922 resultados para Bounded rationatility
Resumo:
The site for CRP-2, 14 km east of Cape Roberts (77.006°S; 163.719°E), was selected to overlap the early Miocene strata cored in nearby CRP-1, and to sample deeper into the east-dipping strata near the western margin ofe he Victoria Land Basin to investigate Palaeogene climatic and tectonic history. CRP-2 was cored from 5 to 57 mbsf (metres below the sea floor) (core recovery 91 %), with a deviation resulting in CRP-2A being cored at the same site. CRP-2A reached down to 624mbsf (recovery 95%), and to strata with an age of c. 33-35 Ma. Drilling took place from 16 October to 25 November 1998, on 2.0-2.2 m of sea ice and through 178 m of water. Core fractures and other physical properties, such as sonic velocity, density and magnetic susceptibility, were measured throughout the core. Down-hole logs for these and other properties were run from 63 to 167 mbsf and subsequently from 200 to 623 mbsf, although density and velocity data could be obtained only to 440 mbsf because of hole collapse. Sonic velocity averages c. 2.0 km S-1 for the upper part of the hole, but there is an sharp increase to c. 3.0 km s-1 and also a slight angular unconformity, at 306 mbsf, corresponding most likely to the early/late Oligocene boundary (c. 28-30 Ma). Velocity then increases irregularly to around 3.6 km s-1 at the bottom of the hole, which is estimated to lie 120 m above the V4/V5 boundary. The higher velocities below 306 mbsf probably reflect more extensive carbonate and common pyrite cementation, in patches, nodules, bedding-parallel masses and as vein infills. Dip of the strata also increases down-hole from 3° in the upper 300 in to over 10° at the bottom. Temperature gradient is 21° k-1. Over 2 000 fractures were logged through the hole. Borehole televiewer imagery was obtained for the interval from 200 to 440 mbsf to orient the fractures for stress field analysis. Lithostratigraphical descriptions on a scale of 1:20 are presented for the full length of the core, along with core box images, as a 200 page supplement to this issue. The hole initially passed through a layer of muddy gravel to 5.5 mbsf (Lithological Sub-Unit or LSU 1.1), and then into a Quaternary diatom-bearing clast-rich diamicton to 21 mbsf (LSU 2. l), with an interval of alternating compact diamicton and loose sand, and containing a rich Pliocene foraminiferal fauna, to 27 mbsf (LSU 2.2). The unit beneath this (LSU 3.1) has similar physical properties (sonic velocity, porosity, magnetic susceptibility) and includes diamictites of similar character to those of LSU 2.1 and 2.2, but an early Miocene (c. 19 Ma) diatom assemblage at 28 mbsf (top of LSU 3.1) shows that this sub-unit is part of the older section. The strata beneath 27 mbsf, primary target for the project, extend from early Miocene to perhaps latest Eocene age, and are largely cyclic glacimarine nearshore to offshore sediments. They are described as 41 lithological sub-units and interpreted in terms of 12 recurrent lithofacies. These are 1) mudstone, 2) inter-stratified mudstone and sandstone, 3) muddy very fine to coarse sandstone, 4) well-sorted stratified fine sandstone, 5) moderately to well-sorted, medium-grained sandstone, 6) stratified diamictite, 7) massive diamictite, 8) rhythmically inter-stratified sandstone and mudstone, 9) clast-supported conglomerate, 10) matrix-supported conglomerate, 11) mudstone breccia and 12) volcaniclastic sediment. Sequence stratigraphical analysis has identified 22 unconformity-bounded depositional sequences in pre- Pliocene strata. They typically comprise a four-part architecture involving, in ascending order, 1) a sharp-based coarse-grained unit (Facies 6,7,9 or 10), 2) a fining-upward succession of sandstones (Facies 3 and 4), 3) a mudstone interval (Facies l), in some cases coarsening upward to muddy sandstones (Facies 3), and 4) a sharp-based sandstone dominated succession (mainly Facies 4). The cyclicity recorded by the strata is interpreted in terms of a glacier ice margin retreating and advancing from land to the west, and of rises and falls in sea level. Analysis of sequence periodicity awaits afirmer chronology. However, apreliminary spectral analysis of magnetic susceptibility for a deepwater mudstone within one of the sequences (from 339 to 347 mbsf) reveals ratios between hierarchical levels that are similar to those of the three Milankovitch orbital forcing periodicities. The strata contain a wide range of fossils, the most abundant being marine diatoms. These commonly form up to 5% of the sediment, though in places the core is barren (notably