la calidad de las grasas podría influir en el control metabólico de los sujetos con diabetes mellitus tipo 2 (DM2). Objetivos: determinar la relación entre la ingesta y la calidad de los ácidos grasos de la dieta con el perfil lipídico, el control metabólico, la funcionalidad de las células pancreáticas y la sensibilidad a la insulina en sujetos con DM2. Métodos: se estudió a 54 sujetos con DM2, se realizaron determinaciones antropométricas, de composición corporal e ingesta dietética de lípidos, ácidos grasos saturados (AGS), trans, monoinsaturados, poliinsaturados, omega 3, omega 6 y colesterol dietario. Se determinaron los parámetros de laboratorio relacionados con el control metabólico (glicemia de ayuno, hemoglobina glicada, perfil lipídico). La secreción de insulina y la sensibilidad a la insulina se determinaron con el test intravenoso de tolerancia a la glucosa modificado con insulina, basado en el modelo mínimo de Bergman. Resultados: se estudió a 28 hombres y 26 mujeres (edad 55,6 ± 6,8 años; IMC 29,5 ± 3,7 kg/m2). Un 48% presentaba c-LDL < 100 mg/dl, el 12,9% de los hombres c-HDL > 40 mg/dl y el 7,4% de las mujeres c-HDL > 50 mg/dl. El 32% consumía > 10% de AGS y > 300 mg/día de colesterol dietario. La ingesta de AGS y el porcentaje de calorías grasas (G%) mostraron una asociación positiva significativa con la resistencia a la insulina y la glicemia. El G% predice en un 84% la variabilidad del c-VLDL. Conclusiones: en los sujetos con DM2, una mayor ingesta de AGS y de grasas se asocia con valores superiores de glicemia y de resistencia a la insulina.

  10. ACCEPTANCE OF FUNCTIONAL FOOD AMONG CHILEAN CONSUMERS: APPLE LEATHER.

    PubMed

    van Vliet, Maya; Adasme-Berrios, Cristian; Schnettler, Berta

    2015-10-01

    Objetivo: el objetivo de este estudio es medir la aceptación de un alimento funcional como la lámina frutal de manzana, en base a características organolépticas. Se identificaron tipos de consumidores y sus preferencias hacia los aditivos naturales que aumentan la funcionalidad del producto y satisfacen las necesidades nutricionales actuales. Materiales y método: una muestra de 800 consumidores permitió la evaluación de la lámina frutal de manzana en términos de aceptación (gusto). se llevó a cabo un panel sensorial utilizando una escala hedónica de nueve puntos. Se utilizó el análisis de conglomerados para establecer diferentes tipos de consumidores, basados en la aceptación del producto. Además, el análisis conjunto permitió determinar la preferencia sobre diferentes aditivos. Resultados: el análisis de conglomerados permitió identificar cuatro grupos con diferencias significativas en los gustos promedios, obtenidos del panel sensorial. Los resultados indican que el dulzor de la lámina frutal de manzana fue mejor evaluada entre todos los grupos y, en promedio, el color fue calificado como el peor atributo. Además, a pesar de que existe una “aceptabilidad global” por el producto, existen diferencias significativas entre los grupos. Los resultados del análisis conjunto indican que, en general, los consumidores prefieren la agregación de aditivos naturales que aumentan la funcionalidad del producto. Conclusiones: en este estudio, la lámina frutal de manzana como alimento funcional se ajusta con el hábito de las personas de consumir alimentos dulces, lo que promueve su aceptación. Además, la agregación de aditivos naturales al producto, tales como anticariogénicos y antioxidantes, permite considerarlo como un alimento funcional sustituto de los snacks, poco saludables y/o de los caramelos.

  11. La implantacion del enfoque constructivista en el aula de ciencia: Estudio de caso multiple

    NASA Astrophysics Data System (ADS)

    Arroyo Betancourt, Luz I.

    participantes basado en lo que estas manifestaron en su practica didactica. Dos maestras coinciden en una vision constructivista social de la construccion del conocimiento, del aprendizaje y de los metodos didacticos. La otra manifesto una vision constructivista piagetiana en el aprendizaje, los metodos didacticos y en la construccion del conocimiento. Se espera que este trabajo, ademas de promover los estudios de caso sobre el enfoque constructivista de ensenanza en el contexto puertorriqueno, sirva para que los maestros, que estan transformando su enfoque educativo de uno tradicional a uno constructivista, tengan una vision mas clara de la implantacion de este enfoque. Se espera ademas que sirva para que el Departamento de Educacion y sus programas de adiestramiento y readiestramiento en servicio, asi como las universidades y sus programas de preparacion de maestros, tomen en cuenta los resultados y recomendaciones de este estudio al revisar sus programas.

  12. HOSPITAL NUTRITIONAL CARE: PROPOSITIONS ENDORSED BY THE SCIENTIFIC COMMUNITY.

    PubMed

    Diez-Garcia, Rosa Wanda; Zangiacomi Martinez, Edson; Penaforte, Fernanda Rodrigues de Oliveira; Japur, Camila Cremonezi

    2015-09-01

    Antecedentes/objetivos: la incidencia de desnutrición hospitalaria y sus consecuencias tanto para el paciente como para el hospital ha exigido procedimientos que aseguren un servicio de atención nutricional hospitalaria de buena calidad. Basado en los informes de la literatura, este estudio tuvo como objetivo construir proposiciones sobre los cuidados nutricionales hospitalarios, que después fueran evaluados y aprobados por la comunidad científica. Métodos: fueron desarrolladas cuarenta y una proposiciones relativas a la atención nutricional clínica del paciente y a la gestión del servicio de alimentación por el Servicio de Alimentación y Nutrición Hospitalaria. Un total de cien profesionales, investigadores y profesores evaluaron las proposiciones. Para analizar si los evaluadores estaban de acuerdo con las proposiciones se utilizó una escala Likert de cinco puntos (estoy en total desacuerdo, estoy parcialmente en desacuerdo, no tengo opinión, estoy parcialmente de acuerdo, estoy totalmente de acuerdo) asociada a cada proposición. Fue considerada concordancia cuando el 70% o más de los evaluadores estaban de acuerdo (totalmente o parcialmente) con la proposición. Para el análisis estadístico fue utilizado el procedimiento Proc Corresp del software SAS 10, versión 8, estadística descriptiva y análisis de correspondencias. Resultados: más del 90% de los entrevistados estaban total o parcialmente de acuerdo con el 85% (35) de las 41 proposiciones; entre el 80 y 90% de los entrevistados estaban total o parcialmente de acuerdo con el 15% (6) de las 41 proposiciones. Todos los criterios propuestos tuvieron más del 70% de concordancia (total y parcial). El menor valor de concordancia total fue del 70%, atribuido a la proposición que sugiere la participación del paciente en la intervención nutricional. Conclusiones: la comunidad científica presentó alto nivel de concordancia con las proposiciones para la atención nutricional hospitalaria, lo

  13. [Medicines reconciliation at hospital admission into an electronic prescribing program].

    PubMed

    Villamayor-Blanco, Lucía; Herrero-Poch, Leticia; De-Miguel-Bouzas, Jose Carlos; Freire Vazquez, M Carmen

    2016-09-01

    Objetivo: Describir y analizar los resultados obtenidos durante un año con un nuevo procedimiento de conciliación de la medicación al ingreso hospitalario basado en un programa de prescripción electrónica asistida. Método: Estudio observacional, prospectivo, no aleatorizado y no controlado de 12 meses de duración, en el que se incluyeron todos los pacientes que ingresaron, durante ese año, en un hospital general concertado de 450 camas. Para la conciliación de la medicación se utilizó el programa de prescripción electrónica como medio para el abordaje multidisciplinar (enfermería, médicos y farmacéuticos). La conciliación se realizó al ingreso hospitalario y se midieron los errores de conciliación. Resultados: Se incluyeron 23.701 pacientes, conciliándose 53.920 medicamentos, de los cuales no tenían discrepancias 48.744 (90,4%) y 5.176 (9,6%) presentaban discrepancias: 4.731 (8,8 % de los fármacos) justificadas y 445 (0,8% de los fármacos) no justificadas. La mayor parte de las discrepancias no justificadas, (n = 310; 69,7%) se debieron a errores en el registro de la medicación domiciliaria al ingreso: medicación no registrada o errores de medicamentos, dosis, frecuencia o vía de administración, omisiones de prescripción, 23,6% (n = 105) y duplicidades, 6,7% (n = 30). En ningún caso el error de conciliación llegó al paciente. Conclusiones: Mediante las ayudas informáticas incluidas en el programa de prescripción electrónica asistida y el abordaje multidisciplinar del proceso de conciliación se consigue realizar la conciliación de la medicación al ingreso en el 98% de los pacientes en el momento del ingreso, evidenciando errores de conciliación solo en el 1,3% de los pacientes.

  14. [ANTHROPOMETRIC PROPORTIONALITY METHOD ELECTION IN A SPORT POPULATION; COMPARISON OF THREE METHODS].

    PubMed

    Almagià, Atilio; Araneda, Alberto; Sánchez, Javier; Sánchez, Patricio; Zúñiga, Maximiliano; Plaza, Paula

    2015-09-01

    Introducción: la aplicación de modelos de proporcionalidad, basados en proporciones ideales, tendría un gran impacto en el deporte de alto rendimiento, debido a que los mejores deportistas tienden a asemejarse antropométricamente. Objetivo: el objetivo de este estudio es comparar los métodos de proporcionalidad antropométrica: Phantom, Combinado y Escalable, en los campeones chilenos de fútbol masculino universitario de los años 2012 y 2013, ocupando como población de criterio a futbolistas profesionales sudamericanos, con el fin de encontrar el método de proporcionalidad más adecuado para poblaciones de deportistas. Metodología: se realizó la evaluación de 22 variables kineantropométricas, según el protocolo ISAK, a una muestra constituida por 13 jugadores pertenecientes a la selección masculina de fútbol de la Pontificia Universidad Católica de Valparaíso. Se obtuvieron los valores Z de cada variable antropométrica de los diferentes métodos, usando sus fórmulas respectivas. Se usó como población de criterio a los futbolistas profesionales sudamericanos. Resultados: se observó una tendencia semejante entre los tres métodos. Se encontraron diferencias significativas (p < 0,05) en los valores Z de los métodos Escalable y Combinado, respecto al método Phantom. No se encontraron diferencias significativas entre los resultados obtenidos por los métodos Combinado y Escalable, excepto en los perímetros radiocarpiano, cadera y muslo. Conclusión: se propone la utilización del método Escalable sobre el método Combinado y Phantom para realizar la comparación de valores Z en variables kineantropométricas en deportistas de la misma disciplina.

  15. Blood lipid profile and glucose of university students (China).

    PubMed

    Liang, Wei; Wang, Linghong; Guo, Daoxia; Nie, Zhognhua; Chen, Yan; Jin, Yuelong; He, Lianping; Yao, Yingshui

    2015-05-01

    Objetivo: El objetivo principal de este estudio fue estimar la glucosa de la sangre y el perfil lípido de la sangre de estudio en una universidad en China. Métodos: Estudio descriptivo basado en la revision de salud; datos para estudiantes universitarios en 2013. La glucosa en la sangre (GLU), perfiles de lípidos (colesterol total (CT), triglicéridos (Tg) y lipoproteína de alta densidad (HDL - c) se midió utilizando Hitachi modelo 747 Analizador automático. Los valores de colesterol LDL se calculan según la fórmula: C - LDL HDL - C = TC Ching Ching TG / 5. Resultados: La media de HDL fueron 51,31 y 56.30 mg / dl para varón y mujer, respectivamente (p < 0,05) y LDL (p < 0.05). La mayoría de los estudiantes tienen nivel normal de Glu (65-110mgl / dl). TC y LDL elevados fueron observados en 6.92% y el 5,82% de varones, asimismo, 5,91% y el 3,57% de mujeres. Altos niveles de TC, LDL y TG fueron detectados en estudiantes universitarios masculinos; 1.02% 0,71% y un 1,41%, respectivamente; en mujeres estudiantes de la Universidad were1.26%, 1.04 y 0,68%, respectivamente. La reducción de los niveles de HDL fueron observados en 5.59% de hombres y el 2,62% de mujeres. Conclusión: El estudio demostró que la prevalencia de la glucosa de la sangre y de lípidos en sangre en los estudiantes universitarios, especialmente la reducción de los niveles de HDL y LDL elevados de TC y en estudiantes universitarios, se ha convertido en un problema de salud crítico. Colegios, escuelas y el Gobierno deben prestar más atención a la salud física de los estudiantes.

  16. [Tasks, roles and expectations of safety practitioners at free-standing occupational health and safety services in Spain].

