| 江西潭坑铅锌(银)矿床特征及成因分析 |
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| 引用本文： | 徐顺国.江西潭坑铅锌(银)矿床特征及成因分析[J].资源调查与环境,2011,32(1):29-36. |
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| 作者姓名： | 徐顺国 |
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| 作者单位： | 江西省地质调查研究院,南昌,330030 |
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| 基金项目： | 江西永平地区矿产远景调查项目 |
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| 摘 要： | 江西省潭坑铅锌(银)矿区位于北武夷铅锌银成矿带内,本文系统阐述了矿区地质和矿床特征,并对矿床的成因进行了探讨。认为本区铅锌(银)矿床,经历了火山喷发沉积和后期热液充填两大成矿期,与次火山岩体(流纹斑岩)有密切的关系,属次火山热液矿床。
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| 关 键 词： | 铅锌(银) 矿床特征 成因类型 喷发沉积 热液充填 次火山热液矿床 江西 |
Characteristics of Tankeng lead-zinc (silver) deposit in Jiangxi province and its genesis analysis |
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| XU Shun-guo.Characteristics of Tankeng lead-zinc (silver) deposit in Jiangxi province and its genesis analysis[J].Resources Survey & Environment,2011,32(1):29-36. |
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| Authors: | XU Shun-guo |
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| Institution: | XU Shun-guo (Jiangxi Provincial Institute of geological Survey,Nanchang 330030,China) |
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| Abstract: | Tankeng lead-zinc(silver) deposit in Jiangxi province is located in the Northern WuyiMountain lead-zinc-silver metallogenic belt. This paper systematically describes geologicalsituation of mineralized area and characteristics of the deposit in order to discuss the gene-sis of the deposit. It is regarded that the deposit experienced two mineralization periods:volcanic-eruptive sedimentation and late hydrothermal filling. In addition, the deposit hasa close relationship with sub-volcanic rocks (rhyolite-porph... |
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| Keywords: | lead-zinc (silver) deposit characteristics of deposit genetic types erup-tive sedimentation hydrothermal filling sub-volcanic hydrothermal deposit Jiangxi |
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