952 resultados para He
Resumo:
La pregunta acerca de la relación entre escritura moderna, ligada a una firma, a una imagen de autor, y el acervo folklórico con el que dialoga, aún comporta una exigencia crítica en torno a la obra de Violeta Parra. La relación entre Décimas autobiográficas y Cantos folklóricos chilenos, desde una perspectiva que pone en el centro la escritura como experiencia, puede cuestionar el aspecto teleológico con que se ha leído ese diálogo. El punto de análisis será esa zona inestable de las huellas de escritura, la operación sobre el acervo colectivo. El cuerpo, como ausencia y metáfora, es uno de los puntos de intensidad donde esas huellas textuales de la tradición pugnan por cobrar sentido; pero esos espacios, para usar una palabra parriana, 'mudan' constantemente
Resumo:
Late Cretaceous (100-73 Ma) pelagic limestones were measured for helium concentration and isotopic composition to characterize the interplanetary dust flux using 3He as a tracer. In the Bottaccione section near Gubbio, Italy, three intervals of elevated 3He concentration were detected: K1 in the Campanian stage at ~79 Ma, K2 in the Santonian stage at ~ 85 Ma, and K3 in the Turonian stage at ~91 Ma. All three of these episodes are associated with high 3He/4He and 3He/non-carbonate ratios, consistent with their derivation from an enhanced extraterrestrial 3He flux rather than decreased carbonate sedimentation or dissolution. While K2 is modest in magnitude and duration and thus is of limited significance, K1 and K3 are each identified by a few myr interval with an ~4-fold enhancement in mean 3He flux compared with pre-event levels. Samples from ODP Hole 762C in the Indian Ocean spanning both K2 and K3 (93-83 Ma) confirm the presence of a peak in the Turonian stage, suggesting that K3 is a global event. The K1 and K3 3He events are similar in most respects to the two peaks previously detected in the Cenozoic, suggesting a similar origin. These have been attributed to a major asteroid collision in the Late Miocene and to a shower of either comets or asteroids in the Late Eocene. Based on the age and temporal evolution of K1, we suggest that it most likely records the collision which produced the Baptistina asteroid family independently dated at ~80 Ma. The K3 event is less easily explained. It is characterized by an unusually spiky and erratic temporal progression, suggesting an unusual abundance of very 3He rich particles not previously seen in the sedimentary 3He record. We suggest this episode arises either from a comet shower or from an asteroid shower possibly associated with dust-producing lunar impacts.
Resumo:
Fil: Bisignano, Julia Alejandra. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
A partir de las nuevas opciones que brinda el catálogo de próxima generación o NextGen, que han obligado a repensar el catálogo, también ha surgido un debate sobre la conveniencia o no de mantener el catálogo individual de cada biblioteca cuando se puede acceder a un catálogo colectivo. Se describen varios tipos de catálogos colectivos y se analizan sus ventajas y desventajas, sobre la base de siete parámetros: actualización de la información, control de calidad, desduplicación y consolidación, información de circulación, eficacia de la búsqueda, desempeño del catálogo y mantenimiento y administración. Se plantea el debate sobre la conveniencia de los catálogos colectivos y del catálogo individual como centro del llamado sistema integrado de gestión bibliotecaria y se pone énfasis en la situación de los catálogos colectivos en nuestro medio.
Resumo:
A partir de las nuevas opciones que brinda el catálogo de próxima generación o NextGen, que han obligado a repensar el catálogo, también ha surgido un debate sobre la conveniencia o no de mantener el catálogo individual de cada biblioteca cuando se puede acceder a un catálogo colectivo. Se describen varios tipos de catálogos colectivos y se analizan sus ventajas y desventajas, sobre la base de siete parámetros: actualización de la información, control de calidad, desduplicación y consolidación, información de circulación, eficacia de la búsqueda, desempeño del catálogo y mantenimiento y administración. Se plantea el debate sobre la conveniencia de los catálogos colectivos y del catálogo individual como centro del llamado sistema integrado de gestión bibliotecaria y se pone énfasis en la situación de los catálogos colectivos en nuestro medio.
