| 云南兰坪县利五巴铜矿床地质特征 |
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| 引用本文： | 黄平,黄波,徐伟钧,聂爱国.云南兰坪县利五巴铜矿床地质特征[J].四川地质学报,2012(4):412-416. |
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| 作者姓名： | 黄平 黄波 徐伟钧 聂爱国 |
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| 作者单位： | [1]贵州大学资源与环境学院,贵阳550003 [2]贵阳市国土资源局,贵阳550004 [3]贵州省有色地质勘查局物化探总队,贵州都匀558000 [4]桂林理工大学地球科学学院,桂林541004 |
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| 摘 要： | 利五巴铜矿位于三江成矿带反"S"型大地构造中段金沙江构造带与兰坪盆地结合部位,位于古—中元古界雪龙山变质岩第二组和第三组的石榴二云石英片岩、黑云石英片岩、碱长片麻岩破碎带中。通过对矿区地层、构造及矿床地质特征分析,结合前人三江地区研究成果及成矿理论认为,该铜矿床为热水喷流沉积型铜矿床,成矿地质条件有利,具良好的找矿前景。
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| 关 键 词： | 利五巴铜矿 地质特征 云南兰坪县 |
Geological Features of the Liwuba Cu Deposit in Lanping, Yunnan |
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| HUANG Ping,HUANG Bo,XU Wei-jun,NIE Ai-guo.Geological Features of the Liwuba Cu Deposit in Lanping, Yunnan[J].Acta Geologica Sichuan,2012(4):412-416. |
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| Authors: | HUANG Ping HUANG Bo XU Wei-jun NIE Ai-guo |
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| Institution: | 1-College of Resources and Environment, Guizhou University, Guiyang 550003; 2-Guiyang Bureau of Land and Resources, Guiyang 550004; 3-Geophysical and Geochemical Exploration Party, Guizhou Nonferrous Metals Geological Exploration Bureau, Duyun, Guizhou 558000; 4-College of Earth Sciences, Guilin University of Technology, Guilin, Guangxi, 541004) |
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| Abstract: | The Liwuba Cu deposit lies in the junction of the Jinshajiang tectonic zone and the Lanping basin and is confined to fracture zone of garnet two-mica quartz schist, biotite quartz schist and alkali-feldspar gneiss of the Paleo-Middle Proterozoic Xuelongshan metamorphic rock. This paper deals with its exhalation-sedimentary genesis based on stratigraphy, structure and geological features. |
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| Keywords: | Liwuba copper deposit geologic feature Lanping Yunnan |
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