云南澜沦南现铜铅锌多金属矿成矿地质条件  

THE GEOLOGICAL CONDITIONS OF NANXIAN CU- PB- ZN MULTIMETALLIC METALLOGENESIS IN LANCANG,YUNNAN

作　　者：王炳华 黄跃 邢程 毕晓路 

机构地区：[1]云南省地质调查院,云南昆明650216

出　　处：《云南地质》2013年第4期433-435,共3页Yunnan Geology

摘　　要：铜铅锌矿赋存于中侏罗统花开左组浅色岩系和杂色岩系破碎带中,为受层位控制的砂页岩型铜矿及受构造控制的热液型铅锌多金属矿床。The Cu - Pb deposit is in the fracture zone of Middle Jurassic Huakaizuo Formation light color rock series and motley rock series, which is the Cu deposit of sandstone - shale type controlled by the horizone and the Pb - Zn multimetallic deposit of hydrothermal type controlled by the structure.

关 键 词：砂页岩型铜矿 地层构造控矿 沉积型和热液型 云南澜沧南现 

分 类 号：P618.42[天文地球—矿床学]