The Mississippi Valley-type Zn-Pb deposit of San Vicente, Central Peru: an Andean syntectonic deposit

Livre Chapitre de livre The Mississippi Valley-type Zn-Pb deposit of San Vicente, Central Peru: an Andean syntectonic deposit eng 2001 author Badoux Vincent 503797 author Moritz Robert 27897 author Fontboté Lluís 26840 Lluis Fontboté 191-195 10.1201/9781003077503-48 9789026518461 Ore-related structures at the Zn-Pb Missi ssippi Valley-type San Vicente deposit, Central Peru, display a system atic geom etry with respect to bedding and a regional thrust, interpreted as Miocene in earlier studies. Sparry dolom ite veins and breccia bodies have a constant NS direction, and are either perpendicular to bedding with dips ~70° to the east, or parallel to bedding, dipping ~25-30° westerly. Zebra structures dis- play identical concordant and discordant relationships relative to bedding. The preferential orientation of the gangue structures is interpreted within a dextral shear zone model, where they are either controlled by tensile fractures formed during thrusting or by pre-existent anis otropies, such as bedding plan es. It is concluded that the San Vicente deposit is coeval with the host thrust zone, and therefore Late Andean in age Dewey 550 42 Département des sciences de la Terre 154 false 692 Mineral Resources and Geofluids Mineral deposits at the beginning of the 21st century A. Piestrzynski c7ea0645-e6e1-4e06-8293-97ccfd8dcf94 Book chapter (Published version) Public badoux_moritz_fontbote_krakow2001.pdf 492379 application/pdf openAccess Faculté des sciences / Section des sciences de la Terre et de l'Environnement / Département des sciences de la Terre

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The Mississippi Valley-type Zn-Pb deposit of San Vicente, Central Peru: an Andean syntectonic deposit	Mineral deposits at the beginning of the 21st century			2001	888	386

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Badoux, Vincent