The corridor of mineralization in the California gold district, in the Santander Department of Colombia

The corridor of mineralization in the California gold district, in the Santander Department of Colombia

In the Santander Massif of the Eastern Cordillera of Colombia, intense Pliocene to Holocene sulfide-rich gold mineralization occurs in a six kilometers long section of the La Baja fault zone, where it crosses partially migmatized gneisses and intrusions of Triassic-Cretaceous quartz monzonites and g...

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Bibliographic Details
Main Author: Wilson Scarpelli
Format: Article
Language:English
Published: Serviço Geológico do Brasil (CPRM) 2021-03-01
Series:Journal of the Geological Survey of Brazil
Subjects:
Andean Precambrian gneisses, Auriferous magnetite-hornblende gneiss, Fault veins, Breccia veins, Collision of Caribbean and Pacific plates
Online Access:https://jgsb.cprm.gov.br/index.php/journal/article/view/128

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https://jgsb.cprm.gov.br/index.php/journal/article/view/128

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