| 福建政和上山岗金银矿床地质特征 |
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| 引用本文： | 王波涛,唐祥应.福建政和上山岗金银矿床地质特征[J].中国科技博览,2013(27):495-496. |
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| 作者姓名： | 王波涛 唐祥应 |
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| 作者单位： | 中国冶金地质总局二局,福州350001 |
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| 摘 要： | 福建政和上山岗金银矿床位于闽西北隆起带与闽东火山断坳带交接部位，金银矿体主要赋存于石英脉中，围岩为多屑凝灰岩、岩屑晶屑凝灰岩等，矿体与围岩界限清晰。矿区内构造发育，其中北东向断裂构造是最重要的导矿和容矿构造；北西向断裂为成矿后期构造，是主要的切割破坏矿体构造。
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| 关 键 词： | 金银矿床 地质特征 上山岗 福建省 |
Geological characteristics of Shangshangang gold- silver deposit in Zhenhe,Fujian province |
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| Wang Botao,Tang Xiangying.Geological characteristics of Shangshangang gold- silver deposit in Zhenhe,Fujian province[J].ZHONGGUO BAOZHUANG KEJI BOLAN,2013(27):495-496. |
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| Authors: | Wang Botao Tang Xiangying |
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| Affiliation: | No.2 Bureau of China Metallurgical Geology Bureau Fujian Fuzhou |
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| Abstract: | Shangshangang gold-silver deposit in Zhenghe of Fujian province is located in the adjoiner of the Northwestern Fujian mole track and the eastern Fujian volcanic fault depression zone. The gold-silver ore bodies are hosted in quartz vein. wail rocks are crystal tuff, debris- crystal tuff et al,and the boundaries clear between ore bodies and wall rocks.The faulted structure is extremely well-developed in Shangshangang gold-silver deposit. NE-direction faults are the main lead ore and ore structure. NW-direction faults are late ore-forming structure and cut and damaged the ore bodies. |
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| Keywords: | gold-silver deposit Geological characteristics Shangshangang Fujian province |
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