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金达整装勘查区处于特提斯-喜马拉雅造山带的中东部,近十年来找到了蒙亚啊、亚贵拉、洞中拉、洞中松多等大-中型Pb-Zn矿床,构成了西藏重要的铅锌矿集区。但是对于此成矿带的地球化学特征较薄弱,且认识不统一。该勘查区已经发现的金属矿床主要是围绕以铅、锌、铜等多种金属元素为主的铅锌类矿床,勘查区的矿种类型主要可以统分为两类:一是以Ag、Cu、Pb、Zn中低温成矿元素为主的铅锌类矿种为主的矿床;另一种是以W、Sn、Mo、Bi高温成矿元素为主的钼矿床。前者已查明的
The Jinda prospecting area is located in the middle and eastern part of the Tethys-Himalayas orogenic belt. In the past ten years, large-medium Pb-Zn deposits such as the Mongolian-Yaghua, Yaquila, Dongzhongla and Songdo have been found, forming Tibet Important lead-zinc deposits. However, the geochemical characteristics of the metallogenic belt are weaker and their understanding is not uniform. The metal deposits that have been discovered in this exploration area mainly surround the lead-zinc deposits dominated by various metal elements such as lead, zinc and copper. The types of ore deposits in the exploration area can be divided into two categories: one is Ag, Cu , Pb, Zn low-temperature ore-forming elements mainly lead-zinc ore deposits; the other is W, Sn, Mo, Bi ore elemental molybdenum deposit. The former has been identified