湖南省郴州市黄泥坳铅锌矿、萤石矿地质特征及矿床成因  

Geological characteristics and genesis of the Huangniao lead⁃zinc and fluorite deposit in Chenzhou,Hunan

作　　者：禹俊 闵钊 张意欣 YU Jun;MIN Zhao;ZHANG Yixin(Mineral Resources Survey Institute of Hunan Province,Chenzhou 423000,Hunan,China)

机构地区：[1]湖南省矿产资源调查所,湖南郴州423000

出　　处：《资源信息与工程》2024年第3期6-9,共4页Resource Information and Engineering

摘　　要：本文对郴州市黄泥坳铅锌、萤石矿的地质特征、矿床成因进行了总结,认为矿床受地层与构造叠加控矿,矿区位于王仙岭和千里山两大岩体之间,岩浆活动带来了成矿物质来源,并提供了热动力。本文为区域上进一步寻找类似成因的矿床提供了一定的依据。This paper summarized the geological characteristics and genesis of the Huangniao lead⁃zinc and fluorite deposit in Chenzhou.It is believed that the deposits are influenced by the overlapping control of strata and structures,with the mining area located between the two major rock masses of Wangxianling and Qianlishan.Magmatic activity serves as the source of ore⁃forming materials and provides thermal power.These findings provided a basis for further searching of deposits of similar origins in the region.

关 键 词：黄泥坳矿区 地质特征 控矿地质条件 矿床成因 

分 类 号：P618[天文地球—矿床学]