between 300 and 412 mbsf). Fifty samples out of 250 reviewed were studied in detail. The assemblages define ten biostratigraphical zones, some of them based on local or as yet undescribed forms. The assemblages are neritic, and largely planktonic, suggesting that the sea floor was mostly below the photic zone throughout deposition of the corcd sequence. Calcareous nannofossils, representing incursions of ocean surface waters, are much less common (72 out of 183 samples examined) and restricted to mudstone intervals a few tens of metres thick, but are important for dating. Foraminifera are also sparse (73 out of 135 samples) and represented only by calcareous benthic species. Changing assemblages indicate a shift from inshore environments in the early Oligocenc to outer shelf in the late Oligocenc, returning to inshore in the early Miocene. Marine palynomorplis yielded large numbers of well-preserved forms from most of the 116 samples examined. The new in situ assemblagc found last year in CRP-1 is extended down into the late Oligocene and a further new assemblage is found in the early Oligoccnc. Many taxa are new, and cannot us yet contribute to an improved understanding of chronology or ecology. Marine invertebrate macrofossils, mostly molluscs and serpulid tubes, are scattered throughout the core. Preservation is good in mudstones but poor in other lithologies. Climate on land is reflected in the content of terrestrial palynomorphs, which are extremely scarce down to c. 300 mbsf. Some forms are reworked, and others represent a low growing sparse tundra with at least one species of Nothofagus. Beneath this level, a significantly greater diversity and abundance suggests a milder climate and a low diversity woody vegetation in the early Oligocene, but still far short of the richness found in known Eocene strata of the region. Sedimentary facies in the oldest strata also suggest a milder climate in the oldest strata cored, with indications of substantial glacial melt-water discharges, but are typical of a coldcr climate in late Oligocene and early Miocene times. Clast analyses from diamictites reveal weak to random fabrics, suggesting either lack of ice-contact deposition or post-depositional modification, but periods when ice grounded at the drill site are inferred from thin zones of in-situ brecciated rock and soft-sediment folding. These are more common above c. 300 mbsf, perhaps reflecting more extensive glacial advances during deposition of those strata. Erosion of the adjacent Transantarctic Mountains through Jurassic basalt and dolerite-intruded Beacon strata into basement rocks beneath is recorded by petrographical studies of clast and sand grain assemblages. Core below 310 mbsf contains a dominance of fine-grained Jurassic dolerite and basalt fragments along with Beacon-derived coal debris and rounded quartz grains, whereas the strata above this level have a much higher proportion of basement derived granitoids, implying that the large areas of the adjacent mountains had been eroded to basement by the end of the early Oligocene. There is little indication of rift-related volcanism below 310 mbsf. Above this, however, basaltic and trachytic tephras are common, especially from 280 to 200 mbsf, from 150 to 46 mbsf, and in Pliocene LSU 2.2 from 21 to 27 mbsf. The largest volcanic eruptions generated layers of coarse (up to 1 cm) trachytic pumice lapilli between 97 and 114 mbsf. The thickest of these (1.2 m at 112 mbsf) may have produced an eruptive column extending tens of km into the stratosphere. A source within a few tens of km of the drill site is considered most likely. Present age estimates for the pre-Pliocene sequence are based mainly on biostratigraphy (using mainly marine diatoms and to a lesser extent calcareous nannofossils), with the age of the tephra from 112 to 114 mbsf (21.44k0.05 Ma from 84 crystals by Ar-Ar) as a key reference point. Although there are varied and well-preserved microfossil assemblages through most of the sequence (notably of diatoms and marine palynomorphs), they comprise largely taxa either known only locally or as yet undescribed. In addition, sequence stratigraphical analysis and features in the core itself indicate numerous disconformities. The present estimate from diatom assemblages is that the interval from 27 to 130 mbsf is early Miocene in age (c. 19 to 23.5 Ma), consistent with the Ar-Ar age from 112 to 114 mbsf. Diatom assemblages also indicate that the late Oligocene epoch extends from c. 130 to 307 mbsf, which is supported by late Oligocene nannofossils from 130 to 185 mbsf. Strata from 307 to 412 mbsf