87 resultados para Depósitos minerais
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The study area is included in the geological context of the Goias Median Massif, a region where there are associations of Archean granite-gneiss complex (Block Moquém) and a Paleoproterozoic metavolcano-sedimentary sequence ( Pilar greenstone belt ). At the south of area, the greenstone sequence is partially overlain by Neopreoterozoic metasediments of the Araxá Group. The lithostratigraphic units of the Pilar greenstone belt define a shift from about N30W direction (north of the deposit) to N60 and 70W in the region south of the Jordino deposit, where are truncated by the Araxá Group rocks. Mineralogical associations described in this paper allow to indicate that the regional metamorphism that affected the rocks of the greenstone belt and Araxá Group, in the mapped area, reached the upper greenschist facies (garnet zone). Data obtained during mapping and by microtectonics analysis allow to indicate the existence of at least four deformational events that acted on the rocks of the Guarinos greenstone belt and Araxá Group, represented by the phases called Dn-1, Dn, Dn + 1 and Dn+2. It was observed that the pattern of sulphide porfitoblasts in mineralized levels is similar to garnet, biotite and muscovite porfiroblasts (tardi to post Dn) that marks the metamorphic peak of the area
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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Pós-graduação em Agronomia (Horticultura) - FCA
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Pós-graduação em Agronomia - FEIS
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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
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Pós-graduação em Geologia Regional - IGCE
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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El objetivo de este trabajo fue verificar la adhesión a la sugerencia de no recapsular agujas, basado en el comportamiento revelado por los cirujanos dentistas de la red municipal de salud bucal de la ciudad de Araçatuba en el estado de Sao Paulo, así como también observar la presencia de depósitos de material corto-punzante, las condiciones de llenado (por sobre el nivel recomendado o no) y su ubicación (cerca o lejos del profesional). Se recolectaron los contenedores de todas las unidades odontológicas de la red municipal. Después de la separación de otros elementos corto-punzante y materiales, además de la selección según como se recapsuló, se procedió al conteo de las agujas con la ayuda de una pinza larga y colocadas sobre una mesa revestida. Del total de 48 unidades odontológicas, se recolectaron 38 contenedores de elementos cortopunzantes con 5591 agujas desechadas. De estas, 2384 (42.7%) estaban recapsuladas por los dos lados, 2.177 (38.9%) en un lado y 1.030 (18.4%) sin recubrimiento. Se concluye que el índice de apego de estos profesionales a la recomendación de no recapsular las agujas es bajo. Los contenedores eran en la mayoría del tipo “Descarpak” y no estaban rellenados encima del nivel indicado; y a la vez se encontraban alejados del responsable de los desechos.
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Geophysical methods are widely used in mineral exploration for several types of mineral deposits. When combined with direct studies as geochemistry, a substantial increase in the probability of ore discovery is possible in mineral exploration activities. Electrical geophysical methods are particularly promising in studies related to the search of sulphides due to the contrast of physical properties electric resistivity and chargeability. This paper presents the results obtained from the application of Resistivity (DC) and Induced Polarization methods, through the electrical profiling technique, aiming at evaluating the potential mineral of a gabbro intruded in a metasedimentary sequence, in an area where several occurrences of gold and copper were described. This gabbro is ranked on the Basic-Ultrabasic stratiform bodies, which gather peridotites, gabbros, and layered anortosites. Three radial lines of electrical profiling were performed, spaced of 60° and crossing at the area center, with readings of electric resistivity and chargeability in Wenner-Schlumberger array. The association of low resistivity and high chargeability areas has allowed defining potentially mineralized zones related to structures that condition the drainage net in the gabbro domain. Grains of gold detected through geochemical prospection of alluvial sediments dowstream from the gabbro may have originated from leaching of ores deposited in fractures through the action of river waters within the gabbro domain, possibly consisting of sulphides and gold.
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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
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Pós-graduação em Geografia - FCT
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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)