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GEOLOGICAL CHARACTERISTICS AND ORE POTENTIAL OF GANGJIANG PORPHYRY COPPER-MOLYBDENUM DEPOSIT,TIBET

Zhou Wei-de

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Abstract

Gangjiang porphyry Cu,Mo deposit occurs in the spotted medium-grain amphibole-biotite monzonitic granite and is controlled by fault and joints and fractures near the fault.In the working area weak silicification,potassium alteration,pyritization,propylitization,argillation etc.are developed.Wide spread mineralization and big and high intensity geophysical and geochemical anomalies indicate that the deposit is of potential for large-super-large Cu,Mo deposit and proposals for further exploration are put forword.

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What this paper is about

Gangjiang porphyry Cu,Mo deposit occurs in the spotted medium-grain amphibole-biotite monzonitic granite and is controlled by fault and joints and fractures near the fault.In the working area weak silicification,potassium alteration,pyritization,propylitization,argillation etc.are developed.Wide spread mineralization and big and high intensity geophysical and geochemical anomalies indicate that the deposit is of potential for large-super-large Cu,Mo deposit and proposals for further exploration are put forword.

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Available abstract

Gangjiang porphyry Cu,Mo deposit occurs in the spotted medium-grain amphibole-biotite monzonitic granite and is controlled by fault and joints and fractures near the fault.In the working area weak silicification,potassium alteration,pyritization,propylitization,argillation etc.are developed.Wide spread mineralization and big and high intensity geophysical and geochemical anomalies indicate that the deposit is of potential for large-super-large Cu,Mo deposit and proposals for further exploration are put forword.

Key concepts: Geology, Biotite, Mineralization (soil science), Geochemistry, Porphyry copper deposit, Molybdenum, Copper, Amphibole

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GEOLOGICAL CHARACTERISTICS AND ORE POTENTIAL OF GANGJIANG PORPHYRY COPPER-MOLYBDENUM DEPOSIT,TIBET — Research Paper | ScholarLens