    PubMed

    Boix Ferrando, Pere; Gil Alcamí, Josep; Velarde Collado, José María; García, María Inés; Daniou Vargas, Ximena

    2013-01-01

    Objetivos: Conocer las actividades profesionales que realizan habitualmente los prevencionistas y su grado de satisfacción con las mismas. Métodos: Se accedió a una muestra de 236 técnicos de prevención con actividad en servicios de prevención ajenos de las comunidades autónomas de Baleares, Andalucía y Madrid a los que se les administró un cuestionario entre noviembre de 2009 y mayo de 2011 basado en el cuestionario propuesto por la Asociación Internacional de la Seguridad Social y la Red Europea de Organizaciones Profesionales en Salud y Seguridad (ISSA-ENSHPO). Resultados: Las tareas más frecuentemente realizadas por los prevencionistas en nuestra muestra (80% o más las realizan como mínimo una vez al mes) son la evaluación de riesgos, la formulación de recomendaciones preventivas, la información y la formación. Algunas tareas, como la fijación de criterios de selección del personal o la realización de análisis coste-beneficio, son mayoritariamente (por más del 50% de los encuestados) consideradas como impropias de los profesionales de la prevención. Los encuestados desearían dedicar más tiempo a la mayoría de las tareas que llevan a cabo, especialmente a las relacionadas con la propia formación y con la interacción en el seno de la empresa. Conclusiones: En el patrón de actividad de los profesionales entrevistados predominan las tareas relacionadas con el asesoramiento técnico en el puesto de trabajo, la formación de trabajadores y la difusión de informaciones, siendo los ámbitos de la gestión del propio conocimiento y el de las relaciones humanas en la empresa los que generan un deseo de mayor dedicación.

  17. Manual del McVCO 1999

    USGS Publications Warehouse

    McChesney, P.J.

    1999-01-01

    El McVCO es un generador de frecuencias basado en un microcontrolador que reemplaza al oscilador controlado por voltaje (VCO) utilizado en telemetría analógica de datos sísmicas. Acepta señales de baja potencia desde un sismómetro y produce una señal subportadora modulada en frecuencia adecuada para enlaces telefónicos o vía radio a un lugar remoto de recolección de datos. La frecuencia de la subportadora y la ganancia pueden ser seleccionadas mediante un interruptor. Tiene la opción de poder operar con dos canales para la observación con ganancia alta y baja. El McVCO fue diseñado con el propósito de mejorar la telemetría analógica de las señales dentro de la Pacific Northwest Seismograph Network (PNSN) (Red Sismográfica del Noroeste del Pacífico). Su desarrollo recibió el respaldo del Programa de Geofísica de la Universidad de Washington y del "Volcano Hazards and Earthquake Hazards programs of the United States Geological Survey (USGS) (Programa de Investigaciones de Riesgos Volcánicos y Programa de Investigaciones de Riesgos Sísmicos de los EEUU). Cientos de instrumentos se han construido e instalado. Además de utilizarlo el PNSN, el McVCO es usado por el Observatorio Vulcanológico de Alaska para monitorear los volcanes aleutianos y por el USGS Volcano Disaster Assistance Program (Programa de Ayuda en las Catástrofes Volcánicas del USGS) para responder a crisis volcánicas en otros países. Este manual cubre el funcionamiento del McVCO, es una referencia técnica para aquellos que necesitan saber con más detalle cómo funciona el McVCO, y cubre una serie de temas que requieren un trato explícito o que derivan del despliegue del instrumento.

  18. ANTHROPOMETRIC PROFILE AND NUTRITIONAL INTAKE IN PATIENTS WITH EPILEPSY.

    PubMed

    de Azevedo Fernandez, Rochelly; Corrêa, Camila; Muxfeld Bianchim, Marino; Schweigert Perry, Ingrid D

    2015-08-01

    Introducción: la calidad de vida alterada es común en los pacientes con epilepsia, especialmente debido a las comorbilidades cardiovasculares, el sobrepeso y la obesidad. Objetivos: evaluar el estado nutricional de los pacientes con epilepsia en base a mediciones antropométricas y la ingesta alimentaria. Métodos: este estudio transversal involucró a 72 pacientes reclutados por conveniencia en la Clínica de Epilepsia del Hospital de Clínicas de Porto Alegre, Brasil. La muestra consistió en pacientes de ambos sexos, mayores de 18 años, que habían sido diagnosticados de epilepsia durante al menos un año. Variables investigadas: medidas antropométricas (peso y talla para la evaluación del estado nutricional y el IMC, circunferencia de la cintura para la evaluación del riesgo cardiovascular); la ingesta nutricional en base a un cuestionario de frecuencia de alimentos; nivel socioeconómico basado en los Criterios de Clasificación Económica del Brasil. Resultados: la prevalencia de sobrepeso/obesidad fue del 66,7%, y el 85,4% de las mujeres tenían un alto riesgo cardiovascular. Los pacientes presentaron una baja frecuencia de control de las crisis (41,7%), alta ingesta de carbohidratos y proteínas, así como baja ingesta de ácidos grasos mono y poliinsaturados (incluyendo ácidos grasos omega 3 y 6). No se observaron diferencias en el estado nutricional ni el consumo entre los pacientes con convulsiones controlados o no controlados. Conclusiones: los pacientes con epilepsia tienen riesgos de comorbilidades, como se evidencia por su tendencia al sobrepeso/obesidad y obesidad abdominal. Aunque el control de las crisis no parece estar relacionado con el estado nutricional y la ingesta, la presencia de tales comorbilidades apunta la necesidad de vigilancia nutricional e intervención en estos pacientes, con un enfoque especial en la redistribución de macronutrientes y en los niveles de ácidos grasos en la dieta.

  19. [Predictor variables for low adherence to a lifestyle modification program of overweight treatment in primary health care].

    PubMed

    Arrebola Vivas, Emilia; López Plaza, Bricia; Koester Weber, Thabata; Bermejo López, Laura; Palma Milla, Samara; Lisbona Catalán, Arturo; Gómez-Candela, Carmen

    2013-01-01

    Objetivos: Identificar variables predictoras de baja adherencia a un programa piloto de Modificación de Estilos de Vida (MEV) para el tratamiento del exceso de peso en Atención Primaria (AP). Material y métodos: Se reclutaron 60 sujetos con IMC > 27 kg/m(2). Profesionales sanitarios dirigieron el programa, en formato grupal y con una periodicidad quincenal, basado en educación nutricional, pautas dietéticas individualizadas, promoción de actividad física y apoyo motivacional. Para identificar las variables relacionadas con la adherencia al programa se utilizó un cuestionario validado sobre Hábitos de Vida de personas con Sobrepeso y Obesidad y se midieron variables antropométricas al inicio y a los seis meses del tratamiento. Una baja adherencia al programa fue considerada cuando los sujetos del estudio acudían a menos del 80% de las visitas quincenales. Resultados: Se adhirieron al programa 27 sujetos (45%). Las variables asociadas a baja adherencia estuvieron relacionadas al inicio del estudio con IMC ≥?35 kg/m(2) (p < 0,05); período de exfumador =?4 meses (p < 0,01); mayor contenido calórico de la dieta (p < 0,01) y menor práctica de ejercicio físico (p < 0,05). A los 6 meses los sujetos que finalizaron el programa presentaron una disminución significativa de: peso (86,0 ± 15,6 vs 79,2 ± 13,4 kg; p < 0,001);% de masa grasa (41,6 ± 4,6 vs 38,8 ± 5,4%; p < 0,001) y glucemia (108 ± 45,48 vs 94,38 ± 11,97 mg/dl; p < 0,01). Además mejoró el perfil calórico de su dieta, disminuyendo sobretodo el porcentaje de grasa sobre el valor calórico total (39,6 ± 4,8 vs. 35,5 ± 5,6%; p < 0,01). Conclusión: Haber dejado de fumar recientemente, padecer obesidad de grado dos o superior, el alto contenido calórico de la dieta y la menor práctica de ejercicio físico fueron las variables basales identificadas como predictoras de una baja adherencia a un programa de MEV para el tratamiento de sobrepeso y obesidad en AP. Esta experiencia piloto una vez

  20. [Validation of an instrument to measure food practices in Chilean families of school children aged 4-7 years].

    PubMed

    Lera, Lydia; Salinas, Judith; Fretes, Gabriela; Vio, Fernando

    2013-11-01

    Introducción: Para enfrentar el problema de la obesidad infantil, es necesario evaluar prácticas alimentarias en familias de escolares. Objetivo: Elaborar y validar un instrumento para medir actitudes, conocimientos y hábitos alimentarios en familias chilenas de escolares de prebásica y básica basado en las guías alimentarias. Métodos: Se realizó un estudio piloto en 30 padres de escolares de prebásica y básica. Se diseñó un cuestionario por los investigadores del estudio considerando la opinión de un grupo de expertos, para medir actitudes, conocimientos hábitos alimentarios en los padres de los escolares. Para la validación del cuestionario, se aplicó en 2 ocasiones, con 15 días de intervalo y se evaluó estabilidad temporal, consistencia interna y concordancia inter-observadores. Posteriormente se aplicó a una muestra de 59 padres y se calculó la consistencia interna del instrumento. Resultados: El cuestionario quedó conformado por 55 preguntas, agrupadas en 4 secciones. Se encontró una buena concordancia inter-observadores para casi todas las preguntas de la sección conocimientos en alimentación y hábitos alimentarios (0,5-1,0). La correlación entre la primera aplicación y la segunda (test-retest) fue elevada (0,6-1,0), así como la consistencia interna (0,75). En la sección frecuencia de consumo del padre y en la de alimentación del niño en el hogar y colegio, la consistencia interna para los dos observadores fue elevada (0,85-0,87; 0,92-0,90; respectivamente). Conclusiones: El instrumento es útil y válido para ser aplicado en familias de escolares de prebásica y básica intervenidas con educación nutricional y esta metodología puede ser replicada en estudios similares.

  1. Physiopathology and treatment of critical bleeding: a literature review.

    PubMed

    González Guerrero, Celia; Montoro Ronsano, José Bruno

    2015-11-01

    Objetivos: desarrollar los factores implicados en la fisiopatología de la coagulopatía asociada al traumatismo (CAT) mediante una revisión de la literatura publicada al respecto; además de revisar la evidencia disponible sobre el tratamiento de la hemorragia crítica y las recomendaciones de las guías de práctica clínica. Métodos: se ha realizado una búsqueda de la bibliografía publicada sobre la fisiopatología y tratamiento de la hemorragia crítica en las bases de datos PUBMED, BestPractice, UpToDate y la Biblioteca Cochrane Plus. Las principales palabras clave utilizadas para la búsqueda han sido: “early trauma induced coagulopathy”, “mechanisms of early trauma-induced coagulopathy”, “blood transfusión guidelines”, “massive transfusion guidelines” y ”fibrinogen replacement therapy”. Los artículos más clínicamente relevantes han sido seleccionados para la revisión. Conclusiones: la fisiopatología de la coagulopatía asociada al traumatismo se trata de un cuadro más complejo y multifactorial de lo que inicialmente se había aceptado. El tratamiento precoz de la coagulopatía es imprescindible para el manejo inicial de la hemorragia crítica. No obstante, el uso de hemoderivados debería ser racional y basado en una evidencia científica homogénea y de alta calidad. Los principales pilares del tratamiento de la hemorragia crítica son la fluidoterapia, el concentrado de fibrinógeno, el concentrado de complejo protrombínico, el plasma, los concentrados de hematíes o de plaquetas, el ácido tranexámico y el calcio. Su administración debería valorarse en función de las condiciones clínicas de cada paciente.

  2. Intuitive eating: an emerging approach to eating behavior.

    PubMed

    Cadena-Schlam, Leslie; López-Guimerà, Gemma

    2014-10-03

    Introducción: Con la finalidad de tratar la obesidad, los profesionales en salud buscan, por medio de intervenciones dietéticas restrictivas y ejercicio, la pérdida de peso como objetivo principal del tratamiento. Aunque en algunos casos estas intervenciones inducen pérdida de peso a corto plazo, en el largo plazo la eficacia de estos tratamientos es, al menos, cuestionable. Investigaciones recientes han sugerido que los tratamientos dirigidos a la pérdida de peso basados en dietas restrictivas no resultan eficaces a largo plazo e incluso pueden comprometer la salud y el bienestar del paciente. En este sentido, algunos investigadores han considerado cambiar el enfoque del tratamiento de la obesidad a un paradigma centrado en la salud y no en la pérdida de peso. Entre los modelos derivados de este nuevo paradigma, Salud a Cualquier Talla (HAES, por sus siglas en inglés) es uno de los más referenciados. Como componente central de este paradigma se sitúa la ingesta intuitiva, la cual se refiere a la confianza en los mecanismos biológicos para regular la ingesta de alimentos (i.e., las señales internas de hambre y saciedad). Recientemente, la ingesta intuitiva ha ganado reconocimiento, pues se ha asociado a diversos parámetros de bienestar físico y psicológico, además, no se ha observado ningún efecto adverso en pacientes que la practican. Objetivo: El presente artículo revisa el concepto de la ingesta intuitiva, así como la evidencia que sustenta este nuevo enfoque. Además, se discute la implicación de cambiar el enfoque convencional de los tratamientos dietéticos a un paradigma centrado en la salud. Diseño: Revisión Narrativa Conclusiones: A pesar de la necesidad de ampliar la investigación de las intervenciones centradas en la salud, este enfoque podría ser una alternativa más prometedora y realista para el abordaje del sobrepeso y la obesidad que los tratamientos de pérdida de peso convencionales.

  3. [Determination of folate content in ready-to-eat food products].