Resumo:
La pregunta acerca de la relación entre escritura moderna, ligada a una firma, a una imagen de autor, y el acervo folklórico con el que dialoga, aún comporta una exigencia crítica en torno a la obra de Violeta Parra. La relación entre Décimas autobiográficas y Cantos folklóricos chilenos, desde una perspectiva que pone en el centro la escritura como experiencia, puede cuestionar el aspecto teleológico con que se ha leído ese diálogo. El punto de análisis será esa zona inestable de las huellas de escritura, la operación sobre el acervo colectivo. El cuerpo, como ausencia y metáfora, es uno de los puntos de intensidad donde esas huellas textuales de la tradición pugnan por cobrar sentido; pero esos espacios, para usar una palabra parriana, 'mudan' constantemente
Resumo:
Fil: Bisignano, Julia Alejandra. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
The accumulation of extraterrestrial 3He, a tracer for interplanetary dust particles (IDPs), in sediments from the Ontong Java Plateau (OJP; western equatorial Pacific Ocean) has been shown previously to exhibit a regular cyclicity during the late Pleistocene, with a period of ~100 ka. Those results have been interpreted to reflect periodic variability in the global accretion of IDPs that, in turn, has been linked to changes in the inclination of Earth's orbit with respect to the invariable plane of the solar system. Here we show that the accumulation in OJP sediments of authigenic 230Th, produced by radioactive decay of 234U in seawater, exhibits a 100-ka cyclicity similar in phase and amplitude to that evident in the 3He record. We interpret the similar patterns of 230Th and 3He accumulation to reflect a common origin within the ocean-climate system. Comparing spatial and temporal patterns of sediment accumulation against regional patterns of biological productivity and against the well-established pattern of CaCO3 dissolution in the deep Pacific Ocean leads to the further conclusion that a common 100-ka cycle in accumulation of biogenic, authigenic and extraterrestrial constituents in OJP sediments reflects the influence of climate-related changes in sediment focusing, rather than changes in the rate of production or supply of sedimentary constituents.
Resumo:
The paper presents characteristics of the Nd and Sr isotopic systems of ultrabasic rocks, gabbroids, plagiogranites, and their minerals as well as data on helium and hydrocarbons in fluid inclusions of the same samples. Materials presented in this publication were obtained by studying samples dredged from the MAR crest zone at 5°-6°N (U/Pb zircon dating, geochemical and petrological-mineralogical studies). It was demonstrated that variations in the isotopic composition of He entrapped in rocks and minerals were controlled by variable degrees of mixing of juvenile He, which is typical of basaltic glass for MAR (DM source), and atmospheric He. Increase in the atmospheric He fraction in plutonic rocks and, to a lesser degree, in their minerals reflects involvement of seawater or hydrated material of the oceanic crust in magmatic and postmagmatic processes. This conclusion finds further support in positive correlation between the fraction of mantle He (R ratio) and 87Sr/86Sr ratio. High-temperature hydration of ultrabasic rocks (amphibolization) was associated with increase in the fraction of mantle He, while their low-temperature hydration (serpentinization) was accompanied by drastic decrease in this fraction and significant increase in 87Sr/86Sr ratio. Insignificant variations in 143Nd/144Nd (close to 0.5130) and 87Sr/86Sr (0.7035) in most of gabbroids and plagiogranites as well as the fraction of mantle He in these rocks, amphibolites, and their ore minerals indicate that the melts were derived from the depleted mantle. Similar e-Nd values of gabbroids, plagiogranites, and fresh harzburgites (6.77-8.39) suggest that these rocks were genetically related to a single mantle source. e-Nd value of serpentinized lherzolites (2.62) likely reflects relations of these relatively weakly depleted mantle residues to another source. Aforementioned characteristics of the rocks generally reflect various degrees of mixing of depleted mantle components with crustal components (seawater) during metamorphic and hydrothermal processes that accompanied formation of the oceanic crust.