have no age-diagnostic assemblages, but below this early Oligocene diatoms and nannofossils have been recovered. A nannoflora at the bottom of the hole is consistent with an earliest Oligocene or latest Eocene age. Magnetostratigraphical studies based on about 1000 samples, 700 of which have so far undergone demagnetisation treatment, have provided a polarity stratigraphy of 12 pre-Pliocene magnetozones. Samples above 270 mbsf are of consistently high quality. Below this, magnetic behaviour is more variable. A preliminary age-depth plot using the Magnetic Polarity Time Scale (MPTS) and constrained by biostratigraphical data suggests that episodes of relatively rapid sedimentation took place at CRP-2 during Oligocene times (c. 100 m/My), but that more than half of the record was lost in a few major and many minor disconformities. Age estimates from Sr isotopes in shell debris and further tephra dating are expected to lead to a better comparison with the MPTS. CRP-2/2A has recorded a history of subsidence of the Victoria Land Basin margin that is similar to that found in CIROS-170 km to the south, reflecting stability in both basin and the adjacent mountains in late Cenozoic times, but with slow net accumulation in the middle Cenozoic. The climatic indicators from both drill holes show a similar correspondence, indicating polar conditions for the Quaternary but with sub-polar conditions in the early Miocene-late Oligocene and indications of warmer conditions still in the early Oligocene. Correlation between the CRP-2A core and seismic records shows that seismic units V3 and V4, both widespread in the Victoria Land Basin, represent a period of fluctuating ice margins and glacimarine sedimentation. The next drill hole, CRP-3, is expected to core deep into V5 and extend this record of climate and tectonics still further back in time.
Resumo:
Colombia has oceanic waters, catchment areas, like lakes, cienagas and swamps, water flows, like rivers, gorges and streams, small rivers and groundwater. The oceanic waters are the Caribbean Sea-1600 km and the Pacific Ocean-1300 km that comprise the north and west continental territory, respectively. Actually the Region of Darién, geographically bounded by the Carribean Sea to the north is becoming to be focused by studies due to use conflicts and disputes about water and a forest reserve on its territories. Considering its location, strategic at northwestern Colombia, frontier region with Central America, several dynamics are imposed. One of them is the implantation of a road system entitled Connecting Road of the Americas. This fact means the construction of an infra-structure that will cross a special zone formed by swamps and jungle known as The Darién Gap. Evidences of such interests are revealed by projects like the constructions of Turbo's Port in the Atlantic Ocean, Department of Antioquia and Tribugá's Port in the Pacific Ocean, Department of Choco, the mountain road and the coastal conection Colombia-Venezuela attending to the main intentions of the central region of the department (Metropolitan Area of Aburrá Valley-AMVA). Human settlements form a productive system, based on small and medium familiar agriculture's production, corresponding to the western portion and piedmont of Abibe's mountain at its antioquian portion, alluvial plan that forms the rivers on this area, the littoral zone that delimits the Carribean Sea, the Darién and Baudó Mountains and the gulf that receives, among other waters, the ones from Atrato and León, as well as the exodus process constitutes a forced exit resulting from actions of several armed groups. It can be identified intense historical, cultural, political and environmental relations, specially the last one associated with strategic ecosystems that are fundamental for the hydric regulation of the region, as well as food safety of the local inhabitants. Results from two researches (UPB, 2007 y 2010) reveals this quick transformation in the spatial re-configuration, demographical and economical indicators and the exacerbated fight for resources, damaging the extractive vocation in the Region. Path to commerce of illegalities (drugs, guns) and to implementation of the agroindustrial project for biofuel production, cooperation program that involves Venezuela, Brazil and Colombia. Appropriation modes allow the existence of strategies since global interests revealing a development logic that privileges the conception of an artificialized nature. Since the smallest portion of rural areas, specific modes of resources exploration are linked to imposed interests of transnational corporations. Disparate consequences are going deeper evidenced by social, technical and nature transformations, envisioning risks for the habitability's condition
