| 樟坑铁铜多金属矿区地质特征及找矿方向 |
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| 引用本文： | 倪建辉. 樟坑铁铜多金属矿区地质特征及找矿方向[J]. 金属矿山, 2004, 0(7): 54-58,72 |
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| 作者姓名： | 倪建辉 |
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| 作者单位： | 福建省第八地质大队 |
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| 摘 要： | 在野外地质调查工作基础上，对樟坑铁铜多金属矿床的地质背景及主要地质特征进行了研究，认为矿床主要赋存于推覆构造破碎带和晚石炭世-早二叠世矽卡岩与碎屑岩过滤带中，矿床成因类型属沉积-改造型。在地质找矿思路上取得新的进展，总结成矿地质特征、探讨了矿床成因及今后找矿方向。
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| 关 键 词： | 推覆构造 铁铜多金属矿 地质特征 |
Geological Characteristics and Prospecting Direction of the Zhangkeng Iron-copper Polymetallic Ore Deposit |
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| Ni Jianhui. Geological Characteristics and Prospecting Direction of the Zhangkeng Iron-copper Polymetallic Ore Deposit[J]. Metal Mine, 2004, 0(7): 54-58,72 |
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| Authors: | Ni Jianhui |
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| Affiliation: | The No.8 Geological Team of Fujian |
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| Abstract: | Regional setting and major geological characteristics of the Zhangkeng iron-copper polymetallic ore deposit are studied on the basis of field geological survey. It can be concluded that this deposit is controlled by the nappe structure and occurs in the transitional belt between C 2-P 1 skarn and clastic rock. It is a kind of hydrothermal superimposed strate-bound deposits. New advance in prospecting thought is achieved, geological characteristics of mineralization are summarised and the mineralization causes and the oriention in future prospecting discussed. |
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| Keywords: | Nappe structure Iron-copper polymetallic ore deposit Geological characteristics |
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