    PubMed

    Fajardo Martín, Violeta; Alonso-Aperte, Elena; Varela-Moreiras, Gregorio

    2013-01-01

    Introducción: Los productos ready-to-eat, ya cocinados, envasados y refrigerados, son cada vez más consumidos en nuestro país. Sin embargo, no existen estudios que cuantifiquen su disponibilidad comercial, composición e información detallada para poder estimar su impacto sobre las ingestas, particularmente de folatos, en los diferentes grupos de población. Objetivos: La finalidad de este trabajo de investigación ha consistido en conocer la disponibilidad actual de alimentos ready-to-eat de base vegetal y aportar datos sobre el contenido de folato total de los mismos. Métodos: La concentración de folato total se determinó en 17 productos precocinados refrigerados, con ingredientes vegetales, mediante el método microbiológico basado en el crecimiento del Lactobacillus casei subespecie rhamnosus resistente a cloranfenicol. La precisión del procedimiento analítico se comprobó mediante un material de referencia certificado y por una prueba de recuperación con ácido fólico tritiado. Resultados y discusión: El contenido medio de FT varió desde 13,6 hasta 103,8 μg/100 g de peso fresco, siendo superior en hamburguesas vegetales, recetas con garbanzos, guisantes o alcachofas con jamón. Los alimentos se sometieron al tratamiento térmico indicado por el fabricante previo a su consumo, observándose que no existen pérdidas de folatos durante este último procesado. El coeficiente de variación de los duplicados del mismo producto fue inferior al 15%. Conclusiones: Se presentan datos pioneros relativos al análisis de folatos en alimentos ready-to-eat en el mercado español, que ayudarán a evaluar la adecuación de la ingesta de folatos en la población. El contenido de folatos de estos productos, su facilidad de consumo y atractiva presentación, los convierte en fuentes potenciales de la vitamina.

  4. [FOOD SOURCES OF SODIUM: ANALYSIS BASED ON A NATIONAL SURVEY IN COLOMBIA].

    PubMed

    Gaitán Charry, Diego Alejandro; Estrada, Alejandro; Argenor Lozano, Gustavo; Manjarres, Luz Mariela

    2015-11-01

    La ingesta elevada de sodio es un factor de riesgo independiente para el desarrollo de enfermedades cardiovasculares –ECV–. Por este motivo, a nivel global se promueve la implementación de la “reducción de la ingesta de sal/sodio como estrategia para la reducción de las ECV”. Para tal fin es importante identificar las fuentes de sodio en la dieta, lo cual hasta la fecha solo se ha realizado, fundamentalmente, en países desarrollados. Objetivos: identificar los alimentos que más sodio aportan a la dieta de los colombianos, basados en los datos de la Encuesta Nacional de la Situación Nutricional –ENSIN– de Colombia. Además, se pretende determinar el nivel de ingesta de sodio proveniente de alimentos en el país. Métodos: se analizaron datos de 39.413 individuos aparentemente sanos, no gestantes, entre los 2 y los 64 años de edad, obtenidos mediante R24h en la ENSIN. Se determinaron los grupos de alimentos que suponen una fuente de sodio, así como el sodio ingerido a partir de dichos alimentos. Resultados: se reportaron 1.274 alimentos y la agrupación de alimentos se realizó con un total de 95, los cuales aportaron un 72% del sodio total proveniente de los alimentos. Estos últimos se dividieron en 12 grupos. Dentro de estos, el de mayor aporte de sodio a la dieta fue el de productos de panadería (30,5%). El promedio de ingesta de sodio por persona proveniente del total de alimentos, sin adición de sal, fue 816,4 ± 474,1 mg/d. La mediana de la misma variable a nivel nacional fue de 721,0 mg/d (RQ = 476,0-1051,0). La ingesta fue mayor en hombres (784,0 mg/d; RQ = 511,0-1156,0) que en mujeres (665,0 mg/d; RQ = 448,0-953,0); p < 0,001. Conclusión: el presente trabajo identificó las principales fuentes de sodio en la dieta de los colombianos y sugiere la conveniencia de priorizar estrategias para la disminución del contenido de sodio en estos grupos, en especial el grupo de productos de panadería. Igualmente, es necesario tener en cuenta la

  5. ASSESSMENT OF GOOD PRACTICES IN HOSPITAL FOOD SERVICE BY COMPARING EVALUATION TOOLS.

    PubMed

    Macedo Gonçalves, Juliana; Lameiro Rodrigues, Kelly; Santiago Almeida, Ângela Teresinha; Pereira, Giselda Maria; Duarte Buchweitz, Márcia Rúbia

    2015-10-01

    Introducción: por ser un adyuvante al tratamiento médico, la alimentación hospitalaria debe ser producida en adecuadas condiciones higiénicas y sanitarias, considerando qué enfermedades transmitidas por los alimentos afectan con mayor severidad a pacientes hospitalizados e inmunodeprimidos. Objetivos: evaluar la adopción de buenas prácticas en los servicios de alimentación hospitalarios, comparando instrumentos de evaluación. Métodos: la evaluación de las buenas prácticas fue realizada utilizando una lista de verificación conforme la Resolución de Directora Colegiada – RDC n.º 216 de la Agencia Nacional de Vigilancia Sanitaria. Para la interpretación de los ítems listados fueron utilizados los parámetros de la RDC n.º 216 y de la Asociación Brasileña de Empresas de Comidas Colectivas (ABERC). Se aplicó el test exacto de Ficher para analizar si existían diferencias estadísticamente significativas y también fue realizado un análisis de agrupamiento de los datos per el método Unweighted Pair-group using Arithmetic Averages y un estudio de la correlación entre las matrices de disimilitud, objetivando verificar la concordancia entre los dos métodos de diagnóstico. Resultados y discusión: las buenas prácticas fueron clasificadas con valores medios totales superiores al 75% de adecuación, en los dos instrumentos utilizados. Se observaron diferencias estadísticamente significativas entre los servicios y la alimentación evaluados por el instrumento de la ABERC. Los servicios de alimentación hospitalarios, de modo general, presentaron condiciones de buenas prácticas aceptables. Conclusión: la comparación de los instrumentos de interpretación basados en la RDC n.º 216 y ABERC mostró resultados semejantes en ambas clasificaciones.

  6. A clinical approach to the nutritional care process in protein-energy wasting hemodialysis patients.

    PubMed

    Ruperto, Mar; Sánchez-Muniz, Francisco J; Barril, Guillermina

    2014-04-01

    Introducción: Malnutrición/desgaste proteico-energético (DPE)/caquexia son situaciones patológicas complejas frecuentemente infradiagnosticadas o no tratadas hasta en un 75% de los pacientes prevalentes en hemodiálisis (HD). El proceso de atención nutricional (PAN) basado en la evaluación, diagnóstico, intervención y monitorización del estado nutricional es un método que los profesionales de la nutrición utilizan para tomar decisiones en la práctica clínica. Objetivo: Esta revisión examina desde la perspectiva de la práctica clínica nutricional: a) el estado nutricional como factor causante de morbi-mortalidad; b) las características fenotípicas de malnutrición, DPE y caquexia y, c) el PAN con especial énfasis en el soporte nutricional y las nuevas terapias nutricionales y farmacológicas en pacientes en HD. Métodos: Revisión sistemática de la literatura usando las bases científicas electrónicas Pubmed, Science Direct, Scielo, Scopus y Medline. Se incluyeron estudios publicados desde 1990 hasta 2013 que valoraban el estado nutricional y/o el soporte nutricional en pacientes en HD. Resultados: De todos los datos epidemiológicos analizados, el PAN fue el método sugerido para identificar malnutrición/ DPE/caquexia. El soporte nutricional como tratamiento aislado no era capaz de revertir totalmente la malnutrición o el DPE. Nuevas estrategias terapéuticas experimentales incluyendo el uso de estimulantes del apetito, agonistas de grelina, antagonistas MC4-R, esteroides anabólicos, antiinflamatorios y colecalciferol entre otros componentes, están siendo aún evaluados clínicamente. Conclusiones: El estado nutricional es un predictor de morbilidad y mortalidad en pacientes en HD. Malnutrición, DPE y caquexia son términos con implicaciones terapéuticas diferentes. El PAN es una herramienta necesaria para la evaluación y la monitorización nutricional en la práctica clínica habitual. Estudios con nuevas terapias farmacológicas o

  7. Reframing HIV care: putting people at the centre of antiretroviral delivery

    PubMed Central

    Duncombe, Chris; Rosenblum, Scott; Hellmann, Nicholas; Holmes, Charles; Wilkinson, Lynne; Biot, Marc; Bygrave, Helen; Hoos, David; Garnett, Geoff

    2015-01-01

    érisée par quatre éléments de délivrance: (1) les types de services délivrés, (2) l’emplacement de la délivrance des services, (3) Les prestataires des services de santé et (4) la fréquence des services de santé. La façon dont ces éléments sont développés dans un cadre de prestation de services peut varier selon les pays et les populations, l’intention étant d’améliorer les résultats d’acceptabilité et des soins. Le but d’obtenir plus de personnes sous traitement avant qu’ils ne tombent malades nécessitera des modèles innovateurs de prestation à la fois pour dépistage et pour les soins. Comme les programmes VIH étendent l’éligibilité au traitement, beaucoup de gens qui entrent dans les soins ne seront pas des “malades- mais des éléments sains de la société, actifs et productifs. Afin de tenir le cadre à l’échelle, il sera important de: (1) définir les individus qui peuvent être traités par un cadre alternatif de prestation, (2) renforcer les systèmes de santé qui soutiennent la décentralisation, l’intégration et le transfert des tâches; (3) rendre la chaîne d’approvisionnement plus robuste et (4) investir dans des systèmes de données pour le suivi des patients et pour le suivi et l’évaluation du programme. Los servicios de atención del VIH durante el inicio de la primera etapa de rápida expansión del tratamiento y cuidados del VIH estaban basados en modelos clínicos existentes, comunes en lugares con abundancia de recursos y poco diferenciados en cuanto a necesidades individuales. Aquí se propone un nuevo marco para el tratamiento basado en intensidades variables de cuidados, hecho a medida según las necesidades específicas de los diferentes grupos de individuos a lo largo del tratamiento. La intensidad del servicio se caracteriza por cuatro componentes de entrega: (1) tipología de los servicios ofrecidos, (2) lugar de entrega de los servicios, (3) proveedor de los servicios sanitarios, y (4

  8. Reframing HIV care: putting people at the centre of antiretroviral delivery

    PubMed Central

    Duncombe, Chris; Rosenblum, Scott; Hellmann, Nicholas; Holmes, Charles; Wilkinson, Lynne; Biot, Marc; Bygrave, Helen; Hoos, David; Garnett, Geoff

    2015-01-01

    érisée par quatre éléments de délivrance: (1) les types de services délivrés, (2) l’emplacement de la délivrance des services, (3) Les prestataires des services de santé et (4) la fréquence des services de santé. La façon dont ces éléments sont développés dans un cadre de prestation de services peut varier selon les pays et les populations, l’intention étant d’améliorer les résultats d’acceptabilité et des soins. Le but d’obtenir plus de personnes sous traitement avant qu’ils ne tombent malades nécessitera des modèles innovateurs de prestation à la fois pour dépistage et pour les soins. Comme les programmes VIH étendent l’éligibilité au traitement, beaucoup de gens qui entrent dans les soins ne seront pas des “malades- mais des éléments sains de la société, actifs et productifs. Afin de tenir le cadre à l’échelle, il sera important de: (1) définir les individus qui peuvent être traités par un cadre alternatif de prestation, (2) renforcer les systèmes de santé qui soutiennent la décentralisation, l’intégration et le transfert des tâches; (3) rendre la chaîne d’approvisionnement plus robuste et (4) investir dans des systèmes de données pour le suivi des patients et pour le suivi et l’évaluation du programme. Los servicios de atención del VIH durante el inicio de la primera etapa de rápida expansión del tratamiento y cuidados del VIH estaban basados en modelos clínicos existentes, comunes en lugares con abundancia de recursos y poco diferenciados en cuanto a necesidades individuales. Aquí se propone un nuevo marco para el tratamiento basado en intensidades variables de cuidados, hecho a medida según las necesidades específicas de lo

  9. Nucleic-acid characterization of the identity and activity of subsurface microorganisms

    NASA Astrophysics Data System (ADS)

    Madsen, E. L.

    pour obtenir des données, de nombreuses futures occasions sont dans l'attente d'explorations. Los métodos basados en ácidos nucleicos para la caracterización de microorganismos en sus propios hábitats han experimentado un gran auge en la última década. La extracción directa en muestras de los biomarcadores ácido desoxirribonucleico (ADN) y ribonucleico (ARN) supone un nuevo método para obtener información sobre ecología microbiana. En este articulo se definen: (1) el nuevo métidi para obtener información sobre ecología microbiana. En este artículo se definen: (1) el hábitat subsuperficial; (2) qué son los métodos basados en ácidos nucleicos; y (3) la información que estos métodos pueden proporcionar. Se revisa y tabula la bibliografía reciente sobre ácidos nucleicos microbianos en la subsuperficie. Hasta ahora la mayoría de estos estudios se han centrado en la identificación y filogenia de los microorganismos, mediante el análisis de sus genes 16S rRNA. Dado el potencial de las técnicas basadas en ácidos nucleicos y el hecho de que hasta ahora su aplicación a los hábitats subsuperficiales haya sido limitada, se presentan muchas opotunidades de futuro.

  10. Tsunami prevention and mitigation necessities and options derived from tsunami risk assessment in Indonesia

    NASA Astrophysics Data System (ADS)

    Post, J.; Zosseder, K.; Wegscheider, S.; Steinmetz, T.; Mück, M.; Strunz, G.; Riedlinger, T.; Anwar, H. Z.; Birkmann, J.; Gebert, N.