Resumo:
Buscamos avanzar en el conocimiento sobre cómo se desarrolla el movimiento de la sociedad argentina en su conjunto, analizado desde un caso particular que es el noreste del Chubut en el período que va desde la imposición de la hegemonía del capital financiero en 1989-1990 hasta el año 2005. Se pretende en esta tesis entender y conceptualizar en términos científicos cómo se mueve esa sociedad, de qué son expresión cada uno de sus conflictos, qué expresan los distintos sectores que se movilizan, qué expresan los cambios estructurales que se desarrollan, etc. Desde esta perspectiva nos interesa específicamente poder aportar al debate sobre cuáles son las opciones de plantear un proyecto alternativo de desarrollo para la provincia, la región y el país. Dentro del tema general de buscar comprender el movimiento de la sociedad, realizamos un abordaje de la realidad desde la utilización de un conocimiento acumulado y desde un recorte de esa realidad. Ese recorte lo realizamos a dos niveles. En primer lugar en términos espaciales: tomamos como base una región que denominamos el noreste de Chubut. Recortamos de la provincia del Chubut al área que tuvo el mayor crecimiento vinculado a los programas de polos de desarrollo durante las décadas del '60, '70 y parte del '80. La misma está delimitada por los actuales departamentos de Rawson y Biedma, de acuerdo a la división administrativa que toma la provincia desde 1957. En segundo lugar realizamos un recorte en términos temporales: abordamos como objeto de estudio al movimiento de la sociedad en esa región durante el período que va de 1989-1990 hasta el 2005. Consideramos que tomar este período nos permite observar el proceso de cambios que se generan con la realización de la hegemonía del capital financiero y el proceso de protestas, luchas y conflictos sociales que en el marco de estos cambios se desarrollan en la sociedad. La decisión de estudiar hasta el 2005 parte de considerar relevante comprender cómo continua el proceso después del 2001-2002. En esos años se produce la recuperación de la economía nacional, con un gran impulso para la región, lo cual genera el interés de poder precisar de qué se trata esta 'recuperación' y si estamos ante un movimiento orgánico o coyuntural de la economía. El período también nos permitió profundizar en el debate de las relaciones de fuerzas políticas, al hacer observable el período en que la burguesía logra recuperar la representación institucional como expresión legítima de la sociedad y consigue frenar la protesta social
Resumo:
Este trabajo se propone explorar las estrategias de legitimación que se desplegaron en un espacio local acotado durante la primera etapa del llamado "Proceso de Reorganización Nacional" en la Argentina. Desde una mirada centrada en los actores, en el análisis del discurso y en la historia local se analizarán los discursos que funcionarios y personalidades de relevancia nacional, provincial y local pronunciaron durante la Primera Exposición Internacional que se llevó a cabo en la ciudad bonaerense de Junín en octubre de 1977. Se intentarán vislumbrar los idearios y las representaciones que construyeron en torno a la figura de los productores agropecuarios, de los intendentes y de los municipios, como también sus vinculaciones con la dimensión simbólica del proyecto autoritario en el que pretendió sustentarse aquella dictadura
Resumo:
El concepto de extensión universitaria ha recorrido un largo trayecto desde sus primeras formulaciones durante el siglo XIX. A lo largo del mismo ha ido incorporando distintos significados, generalmente enmarcados en un modelo de relación asimétrica entre la sociedad y la población asistida. El concepto de apropiación social del conocimiento, de factura más reciente, pretende una aproximación más efectiva y dinámica del público al conocimiento científico. Sin embargo, ambos conceptos mantienen de manera más o menos explícita la relación lineal y asimétrica entre el conocimiento experto y el conocimiento profano. En este trabajo se reflexiona sobre la extensión universitaria como un marco de relación en el que tienda a conjugarse una dinámica de producción de decisiones basadas en la hibridación de conocimientos heterogéneos, con articulación de conocimientos universales y locales, en los que el público y los beneficiarios de las acciones de extensión universitaria asumen papeles activos para la construcción de las soluciones a los problemas acotados localmente.
