摘要
邦郎寨铅、锌多金属矿化体主要赋存于下元古界高黎贡山群下段(Pt1gl1)角闪片岩、板岩及硅质岩和结晶灰岩中,矿体由深部富含挥发分的含矿热液沿层间剥离滑脱构造充填成矿。并在断裂构造有利部位形成热液充填型铅、锌多金属隐伏矿体。
Banglangzhai Pb-Zn muhimetallic metallogenetic body is mainly in Lower Proterozoic Gaoligongs-han Group Lower Member （Pt1 gl1） hornblende schist, slate, siliceous rock and crystalline limestone. The ore- body is formed by the deep ore-bearing thermal fluid rich in volatile filling in the interlayer slide desquamation structure, and the hydrothermal filling type Pb-Zn multimetallic buried orebody is formed in the advantageous place of the fault structure.
出处
《云南地质》
2014年第4期561-565,共5页
Yunnan Geology
关键词
层间滑脱构造
热液充填矿床
云南盈江邦朗寨
Interlayer Slide Desquamation Struture
Hydrothermal Filling Ore Deposit
Banglangzhai, Yingjian, Yunnan