    2009-04-01

    certain area is dependent on expected tsunami intensity, inundated area, estimated tsunami arrival time and available time for evacuation. Referring to the Aceh 2004 Tsunami, an estimated amount of people affected (dead/injured) of 21000 for Kabubaten Aceh Jaya and 85000 for Kab. Banda Aceh is in a comparable range with reported values of 19661 and 78417 (JICA 2005) respectively. Hence the established methodology provides reliable estimates of people affected and people's ability to reach a safe area. Based on the spatial explicit detection of e.g. high tsunami risk areas (and the assessed root causes therefore), specific disaster risk reduction and early warning strategies can be designed. For example additional installation of technical warning dissemination device, community based preparedness and awareness programmes (education), structural and non-structural measures (e.g. land use conversion, coastal engineering), effective evacuation, contingency and household recovery aid planning can be employed and/or optimized within high tsunami risk areas as a first priority. In the context of early warning, spatially distributed information like degree of expected hazard impact, exposure of critical facilities (e.g. hospitals, schools), potential people dead/injured depending on available response times, location of safe and shelter areas can be disseminated and used for decision making. Keywords: Tsunami risk, hazard and vulnerability assessment, early warning, tsunami mitigation and prevention, Indonesia

  11. Groundwater targeting in a hard-rock terrain using fracture-pattern modeling, Niva River basin, Andhra Pradesh, India

    NASA Astrophysics Data System (ADS)

    Srinivasa Rao, Y.; Reddy, T. V. K.; Nayudu, P. T.

    2000-09-01

    'eau souterraine. Dans la région étudiée, les fractures N35°-55°E ont été identifiées comme étant en extension, et les fractures N35°-55°W comme étant à la fois en extension et en cisaillement. Ces fractures sont apparemment les fractures ouvertes les plus jeunes. Partout où la densité des fractures N35°-55°E et N35°-55°W est élevée, la zone altérée est plus épaisse, les fluctuations de la nappe sont faibles et les rendements des puits sont forts. Des zones à potentiel en eau souterraine ont ainsi été délimitées et classées en excellent, bon à très bon, assez bon et médiocre. Resumen. Las zonas de fracturación y de meteorización son las que condicionan el flujo de agua subterránea en rocas duras, debido a la falta de porosidad primaria en la matriz rocosa. Se utilizaron cinco conjuntos de datos fotográficos del satélite Landsat con el fin de preparar un mapa integrado hidrogeomorfológico de la cuenca del río Niva, al sur del estado Andhra Pradesh (India). El objetivo era estudiar el potencial de aguas subterráneas en esta región, que es propensa a períodos de sequía, en la que predominan las rocas duras. Se aplicó el modelo de deformación integrado de Larsson a la identificación de los sistemas de fracturación. El propósito era, por un lado, identificar los conjuntos de fracturas de tracción más jóvenes, que desempeñan un papel principal como reservorios de aguas subterráneas. Por otro lado, se quería comprender la importancia de la densidad de fracturación en el desarrollo de las aguas subterráneas. Se identificó una familia de fracturas de tracción con orientación N35°-55°E y otra familia N35°-55°W que contenía tanto bandas de cizalla como fracturas de tracción. Aparentemente, se trataba de las fracturas abiertas más recientes. El espesor de la zona de meteorización es grande cuando la densidad de fracturas de estas dos familias es elevada, hecho que está asociado a fluctuaciones pequeñas del nivel freático y

  12. Earthquakes along the Ryukyu-Kyushu Arc: Strain segmentation, lateral compression, and the thermomechanical state of the plate interface

    NASA Astrophysics Data System (ADS)

    Kao, Honn; Chen, Wang-Ping

    1991-12-01

    We systematically determined the focal depths and mechanisms of 49 large to moderate-sized earthquakes (mb≥5.4) that occurred along the Ryukyu-Kyushu arc since 1963 by inverting the waveforms and amplitudes of P and SH wave trains at teleseismic distances. The results are sufficiently precise to delineate seismogenic structures near the plate interface in detail, revealing features not predicted by plate kinematics. In contrast to previous studies of this arc and those along other subduction zones, shallow seismicity along the plate interface is systematic, showing two distinct layers of activities. The second layer of seismicity is delineated by a few earthquakes that occurred at depths between 50 and 65 km, some 10-20 km directly beneath the seismogenic portion of the interplate thrust zone. These earthquakes indicate lateral compressional strain within the subducted slab as their P axes are subparallel to the local strike of the arc, not perpendicular to the arc as one would expect from the direction of plate convergence. The occurrence of these events cannot be accounted for by membrane stress due to the geometry of the subducted slab. To our knowledge, similar earthquakes occurred only beneath the northern Indoburman ranges and along the Banda arc where subducted slabs, as part of the Indian plate, are being dragged northward with their northern edges bumping into east-west trending collision zones nearby. By drawing an analogy between the tectonic settings of these three regions, we interpret events beneath the plate interface along the Ryukyu-Kyushu arc as a consequence of ongoing collision between the Philippine Sea plate and Eurasia near Taiwan. The interplate thrust zone is largely aseismic down to a depth of approximately 30 km. A large number of earthquakes showing low-angle thrust faulting commence at this depth and are accompanied by two events that show antithetic thrust faulting at a slightly shallower depth of 20-25 km. These observations suggest

  13. Causes of sinks near Tucson, Arizona, USA

    NASA Astrophysics Data System (ADS)

    Hoffmann, John P.; Pool, Donald R.; Konieczki, A. D.; Carpenter, Michael C.

    éà 17,000m3 a été entraîné lors de la formation de ces entonnoirs. Treize tranchées ont été creusées à des profondeurs de 4 à 6m afin de caractériser les sédiments proches de la surface dans les zones avec et sans entonnoirs. Les sédiments situés à 2m environ sous la surface contiennent un fort pourcentage d'argile dispersée, dans les zones à entonnoirs. Dans les zones sans entonnoirs, la granulométrie des sédiments est constituée en fortes proportions de sables moyens à grossiers, moyennement à bien lités, qui remplissent probablement un ancien chenal. Des levés électromagnétiques montrent que l'association de silts et d'argiles dans les zones à entonnoirs possède une forte conductivitéélectrique, par comparaison avec les sables des zones sans entonnoirs. Les entonnoirs sont dus probablement à des processus, proches de la surface, d'érosion souterraine des sédiments constitués surtout de silts et d'argiles. Les fractures préexistantes résultent sans doute de la dessiccation ou de la tension se produisant lors des périodes d'abaissement de la nappe, liéà l'enfoncement du lit de la rivière au cours des cent dernières années ou même avant.1 Resumen Se ha detectado la formación de dolinas como resultado de la subsidencia que ha tenido lugar en las zonas agrícolas Condado de Pima, Arizona, EEUU. Estos colapsos han aparecido en depósitos aluviales a lo largo de la llanura de inundación del Río Santa Cruz y han hecho que las zonas agrícolas sean peligrosas e inadecuadas para su uso. Las más de 1700 dolinas aparecidas se agrupan a lo largo de dos bandas con dirección nor-noroeste, paralelas al río y a otros ejes de drenaje del llano. Se ha estimado un desplazamiento de 17.000metros cúbicos de sedimentos para formar estas dolinas. Se excavaron trece zanjas de entre 4 y 6metros para caracterizar los sedimentos más superficiales tanto en áreas colapsadas como no colapsadas. Por debajo de los dos metros de profundidad, los

  14. PFI-ZEKE (Pulsed Field Ionization-Zero Electron Kinetic Energy) para el estudio de iones

    NASA Astrophysics Data System (ADS)

    Castaño, F.; Fernández, J. A.; Basterretxea, A. Longarte. F.; Sánchez Rayo, M. N.; Martínez, R.

    Entre las áreas hacia donde ha evolucionado la Química en los últimos años están los estudios de sistemas con especies reactivas de alta energía y los dominados por fuerzas intermoleculares débiles, con energías de unas pocas kcal/mol. En efecto, el estudio de las propiedades de los iones, comenzando por su relación con la molécula neutra de la que procede, la energía de ionización, los estados vibracionales y rotacionales, energías de enlace de Van der Waals entre el ión y una amplia variedad de otras moléculas, sus confórmeros o isómeros y sus reacciones o semi-reacciones químicas están en la raíz de la necesidad de la espectroscopía conocida como PFI-ZEKE, Pulsed Field Ionization-Zero Electron Kinetic Energy. Entre las aplicaciones que requieren estos conocimientos se encuentran la generación de plasmas para la fabricación de semiconductores, memorias magnéticas, etc, así como los sistemas astrofísicos, la ionosfera terrestre, etc. La espectroscopía ZEKE es una evolución de las de fluorescencia inducida por láser, LIF, ionización multifotónica acrecentada por resonancia, REMPI, con uno y dos colores y acoplada a un sistema de tiempo de vuelo, REMPI-TOF-MS, y las espectroscopías de doble resonancia IR-UV y UV-UV. Sus espectros y la ayuda de cálculos ab inicio permite determinar las energías de enlace de complejos de van der Waals en estados fundamental y excitados, identificar confórmeros e isómeros, obtener energías de ionización experimentales aproximadas (100 cm-1) y otras variables de interés. Al igual que con LIF, REMPI y dobles resonancias, es posible utilizar muestras gaseosas, pero los espectros están muy saturados de bandas y su interpretación es difícil o imposible. Se evitan estas dificultades estudiando las moléculas o complejos en expansiones supersónicas, donde la T de los grados de libertad solo alcanzan unos pocos K. Para realizar experimentos de ZEKE hay que utilizar una propiedad recientemente

  15. Causes of sinks near Tucson, Arizona, USA

    NASA Astrophysics Data System (ADS)

    Hoffmann, John P.; Pool, Donald R.; Konieczki, A. D.; Carpenter, Michael C.

    éà 17,000m3 a été entraîné lors de la formation de ces entonnoirs. Treize tranchées ont été creusées à des profondeurs de 4 à 6m afin de caractériser les sédiments proches de la surface dans les zones avec et sans entonnoirs. Les sédiments situés à 2m environ sous la surface contiennent un fort pourcentage d'argile dispersée, dans les zones à entonnoirs. Dans les zones sans entonnoirs, la granulométrie des sédiments est constituée en fortes proportions de sables moyens à grossiers, moyennement à bien lités, qui remplissent probablement un ancien chenal. Des levés électromagnétiques montrent que l'association de silts et d'argiles dans les zones à entonnoirs possède une forte conductivitéélectrique, par comparaison avec les sables des zones sans entonnoirs. Les entonnoirs sont dus probablement à des processus, proches de la surface, d'érosion souterraine des sédiments constitués surtout de silts et d'argiles. Les fractures préexistantes résultent sans doute de la dessiccation ou de la tension se produisant lors des périodes d'abaissement de la nappe, liéà l'enfoncement du lit de la rivière au cours des cent dernières années ou même avant.1 Resumen Se ha detectado la formación de dolinas como resultado de la subsidencia que ha tenido lugar en las zonas agrícolas Condado de Pima, Arizona, EEUU. Estos colapsos han aparecido en depósitos aluviales a lo largo de la llanura de inundación del Río Santa Cruz y han hecho que las zonas agrícolas sean peligrosas e inadecuadas para su uso. Las más de 1700 dolinas aparecidas se agrupan a lo largo de dos bandas con dirección nor-noroeste, paralelas al río y a otros ejes de drenaje del llano. Se ha estimado un desplazamiento de 17.000metros cúbicos de sedimentos para formar estas dolinas. Se excavaron trece zanjas de entre 4 y 6metros para caracterizar los sedimentos más superficiales tanto en áreas colapsadas como no colapsadas. Por debajo de los dos metros de profundidad, los

  16. Surge-tectonic evolution of southeastern Asia: a geohydrodynamics approach

    NASA Astrophysics Data System (ADS)

    Meyerhoff, Arthur A.

    The repeated need for ad hoc modifications in plate-tectonic models to explain the evolution of southeastern Asia reveals their inability to fully explain the complex features and dynamics of this region. As one example, the hypothesis does not provide a mechanism to explain the 180° turns and twists along the strike of several foldbelts and island arcs in the region (e.g. Banda arc). Convection-cell configuration renders such 180° contortions and Rayleigh-Bénard-type convection impossible. However, during the last 10 years, new data bearing on the convection-cell problem have become available in the form of seismotomographic images of the earth's interior. These images show that (i) mantle diapirs as proposed by traditional plate-tectonic models do not exist; (ii) there is no discernible pattern of upper or lower mantle convection, and thus no longer an adequate mechanism to move plates; and (iii) the lithosphere above a depth of about 80 km is permeated by an interconnected network of low-velocity channels. Seismic-reflection studies of the low-velocity channels discovered on the seismotomographic images reveal that these channels have walls with a 7.1-7.8 km s -1 P-wave velocity. Commonly, the interiors of the channels are acoustically transparent, with much slower P-wave velocities, in places as low as 5.4 km s -1. The author and co-workers have interpreted the low velocities as evidence for the presence of partial melt in the channels, and they postulated that this melt moves preferentially eastward as a result of the earth's rotation. They named these channels "surge channels" and their new hypothesis for earth dynamics "surge tectonics". Surge channels underlie every type of tectonic belt, which includes mid-ocean ridges, aseismic ridges, continental rifts, strike-slip fracture zones, and foldbelts. In southeastern Asia, surge channels—mainly foldbelts—lie between all platform and cratonic massifs. These massifs, platforms, and tectonics belts

  17. Groundwater targeting in a hard-rock terrain using fracture-pattern modeling, Niva River basin, Andhra Pradesh, India

    NASA Astrophysics Data System (ADS)

    Srinivasa Rao, Y.; Reddy, T. V. K.; Nayudu, P. T.

