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ÉDITIONS UNIVERSITAIRES EUROPÉENNES Contrôle géologique de la minéralisation de Karuba Masisi; Nord-Kivu: Contrôle géologique de la minéralisation stano-wolframifère du secteur de Karuba, Masisi; Nord-Kivu (l'Est de RDCongo)

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Description

L’étude de terrain abordé sous les aspects cartographique, structural et métallogénique a permis de constater que dans l’ensemble, le secteur de Muvunyi Karuba (Bisunzu) est recoupé par plusieurs réseaux de cassures et de filons (pegmatites et de quartz). Les filons de quartz recoupent également la foliation minérale avec une particularité d’être cataclasé. Quant aux cassures ils ont une direction préférentielle de N76°E. Etant donné, les différentes fracturations qui ont eu lieu durant la phase de déformation, c’est-à-dire après cristallisation du magma, et que c’est au travers certaines de ces fractures qu’ont cristallisé les solutions hydrothermales, donc on conclut que: le premier réseau de filons de quartz résulte de la cristallisation des solutions hydrothermales très différenciées et riches en silice dont la circulation des fluides s’est faite préférentiellement à travers les fractures orientées N150°E/49°NW, tandis que pour le second réseau des filons de quartz, la cristallisation des fluides s’est faite préférentiellement suivant les plans orientés N10°E à N50°E.

Product Specifications

Format
paperback
Domain
Amazon UK
Release Date
11 January 2021
Listed Since
05 February 2021

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