Please use this identifier to cite or link to this item: http://repositorio.unicamp.br/jspui/handle/REPOSIP/342775
Type: Artigo
Title: The Cristalino IOCG deposit: an example of multi-stage events of hydrothermal alteration and copper mineralization
Author: Craveiro, G.S.
Xavier, R.P.
Nobre Villas, R.N.
Abstract: The Cristalino deposit is located 40 km east of Sossego mine, Carajas. The orebody lies along a NW-SE-striking shear zone and is mainly hosted by the Neoarchean bi-modal volcanics of the Grao Para Group. Field work and petrographic data seconded by SEM-EDS analysis allowed recognizing an early sodic metasomatism that was followed by calcic-ferric, potassic and propylitic alterations, and finally by carbonatization. The volcanic rocks were altered under deformation regimes that changed from ductile-brittle to brittle. The deposit resulted from two mineralizing stages. The early stage took place at a greater depth and produced an ore association composed chiefly of chalcopyrite, pyrite, and magnetite as disseminations, breccia and veins particularly in Ca-Fe altered rocks. The later stage occurred at a shallower depth and formed a practically magnetite- free ore association, consisting essentially of chalcopyrite ± pyrite ± hematite in breccias and veins generated mostly during the potassic alteration. These ore associations indicate that the hydrothermal system evolved with temperature decrease and increase in fO 2 , Cu/Fe ratio and sulfur activity. Cristalino is conceived as a multi-stage IOCG deposit similar to others lying in the Carajas E-W corridor of IOCG systems.
Subject: Cobre - Minas e mineração
Transformação hidrotérmica
Country: Brasil
Editor: Sociedade Brasileira de Geologia
Rights: Aberto
Identifier DOI: 10.1590/2317-4889201920180015
Address: https://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892019000100308
Date Issue: 2019
Appears in Collections:IG - Artigos e Outros Documentos

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