| 云南剑川象图铅锌多金属矿成矿地质条件 |
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| 引用本文： | 杨勇,刘杰,杨洪,胡成军.云南剑川象图铅锌多金属矿成矿地质条件[J].云南地质,2012(3):340-342. |
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| 作者姓名： | 杨勇 刘杰 杨洪 胡成军 |
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| 作者单位： | 云南省地质矿产勘查院大理地质矿产所 |
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| 摘 要： | 象图铅锌多金属矿矿化带位于三合洞组(T3s)灰岩中以及顶部灰岩与挖鲁把组(T3wl)薄层状泥岩接触部位层间破碎带中,三个铁、铅、锌矿化体,属沉积改造形成的构造破碎带型铅、锌(铁)矿床。
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| 关 键 词： | 沉积改造型 构造破碎带 层间破碎带 上三叠统三合洞组 云南剑川象图 |
THE GEOLOGICAL CONDITION OF METALLOGENESIS OF XIANGTU PB-ZN MULTIMETALLIC DEPOSIT IN JIANCHUAN,YUNNAN |
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| YANG Yong,LIU Jie,YANG Hong,HU Cheng-jun.THE GEOLOGICAL CONDITION OF METALLOGENESIS OF XIANGTU PB-ZN MULTIMETALLIC DEPOSIT IN JIANCHUAN,YUNNAN[J].Yunnan Geology,2012(3):340-342. |
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| Authors: | YANG Yong LIU Jie YANG Hong HU Cheng-jun |
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| Institution: | (Dali Institute of Geology & Mineral Resources,Yunnan Exploration Institute of Geology & Mineral Resources,Dali 671000) |
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| Abstract: | The metallogenetic zone of Xiangtu Pb-Zn multimetallic deposit is in the Sanhedong Formation(T3s)limestone and the interlayer fracture zone of the contact between the top limestone and Waluba Formation(T3wl)lamellted mudstone.The 3 Fe,Pb,Zn metallogenetic bodies belong to the Pb,Zn(Fe)deposit of structure fracture zone type,formed by sedimentation and reformation. |
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| Keywords: | Sedimentation-Reformation Type Structure Fracture Zone Interlayer Fracture Zone Upper Triassic Sanhedong Formation Xiangtu Jianchuan Yunnan |
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