| 珲春农坪金（铜）矿床地质特征及成因机制 |
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| 引用本文： | 刘玉平 李晨晖. 珲春农坪金（铜）矿床地质特征及成因机制[J]. 吉林地质, 1999, 18(4): 43-48 |
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| 作者姓名： | 刘玉平 李晨晖 |
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| 作者单位： | 吉林有色地质勘查局603队!吉林珲春133300 |
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| 摘 要： | 农坪金（铜）矿床受控于东西向断裂构造带，产于英云闪长（斑）岩蚀变岩中，与闪长玢岩密切相关。矿床成因类型为次火山热液含金慢变岩型。矿床类型特殊，外围找矿潜力较大，对珲春地区金、铜找矿具有指导意义。
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| 关 键 词： | 金矿床 铜矿床 地质特征 成因机制 |
The geological features and origin mechanism of the Nongping Au (Cu) deposit, Hunchun, Jilin province |
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| LIU Yu-ping,LI Chen-hui. The geological features and origin mechanism of the Nongping Au (Cu) deposit, Hunchun, Jilin province[J]. Jilin Geology, 1999, 18(4): 43-48 |
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| Authors: | LIU Yu-ping LI Chen-hui |
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| Abstract: | Nongping Au (Cu) deposit is controlled by W -E feaulted strctural zone and occurs in tonalite, tonalitic porphyry altered rocks which is closely related to tonalitic porphyrite. The origin type of ore deposit is a subvolcanic hydrothermal gold - bearing, altered rock type. Because of unusual deposit type, it has a considerable potentiality for prospecting at its adjacent area, and has a guidable significance to the Au, Cu deposit in the Hunchun area, Jilin province. |
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| Keywords: | Au (Cu) deposit geological features origin mechanism Hunchun Nongping |
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