806 resultados para 963
Resumo:
A análise descrita nesta dissertação tem como objetivo a medida da seção de choque difrativa d963;/d|t| à energia no sistema do centro de massa de √s = 8 TeV. Os eventos usados para obter a seção de choque difrativa foram selecionados para processos de difração simples com um próton espalhado na região frontal e na região cinemática de 0,03 <|t| < 1,0 GeV e 0,03 < ξ < 0.1, usando os dados em comum obtidos em 2012 dos detectores CMS e TOTEM, o qual permite ter uma perspectiva mais detalhada do processo difrativo, devido à aceitação completa que oferece a combinação dos detectores. Os dados foram corrigidos devido à aceitação e eficiência do detector. A partir de uma parametrização exponencial da forma Ae ^Bt, o valor da inclinação do processo em que o próton espalhado é detectado em ambas as direções positiva da CMS é de B= -6,403 1,241 GeV- .
Resumo:
Review of: Vardah Shiloh, Millon 'Ivri-'Arami-'Aššuri bs-Lahag Yihude Zaxo (A New Neo-Aramaic Dictionary: Jewish Dialect of Zakho). Volume I: 'alef—nun\ Volume II: samex-tav. V. Shilo (16 Ben-Gamla Street), Jerusalem 1995. Pp. xiv + 488 (Vol. I); 489-963 (Vol. II). (Modern Hebrew, Zakho Jewish Neo-Aramaic). Hbk.
Resumo:
La ley de Estabilidad Ley 963 de 2005, es un instrumento jurídico cuyo objetivo en principio es lograr integrar el Estado Colombiano a un sistema de globalización económico, abierto a los procesos de activación de la inversión en nuestro país. Por medio de esta ley, el gobierno ha logrado pactar contratos con nuevos inversionistas, nacionales y extranjeros, a quienes se les garantiza seguir aplicando las mismas disposiciones legales y reglamentarias existentes al momento de realizar la inversión y que consideren relevantes o mejor aún motivantes para realizarla.
Resumo:
u.a. Spende von 25 Florin für den Schopenhauer-Fonds; Krankheit von Ludwig Noiré; Philosophie Schopenhauers; Deutsche Zeitung; Antisemitismus in Wien; Schopenhauer und die Juden; Rezeption Schopenhauer; Kritik Julius Frauenstädt und Ernst Otto Timotheus Lindner; Emil Reich; Tragödie; Friedrich Hebbel; Gotthold Ephraim Lessing; Franz Grillparzer; Johannes Immanuel Volkelt; Foucher de Careil; Frankreich; Georg Wilhelm Friedrich Hegel; Ethik; Sixtinische Madonna; Friedrich Schierholz; Julius Hamel; Stadtrat Beck;
Resumo:
Here we present a high-resolution faunal, floral and geochemical (stable isotopes and trace elements) record from the sediments of Ocean Drilling Program Site 963 (central Mediterranean basin), which shows centennial/millennial-scale resemblance to the high-northern latitude rapid temperature fluctuations documented in the Greenland ice cores between 20 and 70 kyr BP. Oxygen and carbon isotopes, planktic foraminifera and calcareous nannofossil distributions suggest that Dansgaard-Oeschger (D/O) and Heinrich events (HE) are distinctly expressed in the Mediterranean climate record. Moreover, recurrent though subdued oscillations not previously identified in the Lateglacial Mediterranean sediments document a significant centennial-scale climate variability in the basin that is greater than previously thought. Alternations between climate regimes dominated by polar outbreaks during D/O stadials and warm D/O interstadials, with associated intensification of continental runoff, are well expressed in the ODP Site 963. These place the Mediterranean basin as an often overlooked recorder of the interplay between large- and regional- scale climate controls at intermediate latitudes, and of the possible interactions between different components of the climate system. Significant changes in Ba/Ca values measured in Globigerinoides ruber shells from a number of D/O stadials and interstadials suggest enhanced freshwater input from the north-eastern Mediterranean borderland during the D/O interstadials. However, the short duration of 3D stratification events never led to complete oxygen consumption along the water column, but clear effects of sluggish 3D circulation in the basin are testified to by negative excursions in d13C measured in selected species of planktic and benthic foraminifera. HEs are constantly associated with lightening in the d18O record of planktic foraminifera, possibly because of the impact of iceberg melting in the Iberian Margin on Mediterranean thermohaline circulation. Interestingly, in two cases in particular, HE2 and HE5, fresher water inputs also affected deeper horizons of intermediate waters, suggesting a basin-wide impact.