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.
出处
《云南地质》
2013年第4期433-435,共3页
Yunnan Geology
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
Cu Deposit Sandstone -Shale Type
Ore Control of Strata -Structure
Sedimentation Type and Hydrothermal Type
Nanxian, Lancang, Yunnan