    2000-09-01

    'eau souterraine. Dans la région étudiée, les fractures N35°-55°E ont été identifiées comme étant en extension, et les fractures N35°-55°W comme étant à la fois en extension et en cisaillement. Ces fractures sont apparemment les fractures ouvertes les plus jeunes. Partout où la densité des fractures N35°-55°E et N35°-55°W est élevée, la zone altérée est plus épaisse, les fluctuations de la nappe sont faibles et les rendements des puits sont forts. Des zones à potentiel en eau souterraine ont ainsi été délimitées et classées en excellent, bon à très bon, assez bon et médiocre. Resumen. Las zonas de fracturación y de meteorización son las que condicionan el flujo de agua subterránea en rocas duras, debido a la falta de porosidad primaria en la matriz rocosa. Se utilizaron cinco conjuntos de datos fotográficos del satélite Landsat con el fin de preparar un mapa integrado hidrogeomorfológico de la cuenca del río Niva, al sur del estado Andhra Pradesh (India). El objetivo era estudiar el potencial de aguas subterráneas en esta región, que es propensa a períodos de sequía, en la que predominan las rocas duras. Se aplicó el modelo de deformación integrado de Larsson a la identificación de los sistemas de fracturación. El propósito era, por un lado, identificar los conjuntos de fracturas de tracción más jóvenes, que desempeñan un papel principal como reservorios de aguas subterráneas. Por otro lado, se quería comprender la importancia de la densidad de fracturación en el desarrollo de las aguas subterráneas. Se identificó una familia de fracturas de tracción con orientación N35°-55°E y otra familia N35°-55°W que contenía tanto bandas de cizalla como fracturas de tracción. Aparentemente, se trataba de las fracturas abiertas más recientes. El espesor de la zona de meteorización es grande cuando la densidad de fracturas de estas dos familias es elevada, hecho que está asociado a fluctuaciones pequeñas del nivel freático y

  18. Surge-tectonic evolution of southeastern Asia: a geohydrodynamics approach

    NASA Astrophysics Data System (ADS)

    Meyerhoff, Arthur A.

    The repeated need for ad hoc modifications in plate-tectonic models to explain the evolution of southeastern Asia reveals their inability to fully explain the complex features and dynamics of this region. As one example, the hypothesis does not provide a mechanism to explain the 180° turns and twists along the strike of several foldbelts and island arcs in the region (e.g. Banda arc). Convection-cell configuration renders such 180° contortions and Rayleigh-Bénard-type convection impossible. However, during the last 10 years, new data bearing on the convection-cell problem have become available in the form of seismotomographic images of the earth's interior. These images show that (i) mantle diapirs as proposed by traditional plate-tectonic models do not exist; (ii) there is no discernible pattern of upper or lower mantle convection, and thus no longer an adequate mechanism to move plates; and (iii) the lithosphere above a depth of about 80 km is permeated by an interconnected network of low-velocity channels. Seismic-reflection studies of the low-velocity channels discovered on the seismotomographic images reveal that these channels have walls with a 7.1-7.8 km s -1 P-wave velocity. Commonly, the interiors of the channels are acoustically transparent, with much slower P-wave velocities, in places as low as 5.4 km s -1. The author and co-workers have interpreted the low velocities as evidence for the presence of partial melt in the channels, and they postulated that this melt moves preferentially eastward as a result of the earth's rotation. They named these channels "surge channels" and their new hypothesis for earth dynamics "surge tectonics". Surge channels underlie every type of tectonic belt, which includes mid-ocean ridges, aseismic ridges, continental rifts, strike-slip fracture zones, and foldbelts. In southeastern Asia, surge channels—mainly foldbelts—lie between all platform and cratonic massifs. These massifs, platforms, and tectonics belts

  19. [Software for performing a global phenotypic and genotypic nutritional assessment].

    PubMed

    García de Diego, L; Cuervo, M; Martínez, J A

    2013-01-01

    Antecedentes: La evaluación nutricional del paciente requiere del manejo simultáneo de una extensa información y de numerosas bases de datos, ya que se analizan tanto aspectos relacionados con el proceso de la nutrición como la situación y evolución clínica del paciente. Con la introducción de la informática dentro del ámbito nutricional se ha producido un avance extraordinario en la administración de la información, permitiendo la realización de valoraciones exhaustivas del estado nutricional de forma rápida y sencilla. Objetivo: Desarrollar un programa informático que sirva como instrumento para la evaluación del estado nutricional del paciente, la educación del personal clínico, en estudios epidemiológicos y con fines pedagógicos. Diseño: Un programa informático que ayude al especialista de la salud a realizar una evaluación nutricional completa del paciente, mediante el registro y valoración de las características fenotípicas y genotípicas. La aplicación ofrece pronósticos nutricionales basados en parámetros antropométricos y bioquímicos, imágenes de estados de desnutrición, cuestionarios de caracterización de enfermedades, criterios de diagnóstico, identificación de alelos relacionados con el desarrollo de ciertas enfermedades metabólicas y cuestionarios de calidad de vida, para una actuación personalizada. El programa incluye como parte de la valoración nutricional del paciente el análisis de la ingesta alimentaria, la elaboración de dietas y la promoción de la actividad física, introduciendo cuestionarios de frecuencia alimentaria, recordatorios dietéticos, índices de alimentación saludable, dietas modelo, test de condición física así como recomendaciones, recordatorios y cuestionarios de actividad física. Resultado: Un programa informático diseñado mediante el lenguaje de programación Java Swing, usando la base de datos SQLite y algunas librerías externas como JFreeChart para el diseño de gr

  20. A protocol for eliciting nonmaterial values through a cultural ecosystem services frame

    PubMed Central

    Gould, Rachelle K; Klain, Sarah C; Ardoin, Nicole M; Satterfield, Terre; Woodside, Ulalia; Hannahs, Neil; Daily, Gretchen C; Chan, Kai M

    2015-01-01

    Servicios Ambientales Culturales Resumen Los deseos, necesidades y valores no materiales de los accionistas influyen frecuentemente sobre el éxito de los proyectos de conservación. Estas consideraciones son difíciles de articular y caracterizar, lo que resulta en entendimiento limitado en el manejo y la política. Concebimos un protocolo de entrevista diseñado para mejorar el entendimiento de los servicios ambientales culturales (SAC). El protocolo inicia con la discusión de actividades relacionadas con ecosistemas (p. ej.: recreación, cacería) y manejo; después señala a los SAC, dando pie a los valores que encierran conceptos identificados en la Evaluación Ambiental del Milenio (2005) y explorado en otras investigaciones sobre SAC. Hicimos pruebas piloto del protocolo en Hawái y Columbia Británica. En cada localidad entrevistamos a 30 individuos de diversos entornos. Analizamos los resultados de las dos localidades para determinar la efectividad del protocolo de entrevista en la obtención de valores no materiales. Los componentes cualitativos y espaciales del protocolo nos ayudaron a caracterizar los valores culturales, sociales y éticos asociados con el ecosistema de múltiples maneras. Los mapas y las preguntas de situación, o de tipo viñeta, ayudaron a los encuestados a articular valores difíciles de discutir. Las preguntas abiertas permitieron a los encuestados expresar una diversidad de valores ambientales y demostraron ser suficientemente flexibles para que los encuestados comunicaran valores que el protocolo no buscaba explícitamente. Finalmente, los resultados sugieren que ciertos valores, aquellos mencionados frecuentemente en la entrevista, son particularmente prominentes para poblaciones particulares. El protocolo puede proporcionar datos eficientes, contextuales y basados en lugar sobre la importancia de atributos ambientales particulares para el bienestar humano. Los datos cualitativos son complementarios para las evaluaciones cuantitativas y

  1. [In Process Citation].

    PubMed

    Molina Recio, Guillermo; Moreno Rojas, Rafael; García Rodríguez, María; Vaquero Abellán, Manuel

    2016-02-16

    Introducción: un gran número de encuestas nutricionales en Perú han identificado la magnitud y la ubicación de los diferentes tipos de desnutrición, siendo la forma crónica la más prevalente. Sin embargo, aunque las tasas pueden considerarse alarmantes (aún más en las zonas rurales), sólo un trabajo contiene información sobre las características de la ingesta, usando recordatorios de 24 horas (R24). Es decir, se carece de otros sistemas de estudio centrados en conocer las características gastronómicas de sus regiones y la biodisponibilidad de los alimentos, con el fin de localizar el origen de esta situación en cada área y proponer soluciones verdaderamente eficaces y eficientes.Objetivo: determinar el valor nutricional de los platos principales consumidos por los residentes de un barrio pobre de la Amazonía Peruana, para identificar las causas de la pérdida de un estado nutricional saludable.Métodos: noventa y ocho participantes completaron tres R24. Basándonos en estos datos, se seleccionaron los 25 platos más comúnmente consumidos y evaluamos su composición nutricional. Tomamos nota de las recetas, pesos y medidas caseras. Además, se observó la preparación y cocción. La composición nutricional media de cada plato se calculó por 100 g utilizando el software Nutriplato 4.6. También se calcularon lasganancias o pérdidas derivadas de los tratamientos culinarios.Resultados: dentro de los platos basados en la leche, el de más alta densidad de energía es el mingado de arroz. En el grupo de los pescados, la mayor cantidad de energía es aportada por el pescado frito, mientras que en las recetas a base de carne, las más energéticas son el tallarín con pollo, la res asada y el cerdo frito. Como platos preparados, el juane tiene la más alta densidad de energía de todas las recetas. Dentro de las guarniciones, aquellas que utilizan los plátanos como el ingrediente principal, el plátano frito y el madurito, son las más energ

  2. Production and quality assurance in the SIT Africa Mediterranean fruit fly (Diptera: Tephritidae) rearing facility in South Africa

    SciTech Connect

    Barnes, B.; Rosenberg, S.; Arnolds, L.; Johnson, J.

    2007-03-15

    esteriles de moscas para el proyecto de la tecnica del insecto esteril (TIE) en huertos de frutos y vinas comerciales en la provincia del Cabo Occidental del Sudafrica. El procedimiento de criar en masa fue en su mayor parte basado en los sistemas desarrollados por el Laboratorio de Agricultura y Biotecnologia de la FAO/IAEA, Seibersdorf, Austria. Un numero de razas que separara los sexos geneticamente fueron utilizadas para producir solo machos para la liberacion. La congestionada condicion inicial para criar las moscas y su manejo de calidad fueron aliviadas en 2001 con la construccion de un nuevo cuarto de cria para adultos y un laboratorio de control de calidad. En 2002, un Sistema de Manejo de Calidad comprensivo fue implementado, y en 2003 una raza mejorada que separa los sexos geneticamente, VIENNA 8, fue proveido por el Laboratorio de la FAO/IAEA en Seibersdorf. En la mayor parte de los primeros 3 anos la facilidad no pudo suplir el numero requerido de machos esteriles de la mosca mediterranea de la fruta para el programa de TIE sin la necesidad para importar machos esteriles de otra facilidad. Desde medio del ano de 2002, despues que el sistema de manejo de calidad fue implementado, la produccion y la calidad mejoraron pero aun quedaron por debajo del nivel optimo. Despues de la introduccion de la raza VIENNA 8 que separa los sexos geneticamente, y junto con el equipo mejorado de control de clima, la estabilidad y los parametros de seguridad de calidad mejoraron substancialmente. Los factores criticos que influyeron en la produccion y la calidad fueron la infraestructura inadecuada para criar las moscas, problemas con la calidad de la dieta para las larvas y la ausencia inicial de un sistema de manejo de calidad. Los resultados muestran claramente la importancia de un manejo efectivo de la calidad, el valor de una raza productiva que separa los sexos geneticamente y la necesidad de contar con una base solida de financimiento para la infraestructura de una cria en

  3. [In Process Citation].

