| 福吉山铜矿矿床地质特征和矿床成因 |
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| 引用本文： | 程光锁,罗文强,单伟,王英,王秀风.福吉山铜矿矿床地质特征和矿床成因[J].有色金属(矿山部分),2009,61(6):33-36. |
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| 作者姓名： | 程光锁 罗文强 单伟 王英 王秀风 |
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| 作者单位： | 1. 中国地质大学(北京)地球科学与资源学院,北京,100083;山东地质科学实验研究院,山东,济南,250013
2. 山东地质科学实验研究院,山东,济南,250013 |
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| 摘 要： | 福吉山铜矿成矿地质特点不同于山东已有的铜矿类型,属于构造热液成因类型。通过对福吉山铜矿床的地质特征、控矿因素及矿床成因的研究,认为矿区近南北向的断裂为铜矿的有利成矿部位,提出应加大矿区深部及外围的找矿力度,进而指出了相应的找矿方向。
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| 关 键 词： | 铜矿 地质特征 矿床成因 福吉山 |
Geological Characteristics and Genesis of Fujishan Copper Deposits |
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| Authors: | CHENG Guangsuo LUO Wenqiang SHAN Wei WANG Ying WANG Xiufeng |
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| Abstract: | The characteristics of Fujishan copper deposits belong to structural hydrothermal type,which are different from the other studied copper deposits in Shandong province.Through study on geological characteristics,ore-controlling factors and genesis of Fujishan copper deposits,it is summarized that the fault with Nearly S-N trend are favorable ore-forming areas.It is put forward that ore exploration in deep and surrounding areas should be strengthened,and ore exploration direction should be studied further in order to find new copper deposits areas in the future. |
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| Keywords: | copper deposits geological characteristics deposit genesis Fujishan |
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