Resumo:
Buscamos avanzar en el conocimiento sobre cómo se desarrolla el movimiento de la sociedad argentina en su conjunto, analizado desde un caso particular que es el noreste del Chubut en el período que va desde la imposición de la hegemonía del capital financiero en 1989-1990 hasta el año 2005. Se pretende en esta tesis entender y conceptualizar en términos científicos cómo se mueve esa sociedad, de qué son expresión cada uno de sus conflictos, qué expresan los distintos sectores que se movilizan, qué expresan los cambios estructurales que se desarrollan, etc. Desde esta perspectiva nos interesa específicamente poder aportar al debate sobre cuáles son las opciones de plantear un proyecto alternativo de desarrollo para la provincia, la región y el país. Dentro del tema general de buscar comprender el movimiento de la sociedad, realizamos un abordaje de la realidad desde la utilización de un conocimiento acumulado y desde un recorte de esa realidad. Ese recorte lo realizamos a dos niveles. En primer lugar en términos espaciales: tomamos como base una región que denominamos el noreste de Chubut. Recortamos de la provincia del Chubut al área que tuvo el mayor crecimiento vinculado a los programas de polos de desarrollo durante las décadas del '60, '70 y parte del '80. La misma está delimitada por los actuales departamentos de Rawson y Biedma, de acuerdo a la división administrativa que toma la provincia desde 1957. En segundo lugar realizamos un recorte en términos temporales: abordamos como objeto de estudio al movimiento de la sociedad en esa región durante el período que va de 1989-1990 hasta el 2005. Consideramos que tomar este período nos permite observar el proceso de cambios que se generan con la realización de la hegemonía del capital financiero y el proceso de protestas, luchas y conflictos sociales que en el marco de estos cambios se desarrollan en la sociedad. La decisión de estudiar hasta el 2005 parte de considerar relevante comprender cómo continua el proceso después del 2001-2002. En esos años se produce la recuperación de la economía nacional, con un gran impulso para la región, lo cual genera el interés de poder precisar de qué se trata esta 'recuperación' y si estamos ante un movimiento orgánico o coyuntural de la economía. El período también nos permitió profundizar en el debate de las relaciones de fuerzas políticas, al hacer observable el período en que la burguesía logra recuperar la representación institucional como expresión legítima de la sociedad y consigue frenar la protesta social
Resumo:
Este trabajo se propone explorar las estrategias de legitimación que se desplegaron en un espacio local acotado durante la primera etapa del llamado "Proceso de Reorganización Nacional" en la Argentina. Desde una mirada centrada en los actores, en el análisis del discurso y en la historia local se analizarán los discursos que funcionarios y personalidades de relevancia nacional, provincial y local pronunciaron durante la Primera Exposición Internacional que se llevó a cabo en la ciudad bonaerense de Junín en octubre de 1977. Se intentarán vislumbrar los idearios y las representaciones que construyeron en torno a la figura de los productores agropecuarios, de los intendentes y de los municipios, como también sus vinculaciones con la dimensión simbólica del proyecto autoritario en el que pretendió sustentarse aquella dictadura
Resumo:
El concepto de extensión universitaria ha recorrido un largo trayecto desde sus primeras formulaciones durante el siglo XIX. A lo largo del mismo ha ido incorporando distintos significados, generalmente enmarcados en un modelo de relación asimétrica entre la sociedad y la población asistida. El concepto de apropiación social del conocimiento, de factura más reciente, pretende una aproximación más efectiva y dinámica del público al conocimiento científico. Sin embargo, ambos conceptos mantienen de manera más o menos explícita la relación lineal y asimétrica entre el conocimiento experto y el conocimiento profano. En este trabajo se reflexiona sobre la extensión universitaria como un marco de relación en el que tienda a conjugarse una dinámica de producción de decisiones basadas en la hibridación de conocimientos heterogéneos, con articulación de conocimientos universales y locales, en los que el público y los beneficiarios de las acciones de extensión universitaria asumen papeles activos para la construcción de las soluciones a los problemas acotados localmente.
