| 马关八梅喷流沉积铅锌锡铜金多金属矿床 |
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| 引用本文： | 杨翰魁.马关八梅喷流沉积铅锌锡铜金多金属矿床[J].云南地质,2008,27(2):175-180. |
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| 作者姓名： | 杨翰魁 |
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| 作者单位： | 云南省有色地质317队,曲靖,655000 |
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| 摘 要： | 矿床产于中寒武田蓬组地层中，受地层、沉积岩相、变质岩相控制。围岩蚀变为黄铁矿化、锰矿化、碳酸盐化、硅化。矿床成因为海底含矿热卤水喷流沉积型。
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| 关 键 词： | 热卤水喷流沉积 多金属矿床 中寒武统地层 八梅马关云南 |
THE EFFUSIVE SEDIMENTARY PB ZN SN CU MULTIMETALLIC DEPOSIT OF BAMEI, MAGUAN |
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| YANG Han-kui.THE EFFUSIVE SEDIMENTARY PB ZN SN CU MULTIMETALLIC DEPOSIT OF BAMEI, MAGUAN[J].Yunnan Geology,2008,27(2):175-180. |
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| Authors: | YANG Han-kui |
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| Institution: | YANG Han-kui (Nonferrous Geological Team 317 of Yunnan, Qujing 655000) |
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| Abstract: | The ore body exists in Middle Cambrian Tianpeng Formation, which is controlled by strata, sedimentary and metamorphic rock facies. The alterations of wall rock are pyritization, Mn mineralization, carbonatization and silicification. The genesis of this ore deposit belongs to the effusive sedimentary type of submarine ore - bearing thermal brine. |
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| Keywords: | Effusive Sediemnt of Thermal Brine Muhimetallic Ore Deposit Middle Cambrian Strata Bamei Maguan Yunnan |
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