| 湖南桃林与剥离断层有关的铅锌及萤石矿化作用 |
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| 引用本文： | 李先福.湖南桃林与剥离断层有关的铅锌及萤石矿化作用[J].现代地质,1992,6(1):46-54. |
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| 作者姓名： | 李先福 |
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| 作者单位： | 武汉化工学院 |
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| 摘 要： | 研究表明,湖南桃林铅—锌—萤石矿床是一个与第三纪剥离断层有关的热液充填型“(断)层状矿床”。从金属矿质的来源,到矿体规模和空间分布,以及成矿的物化条件等明显受剥离断层构造的控制。
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| 关 键 词： | 剥离断层 碎裂糜棱岩 铅锌萤石矿化 湖南桃林 |
LEAD - ZINC - FLUORITE MINERALIZATION ASSOCIATED WITH DENUDATIONAL FAULTS IN TAOLIN ORE AREA, HUNAN |
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| Li Xianfu.LEAD - ZINC - FLUORITE MINERALIZATION ASSOCIATED WITH DENUDATIONAL FAULTS IN TAOLIN ORE AREA, HUNAN[J].Geoscience——Journal of Graduate School,China University of Geosciences,1992,6(1):46-54. |
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| Authors: | Li Xianfu |
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| Institution: | Wuhan Institute of Chemical Technology |
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| Abstract: | Based on the latest structural study of Hunan Taolin ore, we have proved that the Lead-Zinc-fluorite deposit is a "layered deposit" associated with Eogene denudational faults. While the source of useful metals, the scale and distribution of the orebody, the mineral association and zoning, the mineralization sequence, the ore structural and physico-chemical conditions, etc. , all of these have been demonstrated to be controled by the characteristics of the denudational faults in the background of the extentional structure. |
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| Keywords: | : denudational faults cataclastic mylonite had - Zinc- fluorite mineralization Taolin Hunan Province |
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