摘要
云南富源县富盛铅锌矿矿体呈层状、似层状组成矿群,赋存于下二叠统茅口组(P 1 m)碳酸盐岩层间断裂带中,该矿为构造控制的中-低温热液矿床。矿区内南北向的主干断裂是主要的导矿构造,而层间破碎带则直接控制着矿体的分布和形态。
The orebody of Fusheng Pb-Zn deposit in Fuyuan,Yunnan is Bedded,stratoid,grouped in Lower P Maokou Formation(P 1m)carbonatite interlayer fault,which is a middle-low T hydrothermal deposit controlled by the structure.The NS principal fault in the orefield is the main metallogenesis transmission structure;whereas the distribution and shape of orebody are controlled directly by the interlayer fracture zone.
作者
吕召俊
LU Zhao-jun(Fusheng Pb-Zn Deposit Company(Ltd)of Qujing,Kunming 650217)
出处
《云南地质》
2019年第4期426-430,共5页
Yunnan Geology
关键词
构造控矿
热液型矿床
云南富盛
Ore Control of Structure
Hydrothermal Deposit
Fusheng
Yunnan