    PubMed

    Molina Recio, Guillermo; Moreno Rojas, Rafael; García Rodríguez, María; Vaquero Abellán, Manuel

    2016-01-01

    Introducción: un gran número de encuestas nutricionales en Perú han identificado la magnitud y la ubicación de los diferentes tipos de desnutrición, siendo la forma crónica la más prevalente. Sin embargo, aunque las tasas pueden considerarse alarmantes (aún más en las zonas rurales), sólo un trabajo contiene información sobre las características de la ingesta, usando recordatorios de 24 horas (R24). Es decir, se carece de otros sistemas de estudio centrados en conocer las características gastronómicas de sus regiones y la biodisponibilidad de los alimentos, con el fin de localizar el origen de esta situación en cada área y proponer soluciones verdaderamente eficaces y eficientes.Objetivo: determinar el valor nutricional de los platos principales consumidos por los residentes de un barrio pobre de la Amazonía Peruana, para identificar las causas de la pérdida de un estado nutricional saludable.Métodos: noventa y ocho participantes completaron tres R24. Basándonos en estos datos, se seleccionaron los 25 platos más comúnmente consumidos y evaluamos su composición nutricional. Tomamos nota de las recetas, pesos y medidas caseras. Además, se observó la preparación y cocción. La composición nutricional media de cada plato se calculó por 100 g utilizando el software Nutriplato 4.6. También se calcularon lasganancias o pérdidas derivadas de los tratamientos culinarios.Resultados: dentro de los platos basados en la leche, el de más alta densidad de energía es el mingado de arroz. En el grupo de los pescados, la mayor cantidad de energía es aportada por el pescado frito, mientras que en las recetas a base de carne, las más energéticas son el tallarín con pollo, la res asada y el cerdo frito. Como platos preparados, el juane tiene la más alta densidad de energía de todas las recetas. Dentro de las guarniciones, aquellas que utilizan los plátanos como el ingrediente principal, el plátano frito y el madurito, son las más energ

  4. Inversor Resonante de Tres Elementos L-LC con Caracteristica Cortocircuitable para Aplicaciones de Calentamiento por Induccion

    NASA Astrophysics Data System (ADS)

    Espi Huerta, Jose Miguel

    Los generadores de calentamiento por induccion son puentes inversores con carga resonante, cuya mision es basicamente crear una corriente sinusoidal de gran amplitud sobre la "bobina de caldeo", que forma parte del tanque resonante. En el interior de esta bobina se introduce la pieza que se desea calentar. EI campo magnetico creado induce corrientes superficiales (corrientes de Foucault) sobre la pieza, que producen su calentamiento. Los tanques resonantes (tambien llamados osciladores) utilizados en la actualidad son el resonante serie y el resonante paralelo. Aunque ya desde hace algun tiempo se vienen construyendo generadores de alta potencia basados en estos dos osciladores, el exito nunca ha. sido completo en ninguno de los dos casos. Tal y como se explica en la introduccion de esta memoria, los puentes inversores utilizados deben operar sobre una carga inductiva (corriente retrasada) para evitar el fenomeno de la recuperacion inversa de sus diodos y la consiguiente ruptura de los transistores. De la restriccion topologica anterior se deduce que el generador paralelo debe conmutar a frecuencias inferiores a la resonancia, y el serie a frecuencias superiores. A esta restriccion topologica hay que unir otra que es exclusiva del calentamiento por induccion: La corriente por la bobina de caldeo debe ser sinusoidal. De no ser asi, resultaria imposible disponer toda la potencia de calentamiento sobre la pieza en el espesor requerido por la aplicacion. Como consecuencia, los inversores no pueden operar por debajo de la frecuencia de resonancia del oscilador, pues en ese caso se amplifican los armonicos de orden superior de la tension/corriente de entrada situados sobre la resonancia, con la consiguiente distorsion de la corriente de salida. La conjuncion de las dos restricciones anteriores obligan al inversor paralelo a funcionar a la frecuencia de resonancia del oscilador. Esto imposibilita un control por variacion de frecuencia, regulandose la potencia desde la

  5. Cut-off values of waist circumference to predict metabolic syndrome in obese adolescents.

    PubMed

    Masquio, Deborah Cristina Landi; Ganen, Aline de Piano; Campos, Raquel Munhoz da Silveira; Sanches, Priscila de Lima; Corgosinho, Flávia Campos; Caranti, Danielle; Tock, Lian; de Mello, Marco Túlio; Tufik, Sergio; Dâmaso, Ana R

    2015-04-01

    Introducción: El síndrome metabólico es una constelación de alteraciones metabólicas relacionadas con la obesidad abdominal, la inflamación y la resistencia a la insulina, lo que aumenta las enfermedades cardiovasculares y la mortalidad. Los objetivos del presente estudio fueron determinar la prevalencia de comorbilidades y parámetros alterados en adolescentes obesos con y sin SM, y determinar los puntos de corte de la circunferencia de cintura para predecir SM. Métodos: 195 adolescentes obesos y se los dividió según síndrome metabólico diagnóstico basado en criterios de la IDF. Los análisis de sangre se midieron de glucosa, lípidos, enzimas hepáticas, la adiponectina y leptina. Resistencia a la insulina se evaluó mediante HOMA-IR, QUICKI y HOMA-AD. Se obtuvieron ecografía visceral, subcutánea y grasa hepática. La composición corporal se calcula por el sistema BOD POD. Resultados: Se observó una prevalencia del 25% de síndrome metabólico Mets (n = 50). El grupo grupo con síndrome metabólico presentó mayor masa corporal, índice de masa corporal, grasa corporal (kg), sin grasa masa significativa (kg), circunferencia de la cintura, la grasa visceral, la glucosa, la insulina, resistencia a la insulina, colesterol total, LDL-c, VLDL-c, triglicéridos, enzimas hepáticas, enfermedad no alcohólica del hígado graso (EHNA) y la presión arterial. Se observaron QUICKI significativamente menor y la adiponectina en el grupo con síndrome metabólico. El grupo con síndrome metabólico presentaron significativa proporción de leptina / adiponectina mayor en comparación con los que no tienen síndrome metabólico. Puntos de corte de 111,5 cm para los niños y 104,6 cm para las niñas de la circunferencia de cintura se sugirieron para predecir el síndrome metabólico. Además, la circunferencia de la cintura fue positivamente correlacionada con la grasa visceral y el número de parámetros del síndrome metabólico. Conclusión: El grupo con s

  6. When Did the Swahili Become Maritime?

    PubMed Central

    Fleisher, Jeffrey; Lane, Paul; LaViolette, Adria; Horton, Mark; Pollard, Edward; Quintana Morales, Eréndira; Vernet, Thomas; Christie, Annalisa; Wynne-Jones, Stephanie

    2015-01-01

    In this article, we examine an assumption about the historic Swahili of the eastern African coast: that they were a maritime society from their beginnings in the first millennium C.E. Based on historical and archaeological data, we suggest that, despite their proximity to and use of the sea, the level of maritimity of Swahili society increased greatly over time and was only fully realized in the early second millennium C.E. Drawing on recent theorizing from other areas of the world about maritimity as well as research on the Swahili, we discuss three arenas that distinguish first- and second-millennium coastal society in terms of their maritime orientation. These are variability and discontinuity in settlement location and permanence; evidence of increased engagement with the sea through fishing and sailing technology; and specialized architectural developments involving port facilities, mosques, and houses. The implications of this study are that we must move beyond coastal location in determining maritimity; consider how the sea and its products were part of social life; and assess whether the marine environment actively influences and is influenced by broader patterns of sociocultural organization, practice, and belief within Swahili and other societies. [maritime, fishing and sailing, long-distance trade, Swahili, eastern Africa] RESUMEN En este artículo, evaluamos la hipótesis de que los pueblos Swahili de la costa oriental africana fueron una sociedad marítima a partir del primer milenio E.C. Basados en información histórica y arqueológica, proponemos que la asociación de la sociedad Swahili con el mar incrementó considerablemente con el tiempo y se manifestó de una forma significativa particularmente desde principios del segundo milenio E.C. Utilizando teorías recientes sobre maritimidad en otras áreas del mundo, así como investigaciones sobre los Swahili, discutimos tres temas que marcan las diferencias del nivel de orientación marítima de

  7. Condiciones Físicas en Nebulosas Gaseosas

    NASA Astrophysics Data System (ADS)

    Luridiana, V.

    1999-03-01

    El presente trabajo se ha enfocado a determinar y entender las condiciones físicas en una variedad de objetos nebulares, prestando particular atención al problema de la determinación de las abundancias químicas. Para este fin, hemos utilizado métodos analíticos en algunos casos, y modelos numéricos de fotoionización en otros. El objetivo general del trabajo es proveer de una visión amplia de las herramientas teórico-observacionales que se utilizan para la determinación de la estructura de temperatura y densidad de las regiones fotoionizadas, poniendo en evidencia posibles fuentes de errores sistemáticos y sus consecuencias para la determinación de las abundancias químicas, y proponiendo métodos para corregirlos. Los resultados principales de este trabajo est´n listados a continuación: a) Se discute el problema de la discrepancia entre T(C III) y T(O III) en las nebulosas planetarias, y se muestra como tal discrepancia implica probablemente la presencia de fluctuaciones de temperatura. Debido a que la temperatura de O++ es muy afectada por fluctuaciones de temperatura, se recomienda usar la temperatura de C++ para determinar la abundancia de carbono. b) Presentamos dos nuevos métodos para determinar la temperatura electrónica en nebulosas planetarias, basados en la medición de las intensidades de las líneas de He I. Las temperaturas que se obtienen a partir de estos métodos son menores que aquellas que se obtienen a partir de las líneas de [O III], implicando la presencia de fluctuaciones espaciales de temperatura. Despreciando las fluctuaciones de temperatura, se obtienen valores sesgados de las abundancias químicas. Determinamos las abundancias en las nebulosas planetarias de tipo I de algunos de los elementos más importantes, tomando en cuenta las fluctuaciones de temperatura. c) Presentamos modelos numéricos de las dos regiones H II extragalácticas gigantes NGC 2363 y NGC 5461. Con el modelaje numérico, pretendemos acotar las car

  8. THE INFLUENCE OF HLA-DQ2 HETERODIMERS ON THE CLINICAL FEATURES AND LABORATORY OF PATIENTS WITH CELIAC DISEASE.

    PubMed

    Akar, H Haluk; Yıldız, Mikdat; Sevinc, Eylem; Sokucu, Semra

    2015-12-01

    Antecedentes y objetivo: el marcador genético esencial relacionado con la enfermedad celíaca (CD) es la molécula HLA-DQ2 codificada por los genes DQA1*0501 y DQB1*0201. El objetivo de este estudio es evaluar el efecto de estos alelos en las características clínicas, serológicas e histológicas de los niños turcos que tienen la enfermedad celíaca. Material y métodos: nosotros hemos dividido los 36 pacientes celíacos en 4 grupos de acuerdo con su genotipo HLA-DQ2 basado en la presencia o la ausencia de los alelos DQA1*0501 y DQB1*0201. Grupo 1: 4 pacientes que no tenían los alelos HLA-DQ2A1*0501 y DQ2B1*0201; Grupo 2: 12 pacientes que tenían por lo menos uno de estos alelos con un estado heterocigoto; Grupo 3: 12 pacientes que tenián ambos alelos con un estado heterocigoto; Grupo 4: 8 pacientes que tenían ambos alelos con un estado heterocigoto. Nosotros hemos comparado los grupos de acuerdo con las características clínicas, serológicas, histológicas y bioquímicas. Resultados: no había significación estadística entre los grupos por edad, índice de masa corporal, (IMC), peso por altura y aparición de síntomas. Sin embargo, en los grupos 3 y 4 comparados con los grupos 1 y 2 se observaron unas diferencias menores en IMC y anticuerpos antigliadina (AGA), sin una significación estadística. De acuerdo con los antiendomisios (EMA), la puntuación Marsh, las presentaciones clínicas y los valores hematológicos y bioquímicos, no había una significación estadística entre los grupos sin estreñimiento respecto a los valores más altos observados en el grupo 4 sin significación estadística. Se detectó hipertiroidismo en un paciente (25%) del grupo de carga genética más baja (grupo 1) con significación estadística (p < 0,046). El resultado: en este estudio, las pequeñas diferencias que se encontraton entre los grupos no dilucidaron el impacto de los alelos HLA-DQ2 A1*0501 y DQ2B1*0201 en las manifectaciones clínicas, serológicas y de

  9. A protocol for eliciting nonmaterial values through a cultural ecosystem services frame

    PubMed Central

    Gould, Rachelle K; Klain, Sarah C; Ardoin, Nicole M; Satterfield, Terre; Woodside, Ulalia; Hannahs, Neil; Daily, Gretchen C; Chan, Kai M

    2015-01-01

    Servicios Ambientales Culturales Resumen Los deseos, necesidades y valores no materiales de los accionistas influyen frecuentemente sobre el éxito de los proyectos de conservación. Estas consideraciones son difíciles de articular y caracterizar, lo que resulta en entendimiento limitado en el manejo y la política. Concebimos un protocolo de entrevista diseñado para mejorar el entendimiento de los servicios ambientales culturales (SAC). El protocolo inicia con la discusión de actividades relacionadas con ecosistemas (p. ej.: recreación, cacería) y manejo; después señala a los SAC, dando pie a los valores que encierran conceptos identificados en la Evaluación Ambiental del Milenio (2005) y explorado en otras investigaciones sobre SAC. Hicimos pruebas piloto del protocolo en Hawái y Columbia Británica. En cada localidad entrevistamos a 30 individuos de diversos entornos. Analizamos los resultados de las dos localidades para determinar la efectividad del protocolo de entrevista en la obtención de valores no materiales. Los componentes cualitativos y espaciales del protocolo nos ayudaron a caracterizar los valores culturales, sociales y éticos asociados con el ecosistema de múltiples maneras. Los mapas y las preguntas de situación, o de tipo viñeta, ayudaron a los encuestados a articular valores difíciles de discutir. Las preguntas abiertas permitieron a los encuestados expresar una diversidad de valores ambientales y demostraron ser suficientemente flexibles para que los encuestados comunicaran valores que el protocolo no buscaba explícitamente. Finalmente, los resultados sugieren que ciertos valores, aquellos mencionados frecuentemente en la entrevista, son particularmente prominentes para poblaciones particulares. El protocolo puede proporcionar datos eficientes, contextuales y basados en lugar sobre la importancia de atributos ambientales particulares para el bienestar humano. Los datos cualitativos son complementarios para las evaluaciones cuantitativas y

  10. Modelo analítico del efecto de PRS sobre satélites GPS

    NASA Astrophysics Data System (ADS)

    Meza, A.; Brunini, C.; Usandivaras, J. C.

    componente semidiurna. El modelo analítico planteado en este trabajo, predice el comportamiento de los residuos que se observan en las publicaciones más recientes. Esto abre el camino para plantear una estimación distinta de las incógnitas del problema, basado en el método de colocación por mínimos cuadrados. Ello requiere modelar estadísticamente la señal debida a las componentes de la PRS que no son tomadas en cuenta en el modelo determinista.

