摘要
江西冷水坑银铅锌矿田矿断裂构造发育,断裂活动与成矿的关系十分密切,尤其是北西向F2逆冲推覆断裂构造,是矿田乃至区域的导岩、导矿构造,含矿热液沿这些断裂裂隙运移充填构成工业矿体。
The fault is developed in Lengshuikeng Pb-Zn-Ag orelield, Jiangxi. And it is in close relation with the metallogenesis, especially the NW thrust fault F2 which is the guide rock and ore structure in orefield, e-ven regionally. The ore-bearing thermal fluid migrates and fills along this fault fissure and forms the commercial ore body.
出处
《云南地质》
2016年第4期483-487,共5页
Yunnan Geology
关键词
逆冲推覆断裂
构造控矿
江西冷水坑
Thrust Fault
Ore Control of Structure
Lengshuikeng, Jiangxi
