2008Mineral Resources and GeologyRequires access

Geological characteristics and genesis discussion of the Beidabate porphyry Cu-Mo deposit in Wenquan County,Xinjiang

Wang Yu-shui

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Abstract

The Beidabate porphyry Cu-Mo deposit occurs in Variscan rhyolite porphyry with its orebodies presenting in veins.The surface of Cu orebody is covered with oxide,while the Mo orebody mainly locates in the rhyolite porphyry of deep part.The mineralization presents a double-layer mineralizing structure mode with the upside being Cu mineralization and the underside being Mo mineralization,and occurs in veinlet disseminating state.The genesis type of this deposit is porphyry Cu-Mo deposit.

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The Beidabate porphyry Cu-Mo deposit occurs in Variscan rhyolite porphyry with its orebodies presenting in veins.The surface of Cu orebody is covered with oxide,while the Mo orebody mainly locates in the rhyolite porphyry of deep part.The mineralization presents a double-layer mineralizing structure mode with the upside being Cu mineralization and the underside being Mo mineralization,and occurs in veinlet disseminating state.The genesis type of this deposit is porphyry Cu-Mo deposit.

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Available abstract

The Beidabate porphyry Cu-Mo deposit occurs in Variscan rhyolite porphyry with its orebodies presenting in veins.The surface of Cu orebody is covered with oxide,while the Mo orebody mainly locates in the rhyolite porphyry of deep part.The mineralization presents a double-layer mineralizing structure mode with the upside being Cu mineralization and the underside being Mo mineralization,and occurs in veinlet disseminating state.The genesis type of this deposit is porphyry Cu-Mo deposit.

Key concepts: Rhyolite, Mineralization (soil science), Geology, Geochemistry, Porphyry copper deposit, Hydrothermal circulation, Volcano, Seismology

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Geological characteristics and genesis discussion of the Beidabate porphyry Cu-Mo deposit in Wenquan County,Xinjiang — Research Paper | ScholarLens