  11. Linking Indices for Biodiversity Monitoring to Extinction Risk Theory

    PubMed Central

    Mccarthy, Michael A; Moore, Alana L; Krauss, Jochen; Morgan, John W; Clements, Christopher F

    2014-01-01

    ndices que reflejan el riesgo de extinción serían valiosos. Desarrollamos 3 índices de biodiversidad que se basan en modelos sencillos de viabilidad de población y que relacionan el riesgo de extinción con la abundancia. Basamos el primer índice en la media geométrica de la abundancia de especies, y el segundo en una media de poder más general. En el tercer índice integramos la media geométrica y la tendencia. Estos índices requieren los mismos datos que índices previos, pero también se relacionan directamente con el riesgo de extinción. La información de campo sobre mariposas y plantas de bosque, y los estudios experimentales de comunidades protozoarias, muestran que los índices se correlacionan con las tasas locales de extinción. Al aplicar el índice basado en la media geométrica sobre los datos globales de los cambios en la abundancia de aves, sugirió que la probabilidad de extinción promedio de aves ha incrementado aproximadamente 1% desde 1970 hasta 2009. Palabras Clave Índice de biodiversidad, media geométrica, medida de la biodiversidad, riesgo de extinción PMID:24820139

  12. [Body image; literature review].

    PubMed

    Vaquero-Cristóbal, Raquel; Alacid, Fernando; Muyor, José María; López-Miñarro, Pedro Ángel

    2013-01-01

    Introducción: En los países desarrollados existen en la actualidad unos estándares de belleza basados en modelos prodelgadez, que son interiorizados por los adolescentes y los jóvenes, sobre todo en el caso de las mujeres, suponiendo un factor de riesgo para el desarrollo de alteraciones de la imagen corporal y su percepción. Objetivo: Analizar el estado actual de las investigaciones sobre la imagen corporal, las variables sociodemográficas que influyen sobre ella y su relación con la composición corporal, la realización de dietas, los trastornos de la conducta alimentaria, el deporte y los programas de intervención y prevención. Metodología: Se realizó una búsqueda bibliográfica en Medline, Isi Web of Knowlegde y Dialnet, así como una búsqueda manual entre las referencias de los estudios seleccionados y en diferentes bibliotecas. Resultados y discusión: Una mayor influencia sociocultural está asociada a una mayor percepción de la grasa corporal, a una mayor insatisfacción con la imagen corporal y a una menor valoración del autoconcepto físico general. Esto lleva a una gran cantidad de adolescentes y jóvenes a abusar de dietas restrictivas y a sufrir trastornos de la conducta alimentaria. Numerosos estudios han analizado la relación de la práctica deportiva con las alteraciones de la imagen corporal, encontrando resultados contradictorios. Por otra parte, es necesario crear herramientas objetivas para detectar las alteraciones y profundizar en el diseño de programas de prevención e intervención con el fin de evitar la distorsión de la imagen corporal, sobre todo en aquellas franjas de edad donde la población es más vulnerable a este fenómeno. Conclusiones: La excesiva preocupación sobre la imagen corporal trae como consecuencia la realización de dietas y alteraciones como los trastornos de la conducta alimentaria. Existen además otros factores que influyen sobre la imagen corporal y su percepción como es la realización de

  13. [Trends in food consumption of university students].

    PubMed

    De Piero, Alexia; Bassett, Natalia; Rossi, Analia; Sammán, Norma

    2015-04-01

    Los jóvenes universitarios necesitan consolidar buenos hábitos alimentarios basados en una adecuada selección de alimentos, los cuales constituyen un factor de fundamental importancia para mantener un buen estado de salud y prevenir enfermedades. Objetivo: Evaluar la ingesta de alimentos y el perfil de la dieta de estudiantes universitarios de Tucumán y su variación a través del tiempo. Analizar si cumplen las recomendaciones dietéticas actuales. Materiales y métodos: La recolección de datos se llevó a cabo durante los años 1998-1999 (G1) y 2012-2013 (G2); se realizó mediante una autoencuesta alimentaria y cuestionario de frecuencia de consumo de alimentos. Fue aplicada a 329 estudiantes universitarios seleccionados en forma aleatoria. El perfil alimentario se describió según la frecuencia de consumo habitual de los principales grupos de alimentos. Resultados: Los estudiantes resultaron 25,2% hombres y 74,8% mujeres, con edad promedio de 23±3 años. En general, en ambos grupos, la mayoría de los estudiantes presentó un IMC normal, sin embargo se destacó un elevado porcentaje de hombres con sobrepeso (18,2%) y obesidad (12,1%) y mujeres con bajo peso (11,6%). Según los grupos analizados y en función del sexo se observaron algunas diferencias estadísticamente significativas en la composición de macronutrientes de la dieta: en G1 fue mayor el consumo de carbohidratos en detrimento de proteínas y lípidos; se encontraron también diferencias en la ingesta de algunos micronutrientes, observándose mayor consumo de hierro y menor de vitaminas B1, B2, niacina y C en el G2. La dieta fue monótona para ambos grupos y con diferencias en el perfil de nutrientes que la conforman. La más notable fue el incremento gradual del consumo de productos azucarados, alimentos procesados, snacks y menor consumo de lácteos, pescados, frutas y vegetales en el G2. En ambos grupos, la adecuación de la ingesta alimentaria de la población estudiantil no cubrió las

  14. [Efficacy of motivational interventions in the treatment of overweight and obesity].

    PubMed

    Tárraga Marcos, M Loreto; Rosich, Nuria; Panisello Royo, Josefa María; Gálvez Casas, Aránzazu; Serrano Selva, Juan P; Rodríguez-Montes, José Antonio; Tárraga López, Pedro J

    2014-10-01

    ón: el programa basado en intervención motivacional en grupo puede mejorar parámetros antropométricos y estilos de vida en pacientes obesos tratados en un centro de Atención Primaria.

  15. [Complete process of implantation of a nutritional risk screening system in the University Hospital La Paz, Madrid].

    PubMed

    Gómez-Candela, Carmen; Serrano Labajos, Ruth; García-Vazquez, Natalia; Valero Pérez, Marlhyn; Morato Martínez, Marina; Santurino Fontecha, Cristina; González Madroño, Ana; Palma-Milla, Samara

    2013-11-01

    La malnutrición asociada a la enfermedad (MAE) está presente en un porcentaje muy elevado de los pacientes que ingresan en los hospitales y su repercusión es diversa y de mucha trascendencia. Objetivo. Desde la Unidad de Nutrición del Hospital Universitario la Paz, en colaboración con todos los miembros de la Comisión de Nutrición, nos planteamos implantar algún método de cribado en nuestro centro, que permitiese abarcar al mayor número posible de pacientes. Resultados. Debido al gran tamaño de nuestro centro, con cerca de 1500 camas, unido a una escasez de recursos humanos en nuestra unidad, optamos por utilizar el sistema de cribado CONUT (Control Nutricional) 100 % automático y basado en parámetros analíticos, muy fácil de manejar, de bajo coste y cuya validez está confirmada, adaptándolo a nuestras necesidades. El método recoge información de las bases de datos del servicio de Admisión (filiación, edad, fecha) y del Laboratorio (albúmina, colesterol, linfocitos totales) y genera, en el informe de resultados de los análisis clínicos, la información sobre la alerta de riesgo nutricional de cada paciente, así como las recomendaciones nutricionales a seguir en función del riesgo detectado en cada caso. Para llegar su implantación se llevaron a cabo diferentes evaluaciones que nos permitieron conocer previamente la carga extra de trabajo que podría generar su implantación y nuestra capacidad para asumirlas, así como numerosas actividades formativas encaminadas a que los médicos y profesionales sanitarios del hospital asumieran cada vez más responsabilidades en el proceso del tratamiento nutricional de sus pacientes. Este sistema de cribado funciona desde Junio del año 2010 y detecta riesgo de desnutrición en el 32 % de los pacientes evaluados. En general, sólo en los casos en los que la alerta corresponde a una situación de Alto riesgo nutricional, hecho que se da aproximadamente en el 10 % del total, se requirió la intervenci

  16. Sexual performance of mass reared and wild Mediterranean fruit flies (Diptera: Tephritidae) from various origins of the Madeira Islands

    SciTech Connect

    Pereira, R.; Silva, N.; Quintal, C.; Abreu, R.; Andrade, J.; Dantas, L.

    2007-03-15

    The success of Mediterranean fruit fly (medfly) Ceratitis capitata (Wiedemann) control programs integrating the sterile insect technique (SIT) is based on the capacity of released the sterile males to compete in the field for mates. The Islands of Madeira are composed of 2 populated islands (Madeira and Porto Santo) where the medfly is present. To evaluate the compatibility and sexual performance of sterile flies we conducted a series of field cage tests. At same time, the process of laboratory domestication was evaluated. 3 wild populations, one semi-wild strain, and 1 mass reared strain were evaluated: the wild populations of (1) Madeira Island (north coast), (2) Madeira Island (south coast), and (3) Porto Santo Island; (4) the semi-wild population after 7 to 10 generations of domestication in the laboratory (respectively, for first and second experiment); and (5) the genetic sexing strain in use at Madeira medfly facility (VIENNA 7mix2000). Field cage experiments showed that populations of all origins are mostly compatible. There were no significant differences among wild populations in sexual competitiveness. Semi-wild and mass-reared males performed significantly poorer in both experiments than wild males in achieving matings with wild females. The study indicates that there is no significant isolation among strains tested, although mating performance is reduced in mass-reared and semi-wild flies after 7 to 10 generations in the laboratory. (author) [Spanish] El exito de los programas de control de la mosca mediterranea de la fruta (Ceratitis capitata (Wiedemann) que integran la tecnica del insecto esteril (TIE) esta basado en la capacidad de machos esteriles para competir en el campo por sus parejas. Las Islas de Madeira consisten de 2 islas pobladas (Madeira y Porto Santo) donde la mosca mediterranea de la fruta esta presente. Para evaluar la compatibilidad y el funcionamiento sexual de moscas esteriles nosotros realizamos una serie de pruebas de jaula en el

  17. Seizures, cysticercosis and rural-to-urban migration: the PERU MIGRANT study

    PubMed Central

    Gonzales, Isidro; Miranda, J Jaime; Rodriguez, Silvia; Vargas, Victor; Cjuno, Alfredo; Smeeth, Liam; Gonzalez, Armando E; Tsang, Victor C W; Gilman, Robert H; Garcia, Hector H

    2015-01-01

    équences neurologiques de l'infection par la cysticercose sont susceptibles de survivre à la réponse d'anticorps durant des années après la migration des zones rurales vers les zones urbaines. Objetivos Examinar la prevalencia de convulsiones, epilepsia, y seropositividad para cisticercosis entre población rural (de zonas endémicas para cisticercosis), inmigrantes provenientes de zonas rurales a tugurios urbanos no endémicos, y habitantes urbanos de los mismo tugurios urbanos no endémicos. Métodos Se estudiaron tres poblaciones peruanas (n=985) originalmente reclutadas en un estudio de enfermedades crónicas y migración. Estos grupos incluían habitantes rurales de una región endémica (n=200), inmigrantes de larga duración de zonas rurales a urbanas (n=589), e individuos que vivían en la misma zona urbana (n=196). Las convulsiones se detectaron mediante una encuesta y un neurólogo examinó a quienes habían respondido positivamente. Se procesaron muestras de suero de 981/985 individuos en busca de anticuerpos para cisticercosis mediante inmunoblot. Resultados La prevalencia de epilepsia (por 1,000 personas) era de 15.3 en el grupo urbano, 35.6 en inmigrantes y 25 en habitantes rurales. Se observó un gradiente en la seroprevalencia de los anticuerpos para cisticercosis: grupos urbano 2%, inmigrante 13.5% y rural 18% (p<0.05). Se observó un patrón de aumento similar de mayor seroprevalencia entre inmigrantes según la edad que tenían en el momento de emigrar. En pobladores rurales, había una evidencia importante de asociación entre tener una serología positiva y sufrir convulsiones (p=0.011), pero esta asociación no se observaba en inmigrantes de larga duración o residentes urbanos. En la población al completo, comparada con los participantes seronegativos, aquellos con una fuerte reactividad de anticuerpos (≥4 bandas de anticuerpos) tenían una mayor probabilidad de sufrir epilepsia (p<0.001). Conclusiones No solo la migración internacional afecta la

  18. Comparison of brain mechanisms underlying the processing of Chinese characters and pseudo-characters: an event-related potential study.

