997 resultados para 584


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Aprovação pelo Plenário dos direitos dos indios em virtude do acordo de Líderes. Ineditismo da nova Carta Magna de contemplação dos direitos dos povos indígenas. Suspensão, pelo Presidente Ulysses Guimarães, de sessão por duas horas após a apreciação da matéria. Inexistência de acordo sobre a sequência de votação do título Disposições Constitucionais Gerais. Apresentação pelo Constituinte Matheus Iansen sobre a fixação do mandato do Presidente José Sarney.

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高原584是中国科学院西北高原生物研究所生态农业研究中心郜和臣研究员等培育的节水型春小麦新品种,原代号91D58-4,1999年11月25日经青海省农作物品种审定委员会审定通过,定名为"高原584",2003年2月26日又通过甘肃省农作物品种审定委员会第十九次会议审定。

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u.a.: Entgegennahme der Wertpapiere;

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1 Brief von Frederick Pollock an Hans J. Lichtenberger, 06.02.1947; 1 Briefe von Max Horkheimer an das Institute´s Advisory Board 11.01.1947; 1 Brief von Margot von Mendelssohn an Redman Van and Storage Co. (Santa Monica), 07.01.1947; 1 Brief von Gertrud Löwenthal an Redman Van and Storage Co. (Santa Monica), 03.01.1947;

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Geochemical analyses of organic matter were carried out on Quaternary sediments from Sites 582 and 583 (Nankai Trough) and on Pliocene to Miocene sediments from Site 584 (Japan Trench), DSDP Leg 87, to evaluate petroleum-generating potential and to characterize the organic matter. The vitrinite-huminite reflectances of indigenous materials for these sites are less than 0.3% indicating the immature nature of the sediments. The sediments, however, contain remarkable amounts of recycled organic materials. The Quaternary sediments from Sites 582 and 583 contain small amounts of amorphous organic matter (less than 0.75 wt.% organic carbon and 66-90% amorphous debris), which is composed of predominantly recycled, oxidized, and over-matured (or matured) Type III material. The amount of hydrocarbon yield indicates that those sediments have lean-source potential for commercial hydrocarbon generation. The Pliocene to Miocene sediments from Site 584 contain organic matter (0.3-1.09 wt.% organic carbon) of predominantly amorphous debris (68-96%) that originated in two sources, an indigenous Type II material and a recycled, over-matured material. Pyrolysis shows an upward increase in the section of hydrocarbon yield and the same trend is also observed in organic-carbon content. The amount of the yield indicates that the Miocene sediments have lean-to-fair source potential and the Pliocene sediments have fair-to-good source potential.

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Paleomagnetic measurements of sediment samples provide the magnetostratigraphy at Deep Sea Drilling Sites 582, 583, and 584 in the Nankai Trough and the Japan Trench. Drastic changes in the rate of sediment accumulation are documented by the magnetostratigraphic and biostratigraphic correlations. The changes in the accumulation rate correspond to the supply of sediments and variations in the accretionary process, which are directly related to the tectonic cycles in the geologic evolution of the Japanese island arc. Faults and folds within the drilled sedimentary sequences are oriented by paleomagnetic declination. Their directions and stress patterns are related to the relative plate motion along the trough and trench. The original remanent magnetization of the sediment was modified and remagnetized in the tectonic process of accretion by physical deformation, faulting, and intrusion of dewatering veinlets.