摘要
铅锌矿赋存于灯影组硅质条带白云岩中,局部产于筇竹寺组,脉状、透镜状,与峨眉山玄武岩喷发关系密切,属岩浆晚期热液成因。
The Pb-Zn deposit is in the Dengying Formation banded dolomitite,locally in the Qiongzhusi Formation,veined,lenticular.It is in close relation with the Emeishan basalt eruption and belongs to late magmatic hydrothermal genesis.
出处
《云南地质》
2010年第3期367-370,共4页
Yunnan Geology
关键词
构造控矿
碳酸盐岩赋矿
含矿热卤水
硫化矿与氧化矿
云南巧家仑房沟
Ore Structure Control
Ore-Bearing Carbonate rock
Ore-Bearing Thermal Brine
Sulfide Ore and Oxidized Ore
Cangfanggou
Qiaojia
Yunnan
