| 兰坪县青甸湾铅锌矿矿床地质 |
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| 引用本文： | 陈梁,孙德瑜,王列,杨枝斌.兰坪县青甸湾铅锌矿矿床地质[J].云南地质,2009,28(3):280-284. |
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| 作者姓名： | 陈梁 孙德瑜 王列 杨枝斌 |
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| 作者单位： | 云南省有色地质局三一○队,大理,凤仪,671005 |
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| 摘 要： | 铅锌矿位于兰坪盆地铅锌银铜多金属矿集区，上三叠统灰岩为主要赋矿地层，铅质源自海底火山喷发，属火山-沉积改造型中低温热液矿床。
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| 关 键 词： | 中低温铅锌矿 沉积改造 上三叠统层控 灰岩破碎带 云南兰坪青甸湾 |
THE GEOLOGY OF QINGDIANWAN PB-ZN DEPOSIT IN LANPING |
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| CHEN Liang,SUN De-yu,WANG Lie,YANG Zhi-bin.THE GEOLOGY OF QINGDIANWAN PB-ZN DEPOSIT IN LANPING[J].Yunnan Geology,2009,28(3):280-284. |
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| Authors: | CHEN Liang SUN De-yu WANG Lie YANG Zhi-bin |
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| Institution: | ( Nonferrous Geological Team 310 of Yunnan, Dali 671005 ) |
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| Abstract: | This ore deposit is in the concentration area of Pb - Zn - Ag - Cu muhimetallic deposits in Lanping basin. The main ore - bearing bed is Upper Triassic limestone. The Pb is originated from the submarine volcanic eruption, which belongs to the volcanic - sedimentary reformation middle -low T hydrothermal deposit. |
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| Keywords: | Middle - Low T Pb - Zn Deposit Sedimentary Reformation Upper Triassic Stratabound Limestone Fracture Qingdianwan Lanping Yunnan |
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