中文摘要:在1∶5万区域地质矿产调查中，发现西昆仑库科西鲁克一带有数个矿（床）点，涉及的矿种较多，有金、银、铜、铅锌、钼、钨和铁等。这些矿（床）点受区域性成矿断裂——库科西鲁克断裂的控制，分布在岩体边缘接触带的元古界—古生界变质岩中，分布区呈带状展布且较为集中，长约14 km，宽约6 km，包含2个矿床和6个矿点，构成了一个多金属矿集区，具有较好大中型多金属矿床的找矿前景。
Abstract:In the process of 1∶50 000 regional geological and mineral resources survey, several economic deposits were found in Kukexiluke area of West Kunlun. These ore deposits (spots) involve quite a lot of ore species such as Au, Ag, Cu, Pb, Zn, Mo, W and Fe and are distributed in Neoproterozoic and Palaeozoic metamorphic rocks along the rock body marginal contact belt, assuming zonal and fairly concentrated extension. The ore concentration area is 14 km in length and 6 km in width, comprising two deposits and six ore spots. These characteristics constitute a quite ideal polymetallic ore concentration area which has prospecting potential for large and intermediate polymetallic deposits.
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基金项目:“新疆阿克陶县恰尔隆一带1∶5万区域地质矿产调查 (XJQDZ 2006 18)” 项目
引用文本：
黄建国，崔春龙，李文杰，朱余银.2009.新疆西昆仑库科西鲁克多金属矿集区地质特征[J].矿床地质,28(2):218~223HUANG JianGuo, CUI ChunLong, LI WenJie and ZHU YuYin.2009.Geological characteristics of Kukexiluke polymetallic ore concentration area in West Kunlun, Xinjiang[J].Mineral Deposits28(2):218~223
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