| 安徽省全椒县大庙山金矿床地质特征 |
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| 引用本文： | 吴礼彬,孙亚力,程光文,李希隆.安徽省全椒县大庙山金矿床地质特征[J].安徽地质,2000(1). |
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| 作者姓名： | 吴礼彬 孙亚力 程光文 李希隆 |
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| 作者单位： | 安徽省地质矿产局312地质队!安徽 蚌埠 233040(吴礼彬，孙亚力，程光文)，安徽省地质矿产局312地质队!安徽 蚌埠233040(李希隆) |
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| 摘 要： | 大庙山金矿床产于震旦纪灯影组中段地层中，是多种成矿作用叠加改造的产物，成矿物质来 自于岩浆期后热液和灯影组碎屑岩。黄－破断裂是其主要的导矿构造，其次级低序次ＮＮＥ向断裂带是 主要的容矿构造。
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| 关 键 词： | 金矿床 前陆褶冲带 矿床地质特征 |
THE GEOLOGICAL FEATURES OF THE DAMIAOSHAN GOLD DEPOSIT, QUANJIAO, ANHVI |
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| WU Li - bin,SUN Ya -li,CHENG Guang - wen,LI Xi - long.THE GEOLOGICAL FEATURES OF THE DAMIAOSHAN GOLD DEPOSIT, QUANJIAO, ANHVI[J].Geology of Anhui,2000(1). |
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| Authors: | WU Li - bin SUN Ya -li CHENG Guang - wen LI Xi - long |
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| Abstract: | The Damiaoshan gold deposit occurred in the middle member of the Sinian Dengying Formation. It is resulted from polymetallogenic reworking and sourced from post - magmatic hydrothermal solution and the detrital rock of the Dengying Formation. The Huangpo Fault is as the passage - way for its ore fluid and the sub - order NNE - trending fault zone acts as the main host. |
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| Keywords: | gold deposit foreland fold and thrust zone geological features of ore deposit |
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