992 resultados para 325-M0041A
Resumo:
A Constituinte pode decidir amanhã se muda o Regimento Interno, para permitir a apresentação de emendas ao projeto de Constituição aprovado pela Comissão de Sistematização. O Senador Mauro Benevides (PMDB-CE), vice-presidente da Assembleia Nacional Constituinte (ANC), comenta sobre a proposta que altera o regimento para permitir que cada Constituinte tenha direito a três emendas e seis destaques. O grupo "Centrão" já recolheu 324 assinaturas para exigir a mudança do regimento. O Deputado Daso Coimbra (PMDB-RJ) explica que não se pretende modificar trechos inteiros do Projeto da Constituição. Em reunião com o presidente da ANC, o Deputado Ulysses Guimarães (PMDB-SP), integrantes do "Centrão" levaram a proposta do grupo. O Deputado Ricardo Fiuza (PFL-PE) comenta os resultados da reunião. O Senador Mário Covas (SP) admite que se abra espaço para mudanças com a alteração do regimento, mas não aceita a apresentação de um substitutivo em bloco. Uma pesquisa de opinião realizada pelo IBOPE em 23 Estados mostra o que pensa o brasileiro sobre o sistema de governo. Os Deputados Oswaldo Bender (PDS-RS), Paulo Delgado (PT-MG), Antônio Câmara (PMDB-RN) comentam o resultado da pesquisa.
Resumo:
The thermoluminescence intensity as a function of gamma-ray dose of the 325 degreesC peak, in quartz grains extracted from sea sediments and from fluvial aeolic dunes, is studied. It is found that the response curve at low doses has a concavity directed opposite to that of quartz grains extracted from archaeological potteries. To explain this behavior a model is proposed here based on oxygen vacancies and [AlO4/h](0) centers. The experimentally observed ESR intensity of E-I'-centers as a function of radiation dose can also be explained by this model.
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75 Briefe mit Beilagen zwischen Prof. Frances Bartlett Kinne und Max Horkheimer, 1956-1973; 7 Briefe mit Beilagen zwischen Prof. Otto Kirchheimer und Max Horkheimer, 1952-1954; 19 Briefe mit Beilagen zwischen Prof. Guido Kisch und Max Horkheimer, 1955-1956; 23 Briefe mit Beilagen zwischen Walter Kittel (Oberbaurat i. R.), 1964-1973; 14 Briefe mit Beilagen zwischen Jules Klanfer und Max Horkheimer, 1963-1964; 4 Briefe mit Beilagen zwischen Prof. Otto Klineberg und Max Horkheimer, 1960-1961; 1 Brief von Max Horkheimer an Otto Klineberg (Psychologe), 22.6.1960;
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u.a.: Gustav Wilhelm Körber; Arthur Schopenhauer; Giacomo Leopardi;
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4 Briefe zwischen Walter Benjamin und Cecilia Razovsky; 6 Briefe zwischen Cecilia Razovsky und Max Horkheimer; 1 Brief von Cecilia Razovsky an den American Consul, 17.11.1939; 1 Brief von Antonio Sols an Max Horkheimer, 30.10.1940; 1 Brief von Max Horkheimer an Antonio Sols, 11.10.1940; 1 Brief (Abschrift, Auszug) an A. R. L. Gurland von Frau Gurland, 11.10.1940; 3 Briefe zwischen dem Emergency Rescue Committee (New York) und Max Horkheimer, August 1940; 1 Brief von Max Horkheimer an Pastor del Rio, 17.07.1940; 1 Brief von Max Horkheimer an J. Wavrinek, 17.07.1940; 1 Brief von Theodor W. Adorno an Gershom Scholem, 16.07.1940; 1 Brief von Max Horkheimer an Hans Schaudinger, 13.07.1940; 1 Brief von Max Horkheimer an George S. Messersmith, 08.07.1940; 1 Brief von Max Horkheimer an Adolph Kates, 05.07.1940; 1 Brief von Max Horkheimer an Adolph Kates, 29.06.1940; 2 Briefe zwischen dem Refugee Section of the American Friends Service Committee (Philadelphia) und Max Horkheimer, Mai 1940; 2 Briefe von Egon Wissing an Max Horkheimer, 1940; 1 Brief von Max Horkheimer an die Economy Blue Print Co. (New York), 25.05.1940; 1 Brief von Werner Kraft an Max Horkheimer, 30.04.1940;
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Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and d18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1-2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.