920 resultados para Juan Duns Escoto , Beato, ca. 1266-1308-Crítica i interpretació
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"Puestos a escoger entre nuestras concepciones poéticas y la fidelidad a la propia experiencia, finalmente optamos por esta última". Esa frase de Jaime Gil de Biedma bien podría formar parte de uno de los aforismos del libro Juan de Mairena, de Antonio Machado. La problemática de la conformidad de lo ético junto a lo estético nos lleva a la propuesta de ese artículo, es decir, el análisis del importante papel de la obra Juan de Mairena para la afirmación de una posición ético-poética en la obra de Jaime Gil
Resumo:
En el interior del proyecto fundacional de Onetti es posible leer tanto sus elecciones como sus exclusiones, su apuesta a la invención ficcional y su rechazo de las estéticas que califica de "nativistas" y "criollistas" así como su crítica al "compromiso literario". Tracé un itinerario de las huellas de estas exclusiones en sus textos, trayecto que se inicia en El pozo (1939) y en sus escritos contemporáneos de Marcha para articularse en Para una tumba sin nombre (1959). Propongo leer esta última nouvelle a partir de la siguiente pregunta: ¿cómo es posible armar un relato sobre "los miserables" en contra del relato realista y fuera de los mandatos del compromiso político?
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Se intenta leer el libro dibaxu de Juan Gelman escrito en sefardí desde el horizonte de la tradición poética latinoamericana. A través de la metáfora acerca de "la lengua salvada" de Elías Canetti (una imagen-aconteci¬miento de su propia autobiografía) es posible reflexionar sobre la condición de judío y también sobre la relación de la lengua materna y la infancia. En la estela de Rubén Darío y de los poetas posteriores que se vieron en la situación de cambiar de lengua por diversos motivos, Juan Gelman elige el ladino o español sefardí como un doble extrañamiento de la lengua poética: por un lado pertenece a la línea azkenazí y no sefardita y por el otro recupera el español del siglo XV en consonancia con otras propuestas poéticas en las que había ya ensayado el rescate de la voz de poetas españoles como San Juan de la Cruz , Santa Teresa y los poetas místicos árabes. Desde esta perspectiva, el artículo analiza desde la extraterritorialización de la lengua poética los temas de dibaxu y otros libros anteriores a fin de señalar ciertas constantes y sus modos diferentes de articulación en el texto poético.
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A partir del libro El Lectoespectador de Vicente Luis Mora (2012), y en relación con una serie de bibliografía crítica en torno a la internacionalidad del arte y la cultura contemporánea, el presente artículo procura enarbolar una reflexión sobre el desenvolvimiento de la teoría y la crítica española contemporánea dentro de lo que, a partir de Eloy Fernández Porta (2007), se denominó la era "Afterpop". Asimismo, se intenta postular una reflexión en torno a un nuevo estatuto de lo crítico-literario a partir del encuentro que se produce entre literatura y era digital
Resumo:
We present results of a detailed mineralogical and geochemical study of the progressive hydrothermal alteration of clastic sediments recovered at ODP Site 858 in an area of active hydrothermal venting at the sedimented, axial rift valley of Middle Valley (northern Juan de Fuca Ridge). These results allow a characterization of newly formed phyllosilicates and provide constraints on the mechanisms of clay formation and controls of mineral reactions on the chemical and isotopic composition of hydrothermal fluids. Hydrothermal alteration at Site 858 is characterized by a progressive change in phyllosilicate assemblages with depth. In the immediate vent area, at Hole 858B, detrital layers are intercalated with pure hydrothermal precipitates at the top of the section, with a predominance of hydrothermal phases at depth. Sequentially downhole in Hole 858B, the clay fraction of the pure hydrothermal layers changes from smectite to corrensite to swelling chlorite and finally to chlorite. In three pure hydrothermal layers in the deepest part of Hole 858B, the clay minerals coexist with neoformed quartz. Neoformed and detrital components are clearly distinguished on the basis of morphology, as seen by SEM and TEM, and by their chemical and stable isotope compositions. Corrensite is characterized by a 24 Å stacking sequence and high Si- and Mg-contents, with Fe/(Fe+Mg) ratio of = 0.08. We propose that corrensite is a unique, possibly metastable, mineralogical phase and was precipitated directly from seawater-dominated hydrothermal fluids. Hydrothermal chlorite in Hole 858B has a stacking sequence of 14 Å with Fe/(Fe+Mg) ratios of ? 0.35. The chemistry and structure of swelling chlorite suggest that it is a corrensiteychlorite mixed-layer phase. The mineralogical zonation in Hole 858B is accompanied by a systematic decrease in d18O, reflecting both the high thermal gradients that prevail at Site 858 and extensive sediment-fluid interaction. Precipitation of the Mg-phyllosilicates in the vent region directly controls the chemical and isotopic compositions of the pore fluids. This is particularly evident by decreases in Mg and enrichments in deuterium and salinity in the pore fluids at depths at which corrensite and chlorite are formed. Structural formulae calculated from TEM-EDX analyses were used to construct clay-H2O oxygen isotope fractionation curves based on oxygen bond models. Our results suggest isotopic disequilibrium conditions for corrensite-quartz and swelling chlorite-quartz precipitation, but yield an equilibrium temperature of 300° C ± 30° for chlorite-quartz at 32 m below the surface. This estimate is consistent with independent estimates and indicates steep thermal gradients of 10-11°/m in the vent region.
