| 福建省德化县青云山铜金矿地质特征及找矿方向 |
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| 引用本文： | 陈龙照,吴志山.福建省德化县青云山铜金矿地质特征及找矿方向[J].地质找矿论丛,2006,21(10):30-33. |
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| 作者姓名： | 陈龙照 吴志山 |
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| 作者单位： | 中国冶金地质勘查工程总局第二地质勘查院,福建莆田351111 |
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| 摘 要： | 青云山铜金矿为次火山低温热液矿床，矿区共有6个工业铜金矿体，矿体受断裂及构造蚀变带控制，Ⅰ号矿体为石英脉型，其余皆属构造破碎带蚀变岩型。矿区东矿段天花寨一带的不整合面、西矿段的深部、F37和F3断裂及旁侧次级断裂在走向（倾向）上的变化部位是下一步找矿的有利地段。
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| 关 键 词： | 青云山铜金矿 地质特征 找矿方向 福建省 |
| 收稿时间： | 07 5 2006 12:00AM |
GEOLOGICAL CHARACTERISTICS AND ORE-SEARCHING DIRECTIONS OF QINGYUNSHAN COPPER-GOLD DEPOSIT, DEHUA COUNTY, FUJIAN PROVINCE |
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| CHEN Long-zhao, WU Zhi-shan.GEOLOGICAL CHARACTERISTICS AND ORE-SEARCHING DIRECTIONS OF QINGYUNSHAN COPPER-GOLD DEPOSIT, DEHUA COUNTY, FUJIAN PROVINCE[J].Contributions to Geology and Mineral Resources Research,2006,21(10):30-33. |
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| Authors: | CHEN Long-zhao WU Zhi-shan |
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| Abstract: | Qingyunshan copper-gold deposit is a sub-volcano epithermal deposit including 6 ore bodies. The ore body is controlled by fault and the fractural-alteration zone. Ore body I is quartz vein type, the others altered cataclastic rock type. Unconformities at Tianhuazhai in the east ore domain, at depth of the west ore domain, F37 and F3 and sub-faults on either sides of them are targets for further exploration. |
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| Keywords: | province Qingyunshan copper-gold deposit geological characteristics ore-searching dirction Fujian |
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