    PubMed

    Wang, Ting; Li, Hong; Zhang, Qinglin; Tu, Shen; Yu, Caiyun; Qiu, Jiang

    2010-04-01

    450 ms, une plus grande négativité (N360) fut observée pour les pseudo-caractères comparativement aux caractères des régions du scalp au-dessus des régions médianes fronto-centrales. L'analyse dipôle a localisé le générateur de N360 dans le cortex para-hippocampique droit. Ainsi, le N360 pourrait être une composante N400 et refléter une activation sémantique de haut niveau sur la base des traitements orthographique, phonologique et perceptuel-sémantique. La mayoría de los caracteres chinos están compuestos por un radical semántico a la izquierda y un radical fonético a la derecha. El radical semántico puede proporcionar información semántica y el radical fonético puede proporcionar información relacionada con la pronunciación del carácter entero. Los pseudo-caracteres consistieron en diferentes partes sub-léxicas de los caracteres reales chinos y como consecuencia, también tenían radicales semánticos y fonéticos. Pero éstos no se podían leer y tampoco tenían un significado real. Para investigar los patrones de la activación cortical espaciotemporal subyacentes de los procesamientos ortográfico, fonológico y semántico de los caracteres chinos, utilizamos potencial relacionado con eventos (ERPs) para explorar el procesamiento de caracteres chinos y pseudo-caracteres mientras que 14 sanos estudiantes chinos veían los caracteres de forma pasiva. Los resultados demostraron que ambos, caracteres y pseudo-caracteres chinos evocaban potenciales negativos con picos alrededor de los 120 ms (N120), lo cual parece reflejar distinción inicial ortográfica y evaluación. Además, los pseudo-caracteres chinos provocaban una desviación ERP más positiva (P220) en comparación con los caracteres chinos entre 200-250 ms después de la aparición de los estímulos. Esto fue parecido a RP (potenciales de reconocimiento) y puede reflejar un proceso de integración del procesamiento fonológico y semántico basado en la información ortogr

  19. Estimating Climate Resilience for Conservation across Geophysical Settings

    PubMed Central

    ANDERSON, MARK G; CLARK, MELISSA; SHELDON, ARLENE OLIVERO

    2014-01-01

    poder conservar la diversidad biológica mientras permiten que las especies y las comunidades se reorganicen con respecto al clima cambiante. Desarrollamos y probamos tal método, el cual basamos en características físicas asociadas con la diversidad ecológica y la capacidad de recuperación del sitio con respecto al cambio climático, en el noreste de Norteamérica. Mapeamos comprensivamente 30 escenarios geofísicos distintos basados en la geología y la elevación. Dentro de cada escenario geofísico identificamos sitios que estaban conectados por una cubierta natural y que tenían relativamente más microclimas indicados por la topografía diversa y los gradientes de elevación. Hicimos esto al puntuar cada hexágono de 450 ha en la región con estas dos características y al seleccionar aquellos que tuvieron una puntuación >SD 0.5 por encima del puntaje combinado promedio para cada escenario. Nuestra hipótesis fue que estos sitios con altas puntuaciones tuvieron la mayor capacidad de recuperación. Los comparamos con los sitios seleccionados por The Nature Conservancy por sus poblaciones de alta calidad de especies raras y sus ocurrencias de comunidades naturales. Los sitios con altos puntajes capturaron significativamente más de los sitios de biodiversidad de lo que se esperaba por casualidad (p < 0.0001): 75% de las 414 especies objetivo, 49% de las 4592 localidades de especies objetivo y 53% de las 2710 localidades de comunidades objetivo. Los escenarios de lecho rocoso calcáreo, arena gruesa y limo fino tuvieron puntos marcadamente más bajos para la capacidad de recuperación estimada y tuvieron niveles bajos de protección permanente de suelo (en promedio 7%). Ya que nuestro método identifica – para cada escenario geofísico – sitios que tienen mayor probabilidad de retener especies y funciones más tiempo bajo un clima cambiante, revela baluartes naturales para la con

  20. ‘Everybody knows’, but the rest of the world: the case of a caterpillar-borne reproductive loss syndrome in dromedary camels observed by Sahrawi pastoralists of Western Sahara

    PubMed Central

    2013-01-01

    índrome de pérdida reproductiva en dromedarios transmitido por orugas y observado por pastores nómadas saharauis del Sáhara Occidental. Antecedentes Los conocimientos tradicionales de las comunidades locales de todo el mundo son una valiosa fuente de nuevas ideas e información para la ciencia. En este estudio, se utilizaron los conocimientos de etnoveterinaria de pastores saharauis del Sáhara Occidental con el fin de proponer una hipótesis científica sobre las interacciones competitivas entre los camellos y las orugas en el ecosistema del Sáhara. Métodos Entre los años 2005 y 2009, se realizaron 44 entrevistas semi-estructuradas a los pastores saharauis en los territorios administrados por la República Árabe Saharaui Democrática, Sáhara Occidental, mediante un diseño de muestreo por bola de nieve. Resultados Los pastores nómadas saharauis describieron un síndrome reproductivo transmitido por orugas, llamado duda, entre sus camellas. Sobre la base de los conocimientos saharauis sobre el duda y una revisión literaria exhaustiva, se propuso la siguiente hipótesis: 1) brotes esporádico de orugas de la familia Lasiocampidae (géneros Lasiocampa, Psilogaster o Streblote) en árboles de Acacia se pueden presentar después de fuertes lluvias en el ecosistema del Sáhara Occidental; 2) durante estos brotes, los camellos ingieren las orugas durante el pastoreo; 3) como consecuencia de esta ingestión, se producen abortos repentinos o partos de crías debilitadas. Apoyamos esta hipótesis mediante razonamiento inductivo basado en evidencia circunstancial y razonamiento analógico con síndromes similares en yeguas de los Estados Unidos y Australia. Conclusiones Este es el primer reporte de la posible existencia de un síndrome de pérdida reproductiva en camellos, transmitido por orugas. Se insinúa que estos síndromes son más comunes que lo que actualmente se conoce. Se sugieren investigaciones adicionales p

  1. Hydrodynamic model of cells for designing systems of urban groundwater drainage

    NASA Astrophysics Data System (ADS)

    Zimmermann, Eric; Riccardi, Gerardo

    2000-08-01

    érée comme satisfaisante dans tous les cas. Afin de simuler des situations plus complexes, la nouvelle version proposée, CELSUB3, a été mise en œuvre dans un projet destiné à contrôler le niveau de la nappe à l'intérieur d'un système d'égouts, dans la ville de Chaar Ladeado (province de Santa Fe, Argentine). Différentes organisations du projet de drainage, qui ont été testées pour des conditions de recharge dynamique causées par la pluie au cours d'une année critique (la plus humide de la chronique disponible) et une année typique, sont brièvement décrites. Après analyse de dix organisations différentes, la meilleure solution technico-économique retenue est un système de drainage souterrain de conduites avec des stations de pompage et des canaux d'évacuation. Resumen. Se presenta un modelo matemático hidrodinámico cuasi-bidimensional de celdas, CELSUB3, apto para la simulación integral de sistemas de drenaje subterráneo basados en campos de bombeo o drenes subsuperficiales. El modelo de simulación presenta un ensamble de algoritmos, previamente desarrollados y testeados, que representan al escurrimiento a través del medio poroso saturado, escurrimiento en conducciones cerradas, estaciones de bombeo, etc. En la estructura del modelo se propone un nuevo tipo de vinculación entre celdas acuíferas y conductos de drenaje, la cual es verificada en problemas simples con solución analítica conocida arrojando, en todos los casos, resultados satisfactorios. Abordando situaciones más complejas, la nueva versión propuesta fue aplicada en un proyecto de control de niveles freáticos que acompaña un sistema de conductos cloacales, en la localidad de Chañar Ladeado, Santa Fe, Argentina. Se describen las alternativas de drenaje consideradas las cuales fueron evaluadas bajo recargas dinámicas provocadas por años críticamente lluviosos y en situaciones típicas. Los resultados derivados permitieron definir, tras analizar una decena de proyectos

  2. Estimating Climate Resilience for Conservation across Geophysical Settings

    PubMed Central

    ANDERSON, MARK G; CLARK, MELISSA; SHELDON, ARLENE OLIVERO

    2014-01-01

    poder conservar la diversidad biológica mientras permiten que las especies y las comunidades se reorganicen con respecto al clima cambiante. Desarrollamos y probamos tal método, el cual basamos en características físicas asociadas con la diversidad ecológica y la capacidad de recuperación del sitio con respecto al cambio climático, en el noreste de Norteamérica. Mapeamos comprensivamente 30 escenarios geofísicos distintos basados en la geología y la elevación. Dentro de cada escenario geofísico identificamos sitios que estaban conectados por una cubierta natural y que tenían relativamente más microclimas indicados por la topografía diversa y los gradientes de elevación. Hicimos esto al puntuar cada hexágono de 450 ha en la región con estas dos características y al seleccionar aquellos que tuvieron una puntuación >SD 0.5 por encima del puntaje combinado promedio para cada escenario. Nuestra hipótesis fue que estos sitios con altas puntuaciones tuvieron la mayor capacidad de recuperación. Los comparamos con los sitios seleccionados por The Nature Conservancy por sus poblaciones de alta calidad de especies raras y sus ocurrencias de comunidades naturales. Los sitios con altos puntajes capturaron significativamente más de los sitios de biodiversidad de lo que se esperaba por casualidad (p < 0.0001): 75% de las 414 especies objetivo, 49% de las 4592 localidades de especies objetivo y 53% de las 2710 localidades de comunidades objetivo. Los escenarios de lecho rocoso calcáreo, arena gruesa y limo fino tuvieron puntos marcadamente más bajos para la capacidad de recuperación estimada y tuvieron niveles bajos de protección permanente de suelo (en promedio 7%). Ya que nuestro método identifica – para cada escenario geofísico – sitios que tienen mayor probabilidad de retener especies y funciones más tiempo bajo un clima cambiante, revela baluartes naturales para la conservación futura que también capturaría biodiversidad existente sustancial y

  3. Application of the groundwater-balance equation to indicate interbasin and vertical flow in two semi-arid drainage basins, Mexico

    NASA Astrophysics Data System (ADS)

    Carrillo-Rivera, J. J.

    2000-09-01

    conclusion est qu'une étude par bilan de la nappe est une méthode qui n'est pas satisfaisante pour déterminer certains paramètres comme le coefficient d'emmagasinement. En particulier, l'approche par le bilan de la nappe donne des résultats qui ne sont pas fiables lorsque l'on ignore la drainance verticale ou que l'on ne peut pas la définir correctement. L'existence d'une drainance verticale est prouvée par des températures de l'eau souterraine pouvant être supérieures de 23 °C à la température ambiante. Des failles régionales peuvent permettre ces écoulements vers le haut. Lorsque l'on ignore la drainance verticale, on introduit une incertitude sur l'estimation de l'emmagasinement à partir des calculs du bilan régional de la nappe. Sur la base de l'équation du bilan de la nappe, une valeur de S=0,19 semble représenter les conditions captives de la partie développée de l'aquifère ce résultat est plus élevé, de plusieurs ordres de grandeur, que celui que l'on peut raisonnablement attendre des conditions géologiques. Ces résultats sont utiles pour évaluer si une ressource en eau souterraine est "surexploitée". Ces conclusions sont intéressantes lorsque l'on applique des modèles d'écoulement transitoire dans lesquels on ne prend pas en compte la drainance verticale d'une eau plus légère remontant. Resumen. En este trabajo, se investigan las entradas y salidas de flujo horizontal en la ecuación de balance de agua subterránea, así como el papel que desempeñan en el flujo entre cuencas. Se analizan dos ejemplos de México, uno en la Península de Baja California y otro en la parte central del país. En ambos, destaca la influencia del flujo entre cuencas, ya que se estima que una parte importante (aproximadamente el 70%) del agua termal extraída procede de una cuenca superficial externa. Se concluye que el método basado en cálculos de balance de agua subterránea no es satisfactorio para determinar algunos parámetros, como, por ejemplo, el

  4. A quantitative synthesis of the medicinal ethnobotany of the Malinké of Mali and the Asháninka of Peru, with a new theoretical framework

    PubMed Central

    Bletter, Nathaniel

    2007-01-01

    from around the world to pinpoint the species with the highest potential efficacy to take into the laboratory and analyze further, ultimately saving much field and laboratory time and resources. Spanish abstract Las búsquedas que utilizan la etnomedicina y la taxonomía para descubrir nuevas plantas medicinales, pueden aumentar la probabilidad de éxito de encontrar compuestos químicos activos en plantas, en comparación con las búsquedas aleatorias. A pesar de lo anterior, en las últimas décadas, la etnobotánica no ha cumplido con las expectativas de proveer numerosas plantas medicinales y químicos nuevos una vez examinados en el laboratorio. Cada año se describen una plétora de plantas medicinales y sus usos, sin embargo las limitaciones de tiempo y recursos en los laboratorios, unidos al alto coste de los ensayos clínicos de las drogas potenciales, hacen muy difícil probar, aislar, y elucidar la estructura y el mecanismo de los compuestos de estas plantas. Se propone un nuevo marco teórico cuantitativo cuyo fin es focalizar la búsqueda de nueva plantas medicinales. Este marco teórico está basado en la hipótesis que las plantas cercanamente relacionadas, usadas para tratar enfermedades cercanamente relacionadas en culturas distantemente relacionadas, tienen una eficacia potencial más alta, debido a que es más probable que estos hallazgos sean descubrimientos independientes de compuestos químicos similares. Parte de esta hipótesis, que las escogencias racionales se hacen para elegir plantas medicinales similares y que la flora medicinal de dos culturas distantes es más similar que su flora general, se probó usando métodos estadísticos de remuestreo con datos de campo de la comunidad Malinké de Malí y de la Asháninka de Perú, y las enfermedades de paludismo, enfermedad africana del sueño, enfermedad de Chagas, leishmania, diabetes, eczema, asma, y fibromas uterinos. Se encontró, en este caso, que

  5. Variations in hydraulic conductivity with scale of measurement during aquifer tests in heterogeneous, porous carbonate rocks

    NASA Astrophysics Data System (ADS)

    Schulze-Makuch, Dirk; Cherkauer, Douglas S.

    rapport au niveau d'échelle au cours d'essais de nappe individuels, dans des roches carbonatées poreuses, hétérogènes du sud-est du Wisconsin (Etats-Unis). Les résultats obtenus indiquent que la conductivité hydraulique augmente en général au cours d'un essa