Resumo:
Colombia has oceanic waters, catchment areas, like lakes, cienagas and swamps, water flows, like rivers, gorges and streams, small rivers and groundwater. The oceanic waters are the Caribbean Sea-1600 km and the Pacific Ocean-1300 km that comprise the north and west continental territory, respectively. Actually the Region of Darién, geographically bounded by the Carribean Sea to the north is becoming to be focused by studies due to use conflicts and disputes about water and a forest reserve on its territories. Considering its location, strategic at northwestern Colombia, frontier region with Central America, several dynamics are imposed. One of them is the implantation of a road system entitled Connecting Road of the Americas. This fact means the construction of an infra-structure that will cross a special zone formed by swamps and jungle known as The Darién Gap. Evidences of such interests are revealed by projects like the constructions of Turbo's Port in the Atlantic Ocean, Department of Antioquia and Tribugá's Port in the Pacific Ocean, Department of Choco, the mountain road and the coastal conection Colombia-Venezuela attending to the main intentions of the central region of the department (Metropolitan Area of Aburrá Valley-AMVA). Human settlements form a productive system, based on small and medium familiar agriculture's production, corresponding to the western portion and piedmont of Abibe's mountain at its antioquian portion, alluvial plan that forms the rivers on this area, the littoral zone that delimits the Carribean Sea, the Darién and Baudó Mountains and the gulf that receives, among other waters, the ones from Atrato and León, as well as the exodus process constitutes a forced exit resulting from actions of several armed groups. It can be identified intense historical, cultural, political and environmental relations, specially the last one associated with strategic ecosystems that are fundamental for the hydric regulation of the region, as well as food safety of the local inhabitants. Results from two researches (UPB, 2007 y 2010) reveals this quick transformation in the spatial re-configuration, demographical and economical indicators and the exacerbated fight for resources, damaging the extractive vocation in the Region. Path to commerce of illegalities (drugs, guns) and to implementation of the agroindustrial project for biofuel production, cooperation program that involves Venezuela, Brazil and Colombia. Appropriation modes allow the existence of strategies since global interests revealing a development logic that privileges the conception of an artificialized nature. Since the smallest portion of rural areas, specific modes of resources exploration are linked to imposed interests of transnational corporations. Disparate consequences are going deeper evidenced by social, technical and nature transformations, envisioning risks for the habitability's condition
Resumo:
Este trabajo se propone explorar las estrategias de legitimación que se desplegaron en un espacio local acotado durante la primera etapa del llamado "Proceso de Reorganización Nacional" en la Argentina. Desde una mirada centrada en los actores, en el análisis del discurso y en la historia local se analizarán los discursos que funcionarios y personalidades de relevancia nacional, provincial y local pronunciaron durante la Primera Exposición Internacional que se llevó a cabo en la ciudad bonaerense de Junín en octubre de 1977. Se intentarán vislumbrar los idearios y las representaciones que construyeron en torno a la figura de los productores agropecuarios, de los intendentes y de los municipios, como también sus vinculaciones con la dimensión simbólica del proyecto autoritario en el que pretendió sustentarse aquella dictadura
Resumo:
Colombia has oceanic waters, catchment areas, like lakes, cienagas and swamps, water flows, like rivers, gorges and streams, small rivers and groundwater. The oceanic waters are the Caribbean Sea-1600 km and the Pacific Ocean-1300 km that comprise the north and west continental territory, respectively. Actually the Region of Darién, geographically bounded by the Carribean Sea to the north is becoming to be focused by studies due to use conflicts and disputes about water and a forest reserve on its territories. Considering its location, strategic at northwestern Colombia, frontier region with Central America, several dynamics are imposed. One of them is the implantation of a road system entitled Connecting Road of the Americas. This fact means the construction of an infra-structure that will cross a special zone formed by swamps and jungle known as The Darién Gap. Evidences of such interests are revealed by projects like the constructions of Turbo's Port in the Atlantic Ocean, Department of Antioquia and Tribugá's Port in the Pacific Ocean, Department of Choco, the mountain road and the coastal conection Colombia-Venezuela attending to the main intentions of the central region of the department (Metropolitan Area of Aburrá Valley-AMVA). Human settlements form a productive system, based on small and medium familiar agriculture's production, corresponding to the western