999 resultados para Irving, Washington, 1783-1859.
Resumo:
Fil: Jumar, Fernando. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
El presente trabajo consiste en notas de una investigación en curso. Las mismas dan cuenta del dispositivo de escritura de Washington Cucurto en relación con la pija de oro del negro que se implanta el narrador/personaje Tyson Grande/ Washington Cucurto/Norberto Vega en Las aventuras del Señor Maíz (2005). Nos interesa pensar que esa prótesis quirúrgica y corporal exhibe fuerzas (en un sentido deleuziano) que rigen toda la producción de Cucurto/Vega: la social, la económica, la sexual y la cultural latinoamericana. La pija de oro es, entonces, una condensación poética que exhibe la máquina de escritura como una bestia melancólica en cuyo cuerpo se desequilibran fuerzas en disputa por la literatura
Resumo:
Fil: Jumar, Fernando. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Meteorological observations during NARCISSUS cruise from St. Lucia to New York started at 1783-03-08
Resumo:
The bimodal, alkaline volcanic suite of the Kap Washington Group (KWG) at the northern coast of Greenland was investigated during the BGR CASE 2 expedition in 1994. Geochemical and Nd and Sr isotopic data are presented for basalts to rhyolites of the KWG and of related basaltic dykes cutting Lower Paleozoic sediments. In the evd(t) vs. (87Sr/86Sr)t diagram, the KWG basalts and rhyolites follow a common mixing trend with increasing crustal contamination from basic to acid volcanites. Assimilation of pre-existing crustal rocks during formation of the rhyolitic melt is documented by Nd model ages of 0.9-1.2 Ga and by different fractionation trends for the basalts and the rhyolites in the Y vs. Zr diagram. Petrographical and geochemical features indicate intra-plate volcanism which was active most probably during a continental rifting phase. A new Rb/Sr whole rock age on rhyolites of 64 ±3 Ma, corresponding to the result of LARSEN (1982), confirms that the volcanic activity lasted until the Cretaceous-Tertiary boundary. 40Ar139Ar dating on amphibol separates from a comendite yielded strongly disturbed age spectra with a minimum age of 37.7 ±0.3 Ma. This age is interpreted to date a hydrothermal overprint of the volcanic rocks related to compressive tectonics which led to the overthrust of basement rocks over the Kap Washington Group.
