| 福建建阳井后钼矿地质特征及成因探讨 |
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| 引用本文： | 章振国. 福建建阳井后钼矿地质特征及成因探讨[J]. 福建地质, 2011, 30(3): 211-217 |
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| 作者姓名： | 章振国 |
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| 作者单位： | 福建省地质调查研究院,福州,350013 |
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| 摘 要： | 建阳井后钼矿位于闽西北隆起带东缘，浦城一永泰南北向构造岩浆活动带中部。矿床形成于燕山晚期，主要受区域上南北向断裂构造带控制的隐伏斑岩体控制。矿体以线脉一细脉及石英大脉型为主，围岩为中一晚元古代马面山群大岭组变质岩与加里东期二长花岗岩。
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| 关 键 词： | 钼矿床 地质特征 矿床成因 建阳井后 |
Geologic Characteristics and Genesis of the Jinghou Molybdenum Deposit in Jianyang City,Fujian Province |
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| Zhang Zhenguo. Geologic Characteristics and Genesis of the Jinghou Molybdenum Deposit in Jianyang City,Fujian Province[J]. Geology of Fujian, 2011, 30(3): 211-217 |
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| Authors: | Zhang Zhenguo |
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| Affiliation: | Zhang Zhenguo (Fujian Institute of Geology Survey and Research,Fuzhou,350013) |
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| Abstract: | The Jinghou molybdenum deposit in Jianyang City is situated at the east fringe of Northwestern Fujian mole track,in the middle of the Pucheng-Yongtai north-south-trend fault zone.It was formed in late Yenshanian,and controlled by blind porphyry body,Which was controlled by Pucheng-Yongtai north-south-trend fault zone.There are three typical types of ore: line-vein Type,veinlet type,quartz vein type.:quartz vein type and structurally altered rock type.The wall-rock lithology was metamorphic of the Daling For... |
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| Keywords: | molybdenum deposit geologic characteristics genesis of a deposit Jinghou County in Jianyang City |
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