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 Metallogeny of Southern Yejiwei Lead-zinc Deposit,Shizhuyuan,Chenzhou City

作　　者：赵亮[1] 黄满湘[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：《资源环境与工程》2010年第3期242-245,共4页Resources Environment & Engineering

摘　　要：介绍野鸡尾南铅锌矿床地质特征,分析控矿因素,总结成矿规律,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。This paper introduces geological characteristics of the Southern Yejiwei lead-zinc deposits,analyzes ore-controlling factors,and summarized the metallogeny.It is considered that the ore-forming material is coming from the magmatic hydrothermal fluid.Middle-upper Devonian carbonate rocks are the main ore-bearing stratum.The paleokarst is the important host structure which caused by interlayer-gliding structure of S-N strike and fissures of E-W strike.Ore body is distributed intermittently along the tectonic zone.Ore shoot can be formed in the different directions of structural convergence.

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] P618.45[天文地球—地质学]