DISCUSSION ON ORE CONTROLLING CONDITION OF DULENGOU Cu-Co DEPOIST IN EASTERN KUNLUN METALLOGENIC BELT,QINHAI
Pan Tong
Abstract
Pan Tong
Abstract
The Dulengou Cu-Co deposit is located in the eastern area of Kunlun metallogenic belt. It was formed in the structural environment of island arc of late Palaeozoic Era. The ore bearing rock consits of late Cretaceous sericite quartz schist,later structural deformations enriched the ore body. The ore controlling factors are geodynamic mechanism,layer of volcanic rock,structurl deformations in Dulengou Cu-Co deposit.
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The Dulengou Cu-Co deposit is located in the eastern area of Kunlun metallogenic belt. It was formed in the structural environment of island arc of late Palaeozoic Era. The ore bearing rock consits of late Cretaceous sericite quartz schist,later structural deformations enriched the ore body. The ore controlling factors are geodynamic mechanism,layer of volcanic rock,structurl deformations in Dulengou Cu-Co deposit.
Key concepts: Geology, Sericite, Geochemistry, Schist, Paleozoic, Quartz, Volcano, Metamorphic rock