摘要
兰坪县白秧坪-富隆厂多金属矿,包含的矿种有银、铜、铅锌等,矿区中各类矿体呈脉状、透镜状均赋存于断裂构造破碎带中,矿体受断裂构造控制。矿体围岩主要为白垩系下统景星组(K_1j)碎屑岩,其次为中侏罗统花开左组(J_2h)岩层,矿床成因为中低温热液铜银多金属矿。
Baiyangping-Fulongchang multimetallic deposit,Lanping is composed of Ag,Cu,Pb-Zn mineral resources. The various ore bodies are veined,lanticular,in the fault zone. The ore body is controlled by the fault.The wall rock of ore body is mainly Lower Cretaceous Jingxing Formation（ K_1j） clastic rock,secondarily Middle Jurassic Huakaizuo Formation（ J_2h） rock bed. It is a middle-low T hydrothermal Cu-Ag multimetallic deposit.
出处
《云南地质》
2017年第2期262-266,共5页
Yunnan Geology
关键词
断层构造控矿
中低温热液矿
云南兰坪白秧坪富隆厂
Ore Control of Fault
Middle-Low T Hydrothermal Deposit
Baiyangping-Fulong
Lanping
Yunnan
