有热铅锌矿地质特征及成因类型  

Geological Characteristics and Genetic Types of Youre Pb-Zn Deposit

作　　者：潘亮 刘期胜 PAN Liang;LIU Qi-sheng(Geologial Brigade of Sichuan Bureau of Geology and Mineral Resources,Emei 614200,China)

机构地区：[1]四川省地质矿产勘查开发局四0三地质队,四川峨眉614200

出　　处：《世界有色金属》2021年第17期80-81,共2页World Nonferrous Metals

摘　　要：有热铅锌矿位于中国西部特提斯-喜马拉雅构造域东缘,产于松潘-甘孜地槽褶皱系西部的玉树-义敦优地槽褶皱带中段,有热铅锌矿经过勘查工作,其规模目前达到中型。Youre lead-zinc mine area is located in the eastern margin of tethys-himalayan tectonic domain in western china,and occurs in the middle section of yushu-yidunyou geosyncline fold belt in the west of songpan-ganzi geosyncline fold system.After exploration,the hot lead-zinc ore has reached medium scale at present.

关 键 词：铅锌矿 海相喷流-沉积热液型 呷村式 

分 类 号：F426.1[经济管理—产业经济]