| 云南普洱市芒达铜铅银矿地质特征及成因 |
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| 引用本文： | 张颖瑞,洪瑞岐,刘文力,张军伟.云南普洱市芒达铜铅银矿地质特征及成因[J].云南地质,2021(1):37-41. |
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| 作者姓名： | 张颖瑞 洪瑞岐 刘文力 张军伟 |
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| 作者单位： | 云南省地质矿产勘查院 |
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| 摘 要： | 云南普洱市芒达铜铅银矿位于思茅大平掌铜矿西侧,其矿体呈似层状赋存于层间断层构造破碎带中,构造控矿明显,矿体围岩为侏罗系下统芒汇河组三段(J1mh3)沉火山碎屑岩,矿床成因类型属断层构造控制的中低温热液型铜多金属矿床.
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| 关 键 词： | 构造控矿 热液型矿床 云南普洱 芒达 |
THE GEOLOGICAL FEATURE AND GENESIS OF MANGDA CU-PB-AG DEPOSIT IN PUER,YUNNAN |
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| ZHANG Ying-rui,HONGRui-qi,LIU Wen-li,ZHANG Jun-wei.THE GEOLOGICAL FEATURE AND GENESIS OF MANGDA CU-PB-AG DEPOSIT IN PUER,YUNNAN[J].Yunnan Geology,2021(1):37-41. |
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| Authors: | ZHANG Ying-rui HONGRui-qi LIU Wen-li ZHANG Jun-wei |
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| Institution: | (Yunnan Exploration Institute of Geology and Mineral Resources,Kunming 650051) |
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| Abstract: | Mangda Cu-Pb-Ag deposit in Puer,Yunnan is on the W side of Dapingzhang Cu deposit of Simao.The orebody is stratoid in the interlayer fault fracture zone,ore control of structure clear.The wall rock of orebody is Lower J Manghuihe Formation Member 3(J1mh3)sedimentary pyroclastics.It is a middle-low T hydrothermal Cu multimetallic deposit controlled by fault structure in genesis. |
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| Keywords: | Ore Control of Structure Hydrothermal Deposit Mangda Puer Yunnan |
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