Minéralisations cuprifères et volcanisme albitophyrique dans les ophiolites précambriennes de Bou Azzer (Anti-Atlas, Maroc)
Identifieur interne : 000532 ( France/Analysis ); précédent : 000531; suivant : 000533Minéralisations cuprifères et volcanisme albitophyrique dans les ophiolites précambriennes de Bou Azzer (Anti-Atlas, Maroc)
Auteurs : M. Leblanc [France]Source :
- Bulletin Volcanologique [ 0366-483x ] ; 1974-09-01.
Abstract
Abstract: There are many stratiform copper deposits (chalcopyrite, pyrite) in the volcano-sedimentary upper part of the Bou Azzer ophiolitic complex (upper Precambrian). The sulfides are genetically in relationship with a spilitic and keratophyric submarine volcanism. The Bou Azzer complex belongs to an ophiolitic lineament around the West-african craton; this lineament is a metallotect for copper ores.
Url:
DOI: 10.1007/BF02597108
Affiliations:
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<front><div type="abstract" xml:lang="en">Abstract: There are many stratiform copper deposits (chalcopyrite, pyrite) in the volcano-sedimentary upper part of the Bou Azzer ophiolitic complex (upper Precambrian). The sulfides are genetically in relationship with a spilitic and keratophyric submarine volcanism. The Bou Azzer complex belongs to an ophiolitic lineament around the West-african craton; this lineament is a metallotect for copper ores.</div>
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