portion and piedmont of Abibe's mountain at its antioquian portion, alluvial plan that forms the rivers on this area, the littoral zone that delimits the Carribean Sea, the Darién and Baudó Mountains and the gulf that receives, among other waters, the ones from Atrato and León, as well as the exodus process constitutes a forced exit resulting from actions of several armed groups. It can be identified intense historical, cultural, political and environmental relations, specially the last one associated with strategic ecosystems that are fundamental for the hydric regulation of the region, as well as food safety of the local inhabitants. Results from two researches (UPB, 2007 y 2010) reveals this quick transformation in the spatial re-configuration, demographical and economical indicators and the exacerbated fight for resources, damaging the extractive vocation in the Region. Path to commerce of illegalities (drugs, guns) and to implementation of the agroindustrial project for biofuel production, cooperation program that involves Venezuela, Brazil and Colombia. Appropriation modes allow the existence of strategies since global interests revealing a development logic that privileges the conception of an artificialized nature. Since the smallest portion of rural areas, specific modes of resources exploration are linked to imposed interests of transnational corporations. Disparate consequences are going deeper evidenced by social, technical and nature transformations, envisioning risks for the habitability's condition
Resumo:
Buscamos avanzar en el conocimiento sobre cómo se desarrolla el movimiento de la sociedad argentina en su conjunto, analizado desde un caso particular que es el noreste del Chubut en el período que va desde la imposición de la hegemonía del capital financiero en 1989-1990 hasta el año 2005. Se pretende en esta tesis entender y conceptualizar en términos científicos cómo se mueve esa sociedad, de qué son expresión cada uno de sus conflictos, qué expresan los distintos sectores que se movilizan, qué expresan los cambios estructurales que se desarrollan, etc. Desde esta perspectiva nos interesa específicamente poder aportar al debate sobre cuáles son las opciones de plantear un proyecto alternativo de desarrollo para la provincia, la región y el país. Dentro del tema general de buscar comprender el movimiento de la sociedad, realizamos un abordaje de la realidad desde la utilización de un conocimiento acumulado y desde un recorte de esa realidad. Ese recorte lo realizamos a dos niveles. En primer lugar en términos espaciales: tomamos como base una región que denominamos el noreste de Chubut. Recortamos de la provincia del Chubut al área que tuvo el mayor crecimiento vinculado a los programas de polos de desarrollo durante las décadas del '60, '70 y parte del '80. La misma está delimitada por los actuales departamentos de Rawson y Biedma, de acuerdo a la división administrativa que toma la provincia desde 1957. En segundo lugar realizamos un recorte en términos temporales: abordamos como objeto de estudio al movimiento de la sociedad en esa región durante el período que va de 1989-1990 hasta el 2005. Consideramos que tomar este período nos permite observar el proceso de cambios que se generan con la realización de la hegemonía del capital financiero y el proceso de protestas, luchas y conflictos sociales que en el marco de estos cambios se desarrollan en la sociedad. La decisión de estudiar hasta el 2005 parte de considerar relevante comprender cómo continua el proceso después del 2001-2002. En esos años se produce la recuperación de la economía nacional, con un gran impulso para la región, lo cual genera el interés de poder precisar de qué se trata esta 'recuperación' y si estamos ante un movimiento orgánico o coyuntural de la economía. El período también nos permitió profundizar en el debate de las relaciones de fuerzas políticas, al hacer observable el período en que la burguesía logra recuperar la representación institucional como expresión legítima de la sociedad y consigue frenar la protesta social
Resumo:
El concepto de extensión universitaria ha recorrido un largo trayecto desde sus primeras formulaciones durante el siglo XIX. A lo largo del mismo ha ido incorporando distintos significados, generalmente enmarcados en un modelo de relación asimétrica entre la sociedad y la población asistida. El concepto de apropiación social del conocimiento, de factura más reciente, pretende una aproximación más efectiva y dinámica del público al conocimiento científico. Sin embargo, ambos conceptos mantienen de manera más o menos explícita la relación lineal y asimétrica entre el conocimiento experto y el conocimiento profano. En este trabajo se reflexiona sobre la extensión universitaria como un marco de relación en el que tienda a conjugarse una dinámica de producción de decisiones basadas en la hibridación de conocimientos heterogéneos, con articulación de conocimientos universales y locales, en los que el público y los beneficiarios de las acciones de extensión universitaria asumen papeles activos para la construcción de las soluciones a los problemas acotados localmente.