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The Pacific Decadal Oscillation (PDO), the leading mode of sea surface temperature (SST) anomalies in the extratropical North Pacific Ocean, has widespread impacts on precipitation in the Americas and marine fisheries in the North Pacific. However, marine proxy records with a temporal resolution that resolves interannual to interdecadal SST variability in the extratropical North Pacific are extremely rare. Here we demonstrate that the winter Sr/Ca and U/Ca records of an annually-banded reef coral from the Ogasawara Islands in the western subtropical North Pacific are significantly correlated with the instrumental winter PDO index over the last century. The reconstruction of the PDO is further improved by combining the coral data with an existing eastern mid-latitude North Pacific growth ring record of geoduck clams. The spatial correlations of this combined index with global climate fields suggest that SST proxy records from these locations provide potential for PDO reconstructions further back in time.
Resumo:
This data set contains the mineralogical analyses (binocular counting) of the 100-50 µm grain size fraction from bottom sediments collected by scientists of the V.P. Zenkovich Laboratory of Shelf and Sea Coasts (P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences) during the Project ''Arctic Shelf of the Eurasia in the Late Quaternary'' in a number of expeditions to the Barents, Kara, East Siberian and Chukchi Seas on board research vessels R/V Professor Shtokman, H/V Dmitry Laptev, H/V Malygin, and icebreaker Georgy Sedov between 1978 and 1990. The analyses have been carried out according to the methods published by Petelin V.P. (1961) in the Analytical Laboratory of the P.P. Shirshov Institute of Oceanology. Archiving and electronic publication was performed through a data rescue by Evgeny Gurvich in 2003.
Resumo:
This data set contains chemical composition of bottom sediments collected by scientists from the V.P. Zenkovich Laboratory of Shelf and Sea Coasts (P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences) during the Project ''Arctic Shelf of the Eurasia in the Late Quaternary'' in a number of expeditions to the Barents, Kara, East Siberian and Chukchi Seas on board research vessels R/V Professor Shtokman, H/V Dmitry Laptev, H/V Malygin, and icebreaker Georgy Sedov between 1978 and 1990. The analyses have been carried out in the Analytical Laboratory of the P.P. Shirshov Institute of Oceanology. Archiving and electronic publication was performed through a data rescue by Evgeny Gurvich in 2003.
Resumo:
The Global River Discharge (RivDIS) data set contains monthly discharge measurements for 1018 stations located throughout the world. The period of record varies widely from station to station, with a mean of 21.5 years. These data were digitized from published UNESCO archives by Charles Voromarty, Balaze Fekete, and B.A. Tucker of the Complex Systems Research Center (CSRC) at the University of New Hampshire. River discharge is typically measured through the use of a rating curve that relates local water level height to discharge. This rating curve is used to estimate discharge from the observed water level. The rating curves are periodically rechecked and recalibrated through on-site measurement of discharge and river stage.
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Este texto apunta algunos aspectos de la labor crítica desarrollada por Juan Daniel Fullaondo como director de Nueva Forma entre 1966 y 1975. En unos años de crisis disciplinar, esta publicación emprendió una revisión del legado arquitectónico español. Ante un panorama editorial aséptico, los textos críticos de Fullaondo aspiraron a mediar en el decurso histórico con el firme convencimiento de que la crítica, como tal, cumple con una función tan real como el de las propias obras construidas. ABSTRACT: This paper studies some aspects of the critical work that Juan Daniel Fullaondo developed at the Spanish magazine Nueva Forma (New Form), which directed from 1966 to 1975. In these critical years, this monthly publication, which was specialized in architecture and art, undertook a revision of the Spanish Architectural legacy. Despite the aseptic editorial panorama, Fullaondo’s texts firmly aspired to mediate in the collective cultural knowledge. His defense on criticism as a specialized discipline made him vindicate that it could have a role in History as real as masterly projects.
Resumo:
Digitalización Vitoria-Gasteiz Archivos y Bibliotecas Abril 1994 18-6