| 云南德钦鲁春铜铅锌多金属矿同位素及矿床成因 |
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| 引用本文： | 赵灿华,范玉华,孟青.云南德钦鲁春铜铅锌多金属矿同位素及矿床成因[J].云南地质,2011,30(1):32-37. |
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| 作者姓名： | 赵灿华 范玉华 孟青 |
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| 作者单位： | 云南省地质调查院,昆明,650216 |
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| 摘 要： | 矿体产于中三叠统上兰组上段第一层层间裂隙和破碎带.上兰组与其上的攀天阁组属"双峰式"火山岩.地层层位、热液运移和矿质沉淀的构造空间控制了本矿床的产出.属典型的中-高温热液型铜铅锌多金属矿床.
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| 关 键 词： | 中-高温热液型 铜铅锌多金属矿 上兰组上段赋矿 "双峰式"火山岩 云南 德钦鲁春 |
THE ISOTOPE AND GENESIS OF LUCHUN CU-PB-ZN MULTIMETALLIC DEPOSIT IN DEQIN,YUNNAN |
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| ZHAO Can-hua,FAN Yu-hua,MENG Qing.THE ISOTOPE AND GENESIS OF LUCHUN CU-PB-ZN MULTIMETALLIC DEPOSIT IN DEQIN,YUNNAN[J].Yunnan Geology,2011,30(1):32-37. |
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| Authors: | ZHAO Can-hua FAN Yu-hua MENG Qing |
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| Institution: | ZHAO Can-hua,FAN Yu-hua,MENG Qing(Yunnan Institute of Geological Survey,Kunming 650216) |
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| Abstract: | The ore body is in the inter-bed fissure and fracture zone of Middle Triassic Shanglan Formation Upper Member 1st bed.The Shanglan Formation and the superincumbent Pantiange Formation belong to the 2-peak volcanic rock.The stratigraphic horizon,hydrothermal migration and ore precipitation structure space control the formation of this ore deposit,which is a typical mid-high T hydrothermal Cu-Pb-Zn multimetallic deposit. |
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| Keywords: | High T Hydrothermal Type Cu-Pb-Zn Multimetallic Deposit Ore-Bearing Shanglan Formation Upper Member 2-Peak Volcanic Rock Luchun Deqin Yunnan |
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