| 云南腾冲棋盘石铅锌多金属矿矿床地质特征及找矿方向 |
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| 引用本文： | 吴道鹏,雷阳艾,杨飞,普米仓,王文超.云南腾冲棋盘石铅锌多金属矿矿床地质特征及找矿方向[J].化工矿产地质,2013(4):234-241. |
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| 作者姓名： | 吴道鹏 雷阳艾 杨飞 普米仓 王文超 |
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| 作者单位： | 云南省有色地质局三一o队,云南大理671000 |
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| 摘 要： | 棋盘石铅锌多金属矿属于矽卡岩型多金属矿。通过对该矿床地质特征的分析后认为,矿体严格受岩体、碳酸盐岩及构造的控制,矿石类型为矽卡岩型硫化铅锌矿石;围岩蚀变以黄铁矿化、矽卡岩化、绿泥石化、碳酸盐化为特征;岩体与碳酸盐岩接触带为该矿床的重要的找矿方向。
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| 关 键 词： | 铅锌多金属矿 地质特征 找矿地质前提 找矿标志 腾冲县 棋盘石 |
GEOLOGICAL CHARACTERISTICS AND PROSPECTING CRITERIA OF QIPANISHI LEAD-ZINC POLYMETALLIC ORE DEPOSIT IN YUNNAN |
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| Wu Daopeng Lei Yangai Yang Fei Pu Micang Wang Wenchao.GEOLOGICAL CHARACTERISTICS AND PROSPECTING CRITERIA OF QIPANISHI LEAD-ZINC POLYMETALLIC ORE DEPOSIT IN YUNNAN[J].Geology of Chemical Minerals,2013(4):234-241. |
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| Authors: | Wu Daopeng Lei Yangai Yang Fei Pu Micang Wang Wenchao |
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| Institution: | Wu Daopeng Lei Yangai Yang Fei Pu Micang Wang Wenchao Yunnan Nonferrous Geological Bureau team 310, Yunnan Dali, 671000, China |
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| Abstract: | The Qipanshi lead-zinc polymetallic deposit belongs to skarn type polymetallic deposit. lhrougla the analysis on the geological characteristics of the deposit, there are 3 conclusions can be reached： 1） orebody is strictly controlled by the rock, carbonate rock and structure,ore types for the skarn Pb Zn sulphide ore; 2）wall rock alterationpyritization, skarn, chloritization, carbonatation; 3）rock andcarbonate rock in contact with the deposit the important ore prospecting marks. |
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| Keywords: | lead-zinc polymetallic deposit geological characteristics geological preconditions for prospecting prospecting cariteria Tengchongcounty Qipanshi |
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