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| 云南永胜宝坪浅源热液改造型铜矿地质及成因 | |
| 引用本文： | 谭玉荣,秦培林,王学武,高建国.云南永胜宝坪浅源热液改造型铜矿地质及成因[J].云南地质,2008,27(3):357-361. |
| 作者姓名： | 谭玉荣 秦培林 王学武 高建国 |
| 作者单位： | 1. 云南省核工业二○九地质大队,昆明,650032;昆明理工大国土资源学院,昆明,650093 2. 云南省核工业二○九地质大队,昆明,650032 3. 昆明理工大国土资源学院,昆明,650093 |
| 基金项目： | 致谢：论文写作得到昆明理工大国土资源学院高建国博导和云南省核工业二○九地质大队高级工程师王学武两位老师的指导和帮助,在此表示感谢! |
| 摘 要： | 宝坪铜矿赋存于三叠系下统腊美组中。矿体呈似层状，少量脉状，严格受北北西-北西向构造控制。矿床成因类型属浅源热液改造型铜矿床。 |
| 关 键 词： | 构造控矿 热液改造 铜矿床 永胜 宝坪 云南 |
THE GEOLOGY AND GENESIS OF BAOPING CU DEPOSIT OF SHALLOW HYDROTHERMAL REFORMATION TYPE IN YONGSHENG, YUNNAN |
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| TAN Yu-rong,QIN Pei-lin,WANG Xue-wu,GAO Jian-guo.THE GEOLOGY AND GENESIS OF BAOPING CU DEPOSIT OF SHALLOW HYDROTHERMAL REFORMATION TYPE IN YONGSHENG, YUNNAN[J].Yunnan Geology,2008,27(3):357-361. | |
| Authors: | TAN Yu-rong QIN Pei-lin WANG Xue-wu GAO Jian-guo |
| Institution: | TAN Yu - rong, QIN Pei - lin, WANG Xue - wu, GAO Jian - guo ( 1. Geological Team 209 of Yunnan Nuclear Industry, Kunming 650032;2. College of Land Resources, Kunming University of Science ＆ Technology, Kunming 650093 ) |
| Abstract: | The Baoping Cu deposit of Yongsheng occurs in Lower Triassic Lamei Formation. The ore bodies are stratoid, whereas a little is veined, which are controlled strictly by NNW-NW structures. This ore deposit belongs to the shallow hydrothermal reformation Cu deposit in genesis type. |
| Keywords: | Ore Control of Structure Hydrothermal Reformation Cu Deposit Baoping Yongsheng Yunnan |
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