| 沿河县丰水岭萤石矿床地质特征、成矿模式及找矿标志 |
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| 引用本文： | 刘健,叶飞.沿河县丰水岭萤石矿床地质特征、成矿模式及找矿标志[J].企业技术开发,2013(16):89-91. |
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| 作者姓名： | 刘健 叶飞 |
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| 作者单位： | 贵州省地质矿产勘查开发局103地质大队 |
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| 摘 要： | 沿河县丰水岭萤石矿是产于奥陶系湄潭组、红花园组地层中的低温热液型萤石矿,通过对地质特征和成矿模式的分析,认为找矿的主要标志为地层岩性和断裂构造。富集成矿的主要部位为奥陶系湄潭组、红花园组与北西向断裂交汇部位。
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| 关 键 词： | 萤石矿 地质特征 成矿模式 |
Geological features,metallogenic model and prospecting criteria of fluorite mine in Fengshuiling of Yanhe County |
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| LIU Jian,YE Fei.Geological features,metallogenic model and prospecting criteria of fluorite mine in Fengshuiling of Yanhe County[J].Technological Development of Enterprise,2013(16):89-91. |
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| Authors: | LIU Jian YE Fei |
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| Institution: | 103 geological Team of Guizhou Geological and Mineral Exploration and Development Bureau,Tongren,Guizhou 554300,China) |
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| Abstract: | Fengshuiling fluorite mine in Yanhe blongs to epithermal fluorite deposite,which originate in Meitan and Honghuayuan group of the Ordovician.By analyzing the geological characteristics and metallogenic model,the main sign of prospecting is identified as formation lithology and falt structure.The main parts of enrichment of ore are the intersection of Meitan and Honghuayuan group of Ordovician and NW faults. |
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| Keywords: | fluorite mine geological characteristics metallogenic model |
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