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天宝山矿床位于四川省会理县境内,距离县城以北约50km,有公路与川滇公路相接,交通非常方便。矿床为一个非常典型的筒柱状的超大型铅锌矿;研究历史久,人员众多,但仍对构造控矿认识不清,构造成矿研究及其薄弱;根据区域构造特征,矿体实际特征给出天宝山铅锌矿构造控矿的一些新的认识,认为天宝山断裂为张性生长断裂,也即本矿床的控矿断裂,而并非前人所说的益门断裂西侧派生断裂。
The Tianbao Mountain deposit is located in Huili County, Sichuan Province, about 50km north of the county seat. There is a highway connecting Sichuan-Yunnan Highway and the traffic is very convenient. The deposit is a very typical cylindrical ultra-large lead-zinc mine. The study has a long history and many personnel, but it is still unclear about the structural ore-controlling and the research on the structural mineralization is weak. Based on the regional tectonic characteristics and the actual characteristics of ore bodies A new understanding of the tectonically controlled ore-forming of the Tianbaoshan Pb-Zn deposit suggests that the Tianbaoshan fault is an extensional growth fault, ie the ore-controlling fault of this deposit, rather than the westward derivative fault of the Yimen fault as previously described.