郴州柿竹园野鸡尾南铅锌矿控矿因素与成矿规律  

Ore-controlling factors and mineralization regularity of Pb-Zn deposit in south Yejiwei of Shizhuyuan, Chenzhou

作　　者：赵亮[1] 马德成[1] 

机构地区：[1]中南大学地学与环境工程学院,湖南长沙410083

出　　处：《矿产与地质》2010年第1期55-58,共4页Mineral Resources and Geology

摘　　要：介绍了野鸡尾南铅锌矿床地质特征,分析了控矿因素,总结了成矿规律,认为成矿物质来自岩浆热液,中上泥盆统碳酸盐岩是主要的赋矿地层,近南北向层间滑动构造及由东西向裂隙发育而成的古岩溶是重要的容矿构造,矿体沿构造带断续分布,不同方向构造交汇部位可形成富矿柱。In the paper, the authors made an introduction to the geological characteristics of South Yejiwei Pb-Zn ore deposit, analyzed the ore-controlling factors and summarized the mineralization regularities. They consider that the ore-forming materials came from the magmatic hydrothermal solution, carbonates stratum of middle-upper Devonian is the main ore-bearing stratum, the paleokarst caused by interface sliding structure in SN strike direction and fissures in EW strike direction are essential ore-hosting structures, ore body distributed intermittently along the tectonic zone, and rich jambs can be formed in the intersection of different direction construction.

关 键 词：野鸡尾南 岩浆热液 控矿因素 成矿规律 

分 类 号：P618.42[天文地球—矿床学] P618.43[天文地球—地质学]