新疆维宝铅锌矿位于东昆仑北祁漫塔格复合沟弧带,分为维宝主矿段和维东两个矿点。维宝主矿段内无岩体出露,以条带状矿石为主,矿体严格赋存于中元古界狼牙山组矽卡岩中,层控特征明显;维东矿点内有三叠纪闪长花岗岩出露,矿体呈脉状,矿石以块状为主。矿区内广泛发育北西-南东向断裂。单从矿床地质上很难准确地限定维宝铅锌矿的成矿类型是矽卡岩型还是 The lead-zinc mine in Weibao, Xinjiang, is located in the North Qimantag Compound Grouped Arc Belt in the East Kunlun Mountains. There is no rock mass exposed in the main section of Weibao, with strip-shaped ore as the main body, and the ore body is strictly occured in the skarn of the Yelishan Formation in the Middle Proterozoic. The stratabound control features are obvious. There are three The feldspathic diorite granite is exposed. The ore bodies are vein-shaped and the ore is mainly massive. Northwest - South-East fault is widely developed in the mining area. It is difficult to accurately define the mineralization type of the lead-zinc mine in Weibao from skarn type