1000 resultados para COOPERACION CIENTIFICA


Relevância:

10.00% 10.00%

Publicador:

Resumo:

Incluye Bibliografía

Relevância:

10.00% 10.00%

Publicador:

Resumo:

Da cuenta de las principales actividades operacionales realizadas por el sistema de la CEPAL desde el 21 periodo de sesiones de la Comision, especialmente en el marco de su resolucion 486(XXI): Cooperacion tecnica y economica entre paises y regiones en desarrollo.

Relevância:

10.00% 10.00%

Publicador:

Resumo:

Contiene asistencia, organizacion de los trabajos y resumen de los debates sobre los temas: restricciones al desarrollo sostenido en America Latina y el Caribe y requisitos para su superacion; cooperacion entre paises y regiones en desarrollo; reuniones de organos auxiliares, y reuniones regionales auspiciadas por CEPAL en preparacion de conferencias mundiales de las Naciones Unidas; programa de trabajo para 1990-1991, y actividades realizadas desde el 21 Periodo de Sesiones de la Comision por CEPAL, CELADE e ILPES; calendario de conferencias para 1988-1990; y admision de Aruba como miembro asociado de CEPAL.

Relevância:

10.00% 10.00%

Publicador:

Resumo:

In the S - SW region of Goiás State, Brazil, the Araxá Group is constituted of a metasedimentary sequence containing schistose and gneissic (garnet-biotite-quartz schists, feldspatic garnet-biotite-quartz schists, garnet-biotite-quartz paragneisses, with muscovite and locally amphibole, epidote, kyanite and staurolite. This sequence presents intercalations of metaul-tramafc rocks (serpentinite, actinolite schist, talc schist, chlorite schist), metamafc ones (amphibolite, amphibole schist containing or not garnet, garnet amphibolite) and associated granitic bodies. Chemically, the Araxá Group metasediments present peraluminous composition, showing enrichment in LILE, when compared with HFSE and REE, and displaying negative anomalies of Nb, Ta, Sr, P and Ti. Their chemical composition is that of greywake and the chemical characteristics of the sediments are generated in magmatic arcs. Isotopic data for Sm/Nd - model ages (TDM) between 1,04 - 1,51 and 1,76 - 2,26 Ga - and U/Pb (predominance of zircon with ages < 900 Ma) suggest that these metasediments have Neoproterozoic rocks as the source rocks. Chemical and isotopic characteristics of the studied metasediments suggest that their source are rocks originated in magmatic arcs and that they were deposited in a fore arc basin developed in the margins of Neoproterozoic island arcs.