| 云南维西娃渣铁铅锌多金属矿床 |
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| 引用本文： | 黄跃,王炳华,罗光明,胡清华.云南维西娃渣铁铅锌多金属矿床[J].云南地质,2013(4):429-432,442. |
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| 作者姓名： | 黄跃 王炳华 罗光明 胡清华 |
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| 作者单位： | 云南省地质调查院矿产所,云南昆明650216 |
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| 摘 要： | 矿床属与中三叠统中酸性火山岩有关的喷流型（或火山沉积改造型）铁铅锌多金属矿,并受地层构造双重控制.
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| 关 键 词： | 铁铅锌多金属 双重控制地层 热液喷流型 云南维西娃渣 |
THE GEOLOGICAL FEATURE OF WAZHA FE-PB-ZN MULTIMETALLIC DEPOSIT IN WEIXI,YUNNAN |
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| HUANG Yue,WANG Bing-hua,LUO Guang-ming,HU Qing-hua.THE GEOLOGICAL FEATURE OF WAZHA FE-PB-ZN MULTIMETALLIC DEPOSIT IN WEIXI,YUNNAN[J].Yunnan Geology,2013(4):429-432,442. |
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| Authors: | HUANG Yue WANG Bing-hua LUO Guang-ming HU Qing-hua |
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| Institution: | (Branch of Mineral Resources, Yunnan Institute of Geological Survey, Kunming 650216) |
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| Abstract: | The Fe deposit belongs to the effusion type （or volcanic deposition reformation type） related with Middle Triassic intermediate- acid volcanic rock in genesis. The Pb-Zn multimetallic deposit is related to Shanglan Formation slate, silty slate with intercalation of limestone, marl and Sanhedong Formation limestone in genesis, which is a Cu -Pb -Zn multimetallic deposit of hydrothermal type controlled by both strata and structure. |
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| Keywords: | Fe - Pb - Zn Multimetallic Dual Control Hydrothermal Effusion Type Wazha Weixi Yunnan |
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