| 云南巍山县火山村铅锌矿成因浅析 |
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| 引用本文： | 赵贤,邹绍丹,赵庆红,董绍华.云南巍山县火山村铅锌矿成因浅析[J].云南地质,2014,33(3):357-361. |
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| 作者姓名： | 赵贤 邹绍丹 赵庆红 董绍华 |
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| 作者单位： | 云南省地质矿产勘查院大理地质矿产所,云南大理,671000 |
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| 摘 要： | 火山村铅锌矿属中低温热液铅锌矿床,矿体产于构造裂隙带中,围岩蚀变有碳酸盐化、硅化、褐铁矿化、萤石化、泥化.其中尤以硅化、碳酸盐化、褐铁矿化、萤石化与矿化关系密切.
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| 关 键 词： | 中低温热液矿床 构造裂隙控矿 云南巍山火山村 |
A PRELIMINARY ANALYSIS OF HUOSHANCUN PB-ZN DEPOSIT IN WEISHAN,YUNNAN |
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| ZHAO Xian,ZOU Shao-dan,ZHAO Qing-hong,DONG Shao-hua.A PRELIMINARY ANALYSIS OF HUOSHANCUN PB-ZN DEPOSIT IN WEISHAN,YUNNAN[J].Yunnan Geology,2014,33(3):357-361. |
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| Authors: | ZHAO Xian ZOU Shao-dan ZHAO Qing-hong DONG Shao-hua |
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| Institution: | ( Dali Branch, Yunnan Exploration Institute of Geology ＆ Mineral Resources, Dali 671000) |
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| Abstract: | Huoshancun Pb-Zn deposit is a middle-low T hydrothermal Pb-Zn deposit, with ore body in the structure fissure zone, wall rock alteration carbonatization, silicification, limonitization, fluoritization, argillitiza- tion. The metallogenesis is in close relation with the silicification, carbonatization, limonitization, fluoritization. |
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| Keywords: | Middle-Low T Hydrothermal Deposit Ore Control of Structure Fissure Huoshancun Village Weishan Yunnan |
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