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阳储岭钨钼矿床赋存于中酸性杂岩体中,黑云母是岩体中常见而普遍的矿物.笔者通过对黑云母地球化学及形成条件的研究,探讨了钨钼矿床类型及成矿特点.矿区地质概况阳储岭钨钼矿区位于九岭东西构造带九宫山-高台山东西构造隆起带与石门街新华夏系断裂复合部位.地层由震旦纪双桥山群浅变质岩系组成,近东西向展布.矿区东西向
The Yangzhuling tungsten-molybdenum deposit occurs in moderately acidic complex rock, and biotite is a common and common mineral in rock mass.Based on the study of biotite geochemistry and formation conditions, the author discusses the type and mineralization of tungsten-molybdenum deposit Features Geological Survey of the Mining Area The Yangzhuling tungsten-molybdenum mine is located in the Jiulongshan-Gaotai Mountain structural uplift belt and the Shihmen-Xinhuaxia fracture complex in the Jiuling Western-East structural belt.The strata consist of the shallow metamorphic rocks of the Shuangqiaoshan Group in the Sinian , Nearly east-west distribution. Mining east-west