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西藏察隅县那阿钨矿在大地构造位置上处于拉达克—冈底斯弧盆系东段,隆格尔—工布江达复合岛弧的错高-德玛拉变质杂岩带上,属冈底斯—念青唐古拉陆块活动大陆边缘。是西藏地区近年来发现的具有代表性意义的矽卡岩型钨矿之一,属典型的接触交代型矽卡岩型钨矿床。白钨矿主要赋存在古—中元古界德玛拉岩群蛇躲岩组中,岩性主要由黑云片岩、二云片岩、石英片岩、板岩、角岩、变质石英砂岩及大理岩组成。矽卡岩化和钨钼成矿作用主要发育在岩体与含钙的围岩地层的接触带、或远离接触带的大理岩地
The Tazian tungsten deposit in Zayu, Tibet, is located in the eastern part of the Ladakh-Gangdese central-basin basin and the fault-raised demarcation complex of the Longger-Gongbujiangda composite island in the tectonic setting. The Seychelles - Nyainqentanglha Land Activities Continental Edge. It is one of the typical skarn-type tungsten deposits discovered in recent years in Tibet. It belongs to the typical contact metasomatic skarn type tungsten deposit. The scheelite mainly occurs in the snake-dikes of the De-Mala Group, Palaeo-Proterozoic. The lithology is mainly composed of biotite schist, ductile schist, schist schist, slate, horn rock, metamorphic quartz sandstone and marble composition. Skarnization and tungsten-molybdenum mineralization mainly occur in the contact zone between the rock mass and the calcium-bearing wall rock formation or the marble zone far from the contact zone