江西冷水坑铅锌矿田断裂构造与成矿作用  

THE FAULT AND METALLOGENESIS OF LENGSHUIKENG PB-ZN OREFIELD IN JIANGXI

作　　者：昝芳[1] 漆剑 杨启军[1] 

机构地区：[1]桂林理工大学地球科学学院,广西桂林541006 [2]江西省核工业地质局261大队,江西鹰潭335001

出　　处：《云南地质》2016年第4期483-487,共5页Yunnan Geology

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.

关 键 词：逆冲推覆断裂 构造控矿 江西冷水坑 

分 类 号：P611[天文地球—矿床学]