| 福建南平巨口白石岩钼矿床地质特征及成因探讨 |
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| 引用本文： | 黄道锐.福建南平巨口白石岩钼矿床地质特征及成因探讨[J].福建地质,2008,27(3):275-280. |
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| 作者姓名： | 黄道锐 |
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| 作者单位： | 福建省闽清县国土资源局,闽清,350800 |
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| 摘 要： | 南平巨口白石岩钼矿床位于闽西北隆起带的东南边缘与浦城-嵩口南北向断裂带交汇部位，产于燕山早期黑云母花岗岩小岩株的相变带上，矿化蚀变分带和工业钼矿体的容矿岩百、结构构造显示为成分单一的岩浆期后热液充填交代型钼矿床。
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| 关 键 词： | 钼矿床 热液充填交代型 南北向断裂带 找矿方向 |
Geologic Characteristics and Genesis of the Baishiyan Molybdenum Deposit in Nanping, Fujian Province |
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| Huang Daorui.Geologic Characteristics and Genesis of the Baishiyan Molybdenum Deposit in Nanping, Fujian Province[J].Geology of Fujian,2008,27(3):275-280. |
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| Authors: | Huang Daorui |
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| Institution: | Huang Daorui ( Minqing Land and Resources Bureau of Fujian Province, Minqing , 350800) |
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| Abstract: | The Baishiyan molybdenum deposit in Nanping City is situated at the interjunction between the southeast fringe of Northwestern Fujian mole track and the Pucheng-Songkou north-south-trend fault zone and was discovered in the facies change belt of small biotite-granite stock intruded in the early Yanshanian stage.The host rocks and structures of the mineralizing and alteration zoning and the industry molybdenum orebody show that it is the simplex hydrothermal filling and metasomatic type of the molybdenum deposit forming in the magmatic post-stage. |
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| Keywords: | molybdenum deposit hydrothermal filling and metasomatic type north-south-trend fault zone ore-finding target |
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