| 云南永平上别咧铜多金属矿成因 |
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| 引用本文： | 杨利翔,段红达,吴道鹏.云南永平上别咧铜多金属矿成因[J].云南地质,2008,27(2):203-209. |
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| 作者姓名： | 杨利翔 段红达 吴道鹏 |
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| 作者单位： | 云南省有色地质三一○队,大理,671000 |
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| 摘 要： | 上别列铜多金属矿床属水泄咱咧铜钴矿区外围新发现的矿点，赋存于兰坪-思茅盆地中生带红色碎屑岩建造厂街-水泄成矿带中，区内有30余处矿点，中-小型铜、铁矿点二处。认为属改造型中低温热卤水裂隙充填矿床，水泄咱咧铜钴矿区外围具备进一步找矿的条件。
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| 关 键 词： | 铜多金属 中低温热卤水 裂隙充填矿床 后期改造 水泄上别咧云南 |
THE GENESIS OF SHANGBIELIE CU MULTIMETALLIC DEPOSIT OF YONGPING, YUNNAN |
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| YANG Li-xiang,DUAN Hong-da,WU DAO-peng.THE GENESIS OF SHANGBIELIE CU MULTIMETALLIC DEPOSIT OF YONGPING, YUNNAN[J].Yunnan Geology,2008,27(2):203-209. |
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| Authors: | YANG Li-xiang DUAN Hong-da WU DAO-peng |
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| Institution: | (Nonferrous Geological Team 310 of Yunnan, Dali 671000) |
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| Abstract: | The Shangbielie Cu muhimetallic deposit is a new ore occurrence discovered outside the Shuixie- Zanlie Cu- Co orefield, which exists in Changjie- Shuixie metallogenetic Zone of Mesozoic red clastic rock formation in Lanping - Simao basin. We believe that this ore deposit belongs to the middle - low T thermal brine fissure filling ore deposit of reformation type. The area a- round Shuixie - Zanlie Cu - Co orefield has the condition of further ore - prospecting. |
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| Keywords: | Cu Multimetallic Deposit Middle -Low T Thermal Brine Fissure Filling De- posit Reformation Type Shangbielie Shuixie Yunnan |
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