| 普洱大箐铜矿地质及成因 |
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| 引用本文： | 张荣伟.普洱大箐铜矿地质及成因[J].云南地质,2008,27(3):351-356. |
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| 作者姓名： | 张荣伟 |
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| 作者单位： | 云南省有色地质地球物理化学勘查院,昆明,650216 |
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| 基金项目： | 本文在编写过程中得到荣蕙锋高工、莫向云高工的大力支持和帮助,在此深表感谢! |
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| 摘 要： | 矿体产于断层破碎带中，受断层和地层层位控制。根据矿床地质特征研究，发现大箐铜矿与兰坪金满铜矿具有一定相似性，认为大箐铜矿应属中低温热液型构造铜矿床。
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| 关 键 词： | “大脉型”铜矿 破碎带控矿 热卤水 普洱 大箐 云南 |
THE GEOLOGY AND GENESIS OF DAQING CU DEPOSIT IN PUER |
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| ZHANG Rong-wei.THE GEOLOGY AND GENESIS OF DAQING CU DEPOSIT IN PUER[J].Yunnan Geology,2008,27(3):351-356. |
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| Authors: | ZHANG Rong-wei |
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| Institution: | ZHANG Rong-wei (Yunnan Nonferrous Geoexploration Institute, Kunming 650216) |
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| Abstract: | The ore bodies occur in the fault fracture zone, which are controlled by the fault and stratigraphic horizon. According to the study of geological characteristics of ore deposit, etc, the Daqing Cu deposit is somewhat similar to the Jinman Cu deposit in Lanping. We think that the Daqing Cu deposit must belong to middle -low T hydrothermal structural Cu deposit. |
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| Keywords: | ＂Large Vein＂ Cu Deposit Ore Control of Fracture Zone Thermal Brine Daqing Yunnan |
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