| 福建省武夷山坪地钼矿床地质特征及成因探讨 |
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| 引用本文： | 傅树超. 福建省武夷山坪地钼矿床地质特征及成因探讨[J]. 地质与勘探, 2011, 47(2): 268-276 |
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| 作者姓名： | 傅树超 |
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| 作者单位： | 中国地质大学,湖北武汉,430074 |
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| 摘 要： | 坪地钼矿床位于福建省武夷山五夫镇境内,由坪地、上西坑、东坑三个钼矿段组成.控矿地质条件有早元古代大金山组变质岩、晚侏罗世中细粒钾长花岗岩和南北向断裂构造.成矿阶段分为:中高温热液成矿阶段形成坪地钼矿段,中温热液成矿阶段形成上西坑钼矿段.通过综合资料分析,表明坪地钼矿床成因类型属岩浆热液充填交代型钼矿床,成矿时代为晚侏罗...
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| 关 键 词： | 钼矿床 特征 成因 武夷山 坪地 |
| 收稿时间： | 2010-05-12 |
| 修稿时间： | 2011-01-06 |
Geologic Characters and Genesis of the Pingdi MolybdenumDeposit in the Wuyi Shan Mountains, Fujian Province |
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| FU Shu-chao. Geologic Characters and Genesis of the Pingdi MolybdenumDeposit in the Wuyi Shan Mountains, Fujian Province[J]. Geology and Prospecting, 2011, 47(2): 268-276 |
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| Authors: | FU Shu-chao |
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| Affiliation: | FU Shu-chao (China University of Geosciences,Wuhan,Hubei 430074) |
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| Abstract: | The Pingdi molybdenum deposit,located at the Wufu town,Wuyi Shan Mountains,Fujian Province,consists of three ore sections named Pingdi,Shangxikeng and Dongkeng.The ore-controlling geological conditions include the Dajinshan metamorphic rock of Early Proterozoic,intermediate-fine grained moyite of Late Jurassic and north-south trending fault structure.Its mineralization can be divided into three ore-forming stages.The Pingdi molybdenum section formed at the intermediate-high temperature hydrothermal ore-form... |
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| Keywords: | molybdenum deposit characteristic genesis Wuyi Shan Mountains Pingdi |
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