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Controle geológico da mineralização de Karuba Masisi; Kivu do Norte: Controle geológico da mineralização de stano-wolfram no setor Karuba, Masisi; Kivu Norte (Leste da RDCongo)

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Description

O estudo de campo abordado sob os aspectos cartográficos, estruturais e metalogénicos permitiu constatar que, no seu conjunto, o sector de Muvunyi Karuba (Bisunzu) é intersectado por várias redes de quebras e veias (pegmatites e quartzo). As veias de quartzo também interceptam a foliação mineral com a peculiaridade de serem cataclastadas. Quanto às fracturas, elas têm uma direcção preferencial de N76°E. Dadas as diferentes fraturas ocorridas durante a fase de deformação, ou seja, após a cristalização do magma, e que é através de algumas dessas fraturas que as soluções hidrotermais cristalizaram, concluímos que : a primeira rede de veias de quartzo resulta da cristalização das soluções hidrotermais, que são altamente diferenciadas e ricas em sílica, e cuja circulação dos fluidos ocorreu preferencialmente através de fraturas orientadas N150°E/49°NW, enquanto que para a segunda rede de veias de quartzo, a cristalização dos fluidos ocorreu preferencialmente em planos orientados N10°E a N50°E.

Product Specifications

Format
paperback
Domain
Amazon UK
Release Date
26 May 2021
Listed Since
27 May 2021

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