| 云南澜沦南现铜铅锌多金属矿成矿地质条件 |
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| 引用本文： | 王炳华,黄跃,邢程,毕晓路.云南澜沦南现铜铅锌多金属矿成矿地质条件[J].云南地质,2013(4):433-435. |
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| 作者姓名： | 王炳华 黄跃 邢程 毕晓路 |
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| 作者单位： | 云南省地质调查院,云南昆明650216 |
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| 摘 要： | 铜铅锌矿赋存于中侏罗统花开左组浅色岩系和杂色岩系破碎带中,为受层位控制的砂页岩型铜矿及受构造控制的热液型铅锌多金属矿床.
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| 关 键 词： | 砂页岩型铜矿 地层构造控矿 沉积型和热液型 云南澜沧南现 |
THE GEOLOGICAL CONDITIONS OF NANXIAN CU-PB-ZN MULTIMETALLIC METALLOGENESIS IN LANCANG,YUNNAN |
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| WANG Bing-hua,HUANG Yue,Xing Cheng,BI Xiao-lu.THE GEOLOGICAL CONDITIONS OF NANXIAN CU-PB-ZN MULTIMETALLIC METALLOGENESIS IN LANCANG,YUNNAN[J].Yunnan Geology,2013(4):433-435. |
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| Authors: | WANG Bing-hua HUANG Yue Xing Cheng BI Xiao-lu |
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| Affiliation: | ( Yunnan Institute of Geological Survey, Kunming 650216 ) |
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| Abstract: | The Cu - Pb deposit is in the fracture zone of Middle Jurassic Huakaizuo Formation light color rock series and motley rock series, which is the Cu deposit of sandstone - shale type controlled by the horizone and the Pb - Zn multimetallic deposit of hydrothermal type controlled by the structure. |
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| Keywords: | Cu Deposit Sandstone -Shale Type Ore Control of Strata -Structure Sedimentation Type and Hydrothermal Type Nanxian Lancang Yunnan |
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