968 resultados para National Personnel Records Center (U.S.)--Records and correspondence
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Includes bibliography
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Includes bibliography
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Incluye Bibliografía
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Incluye Bibliografía
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Includes bibliography
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First meeting on European soil. The Nineteenth Meeting of National Customs Directors of Latin America, Spain and Portugal was held in Palma, Mallorca, Spain, from 2 to 6 November 1998. The opening session stressed the importance of this being the first meeting held on European soil, and members were urged to pool their efforts to develop closer cooperative ties between the region's customs services.
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The seventeenth Meeting of National Customs Directors of Latin America, Spain and Portugal was held in Santa Cruz, Bolivia from 27 to 31 January 1997. The meeting was attended by representatives from Argentina, Bolivia, Brazil, Chile, Cuba, Dominican Republic, El Salvador, Mexico, Nicaragua, Panama, Paraguay, Peru, Portugal, Spain, Uruguay and Venezuela. Observers from Australia, France, Japan and the United States were also present. Representatives of the following international organizations also attended the meeting: Association of Customs Agents of Uruguay, International Association of Professional Customs Agents (ASAPRA), Latin American Integration Organization (LAIA), Inter-American Development Bank (IDB), Economic Commission for Latin America and the Caribbean (ECLAC), United Nations Conference on Trade and Development (UNCTAD), Latin American Convention of Courier Enterprises (CLADEC), Central American Institute of Business Administration (INCAE), Board of the Cartagena Agreement (JUNAC), Organization of American States (OAS), World Customs Organization (WCO), and Postal Union of the Americas, Spain and Portugal (PUASP).
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The twentieth Meeting of National Customs Directors of Latin America, Spain and Portugal was held from 26 to 29 October 1999 in Cancún, Quinta Roo, Mexico. Working groups discussed issues relating to control, harmonization of customs procedures, strategic alliances for combating commercial fraud, integrity and the impact of the year 2000 computer problem on customs services. At the plenary meeting of this session, agreement was reached on 30 points.Uruguay, headquarters for the twenty-first meeting: The delegation of Uruguay's offer to host the twenty-first meeting in October 2000 was accepted.
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Caxias é um depósito de ouro orogênico do fragmento cratônico São Luís, que é correlacionável aos terrenos Riacianos do Cráton Oeste-Africano. O depósito se formou após o metamorfismo regional (estimado em 2100 ± 15 Ma) e está hospedado em zona de cisalhamento que secciona xistos do Grupo Aurizona (2240 ± 5 Ma) e o Microtonalito Caxias. O microtonalito foi aqui datado em 2009 ± 11 Ma, e representa um estágio magmático tardio na evolução do fragmento cratônico São Luís. Cristais de zircão com idades de 2139 ± 10 Ma foram herdados da fonte magmática ou são produto de contaminação durante a intrusão. A composição dos isótopos de chumbo sugere que granitoides de arco de ilhas de ca. 2160 Ma são a fonte provável para o Pb incorporado na pirita relacionada com o minério. Sericita hidrotermal mostra idade 40Ar/39Ar de 1990 ± 30 Ma, que, combinada com a idade de posicionamento do microtonalito hospedeiro, limita o evento mineralizador ao intervalo 2020-1960 Ma.
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During the Ediacaran, southern Brazil was the site of multiple episodes of volcanism and sedimentation, which are best preserved in the 3000 km(2) Camaqua Basin. The interlayered sedimentary and volcanic rocks record tectonic events and paleoenvironmental changes in a more than 10 km-thick succession. In this contribution, we report new U-Pb and Sm-Nd geochronological constraints for the 605 to 580 Ma Born Jardim Group, the 570 Ma Acampamento Velho Formation, and a newly-recognized 544 Ma volcanism. Depositional patterns of these units reveal the transition from a restricted, fault-bounded basin into a wide, shallow basin. The expansion of the basin and diminished subsidence rates are demonstrated by increasing areal distribution and compressed isopachs and increasing onlap of sediments onto the basement to the west. The Sm-Nd isotopic composition of the volcanic rocks indicates mixed sources, including crustal rocks from the adjacent basement. Both Neoproterozoic and Paleoproterozoic sources are indicated for the western part of the basin, whereas only the older Paleoproterozoic signature can be discerned in the eastern part of the basin. (C) 2011 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.