| 中条山胡—蓖型铜矿床成因新认识 |
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| 引用本文： | 李先福,岑博雄.中条山胡—蓖型铜矿床成因新认识[J].武汉化工学院学报,1993(3). |
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| 作者姓名： | 李先福 岑博雄 |
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| 作者单位： | 武汉化工学院,中国地质大学 武汉 |
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| 基金项目： | 本文得到75-55-03-08攻关项目资助。 |
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| 摘 要： | 讨论了剥离断层与成矿物质来源,矿体空间分布型式以及矿化特征等方面联系,从而提出胡-蓖型铜矿床是一个受剥离断层控制的“热液型(断)层状矿床”。
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| 关 键 词： | 矿床成因 剥离断层控矿 胡-蓖型 |
New Understanding of HU-BI Copper Deposits Origins in Shanxi Zhongtiao Mountains |
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| Li Xianfu Cen Boxiong.New Understanding of HU-BI Copper Deposits Origins in Shanxi Zhongtiao Mountains[J].Journal of Wuhan Institute of Chemical Technology,1993(3). |
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| Authors: | Li Xianfu Cen Boxiong |
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| Affiliation: | Li Xianfu Cen Boxiong |
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| Abstract: | The Hu-Bi Copper deposits of shanxi province occur in the Early Proterozonic Zhongtiao Group. Previous workers on the area count them as metamorphic-sedimentary deposits controled by Bizigou Formation. But based on the geological mappong and structural analysis of the ore area, we have demonstrated that Bizigou formation took place faulting and folding, and the mineracizational marble is yuji as ban Formation (not Bizigou Formation). So" the formationdl controling deposit" islack of the most foandationalgeoloyical evidences. As a matter of fact, the Hu-Bi deposits are associated with the denudational faults, and the copper sources, distribution of orebody over the area, the mineracizational characteristics et al are controled by the faults. |
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| Keywords: | Deposit origins Denudational fault controling deposits Hu-Bi copper de-posits Zhongtiao mountains in shanxi province of china |
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