| 云南省临沧邦东忙牙铜矿成矿信息分析 |
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| 引用本文： | 王刚,龙庆兵,李俊,高建国.云南省临沧邦东忙牙铜矿成矿信息分析[J].云南地质,2011,30(3):344-347. |
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| 作者姓名： | 王刚 龙庆兵 李俊 高建国 |
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| 作者单位： | 1. 云南省核工业二0九地质大队,昆明,650032
2. 昆明理工大国土资源学院,昆明,650093 |
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| 摘 要： | 忙牙区1∶1万土壤化探测量发现三个铜异常晕圈,三条矿化带,均赋存于火山岩与二叠系浅变质接触带内及其附近,矿床成因属中—低温热液型,且受构造控制。
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| 关 键 词： | 中低温热液型 铜矿床 接触变质带 构造控矿 云南临沧邦东 |
AN ANALYSIS OF THE METALLOGENESIS INFORMATION OF MANGYA CU DEPOSIT OF BANGDONG IN LINCANG, YUNNAN |
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| WANG Gang,LONG Qing-bing,LI Jun,GAO Jian-guo.AN ANALYSIS OF THE METALLOGENESIS INFORMATION OF MANGYA CU DEPOSIT OF BANGDONG IN LINCANG, YUNNAN[J].Yunnan Geology,2011,30(3):344-347. |
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| Authors: | WANG Gang LONG Qing-bing LI Jun GAO Jian-guo |
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| Institution: | WANG Gang1,LONG Qing-bing1,LI Jun2,GAO Jian-guo2(1.Geological Team 209,Yunnan Nuclear Industry,Kunming 650032)(2.College of Land Resources,Kunming University of Science & Technology,Kunming650093) |
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| Abstract: | According to the 1：10000 soil geochemical survey in Mangya area, we find out that 3 Cu anoma- lies and 3 metallogenetic zones are in or near the contact between volcanic rock and P epi - metamorphic rock. The genesis of ore deposit belongs to the mid - low T hydrothermal type, which is controlled by the structure. |
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| Keywords: | Mid - Low T Hydrotherrnal Type Cu Deposit Contact Metamorphic Type Ore Control ofStructure Bangdong Lincang Yunnan |
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