| 福建省梅仙铅锌银矿田成矿地质特征和成因模式 |
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| 引用本文： | 吴志强. 福建省梅仙铅锌银矿田成矿地质特征和成因模式[J]. 矿产与地质, 2003, 17(5): 606-609 |
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| 作者姓名： | 吴志强 |
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| 作者单位： | 江苏省有色金属华东地质勘查局,江苏,南京,210007 |
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| 摘 要： | 梅仙铅锌银矿田形成于裂谷成矿环境，具有块状硫化物矿床特征，成矿物质和成矿热液有多来源特征，成矿经历了同生沉积、变质改造和岩浆热液叠加三个阶段，并与闽中裂谷带的构造演化密切相关，提出了“三阶段”成因模式。
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| 关 键 词： | 铅锌银矿床 成因模式 地质特征 福建省梅山 |
| 文章编号： | 1001-5663(2003)05-0606-04 |
| 修稿时间： | 2003-04-07 |
THE GEOLOGICAL CHARACTERISTICS AND GENETIC MODEL OF MEIXIAN LEAD-ZINC-SILVER ORE FIELD IN FUJIAN PROVINCE |
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| WU Zhi-qiang. THE GEOLOGICAL CHARACTERISTICS AND GENETIC MODEL OF MEIXIAN LEAD-ZINC-SILVER ORE FIELD IN FUJIAN PROVINCE[J]. Mineral Resources and Geology, 2003, 17(5): 606-609 |
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| Authors: | WU Zhi-qiang |
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| Abstract: | Meixian Pb-Zn-Ag ore field were formed in the central Fujian rift zone, with the distinct characteristics of massive sulfide deposits. Both ore-forming materials and fluids were originated from multiple sources, and the mineral deposits were resulted from superimposition and transformation of multiple geological events. Consequently, a three-epoch genetic model, related to tectonic evolution of the rift, was proposed for Meixian Pb-Zn-Ag ore field. |
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| Keywords: | gehetic model geological characteristics Meixian Pb-Zn-Ag ore field Fujian province |
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