Resumo:
The density, species composition, and possible change in the status of pack ice seals within the Weddell Sea were investigated during the 1997/1998 summer cruise of the RV "Polarstern" (ANT-XV/3, PS48). Comparisons were made with previous surveys in the Weddell Sea where it was assumed that all seals were counted in a narrow strip on either side oft he ship or aircraft. A total of 15 aerial censuses were flown during the period 23 January - 7 March 1998 in the area bounded by 07°08' and 45°33' West longitude. The censused area in the eastern Weddell Sea was largely devoid of pack ice while a well circumscribed pack ice field remained in the western Weddell Sea. A total of 3,636 (95.4 %) crabeater seals, 21 (0.5 %) Ross seals, 45 (1.2 %) leopard seals and 111 (2.9 %) Weddell seals were observed on the pack ice during a total of 1,356.57 linear nautical miles (244.2 nm) of transect line censused. At a mean density of 21.16 1/nm**2 over an area of 244.2 nm, it is the highest densities on record for crabeater seals, density of up to 411.7 1/nm**2 being found in small areas. The overall high densities of seals (30.18 1/nm**2) recorded for the eastern Weddell Sea (27.46 1/nm**2, 0.27 1/nm**2, and 0.66 1/nm**2 for crabeater, leopard and Weddell seals respectively) is a consequence of the drastically reduced ice cover and the inverse relationship that exists between cover and seal densities. Ross seal densities (0.08 1/nm**2) were the lowest on record fort the area. It is suggested that seals largely remain within the confines of the pack ice despite seasonal and annual changes in its distribution. Indications are that in 1998 the El Niño has manifested itself in the Weddell Sea, markedly influencing the density and distribution of pack ice seals.
Resumo:
In central Antarctica, drainage today and earlier back to the Paleozoic radiates from the Gamburtsev Subglacial Mountains (GSM). Proximal to the GSM past the Permian-Triassic fluvial sandstones in the Prince Charles Mountains (PCM) are Cretaceous, Eocene, and Pleistocene sediment in Prydz Bay (ODP741, 1166, and 1167) and pre-Holocene sediment in AM04 beneath the Amery Ice Shelf. We analysed detrital zircons for U-Pb ages, Hf-isotope compositions, and trace elements to determine the age, rock type, source of the host magma, and "crustal" model age (T(C)DM). These samples, together with others downslope from the GSM and the Vostok Subglacial Highlands (VSH), define major clusters of detrital zircons interpreted as coming from (1) 700 to 460 Ma mafic granitoids and alkaline rock, epsilon-Hf 9 to -28, signifying derivation 2.5 to 1.3 Ga from fertile and recycled crust, and (2) 1200-900 Ma mafic granitoids and alkaline rock, epsilon-Hf 11 to -28, signifying derivation 1.8 to 1.3 Ga from fertile and recycled crust. Minor clusters extend to 3350 Ma. Similar detrital zircons in Permian-Triassic, Ordovician, Cambrian, and Neoproterozoic sandstones located along the PaleoPacific margin of East Antarctica and southeast Australia further downslope from central Antarctica reflect the upslope GSM-VSH nucleus of the central Antarctic provenance as a complex of 1200-900 Ma (Grenville) mafic granitoids and alkaline rocks and older rocks embedded in 700-460 Ma (Pan-Gondwanaland) fold belts. The wider central Antarctic provenance (CAP) is tentatively divided into a central sector with negative ?Hf in its 1200-900 Ma rocks bounded on either side by positive epsilon-Hf. The high ground of the GSM-VSH in the Permian and later to the present day is attributed to crustal shortening by far-field stress during the 320 Ma mid-Carboniferous collision of Gondwanaland and Laurussia. Earlier uplifts in the ~500 Ma Cambrian possibly followed the 700-500 Ma assembly of Gondwanaland, and in the Neoproterozoic the 1000-900 Ma collisional events in the Eastern Ghats-Rayner Province at the end of the 1300-1000 Ma assembly of Rodinia.
