摘要
岩头村铜矿矿体主要受断裂构造控制,矿体呈透镜状、似层状沿断层构造破碎带产出,围岩为上三叠统小定西组第二段(T_3xd^2)中酸性火山岩,属中高温热液矿床。
The ore body ol Yantoucun Cu deposit is mainly controlled by the fault structure, which is lenticu-lar ,stratoid along the fault fracture zone. The wall rock is Upper Triassic Xiaodingxi Formation Member 2 （Tgxd2） intermediate-acid volcanic rock, belonging to the middle-high T hydrothermal deposit.
出处
《云南地质》
2016年第4期542-546,共5页
Yunnan Geology
关键词
断层构造控矿
中高温热液型矿床
云南兰坪岩头村
Ore Control ol Fault
Middle-High T Hydrothermal Deposit
Yantoucun, Lanping, Yunnan
