| 冀西安妥岭斑岩型钼矿成矿地质条件浅析 |
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| 引用本文： | 李会恺,;乔增宝,;韩亮,;鹿波,;赵体群.冀西安妥岭斑岩型钼矿成矿地质条件浅析[J].山东地质,2009(9):20-25. |
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| 作者姓名： | 李会恺 ;乔增宝 ;韩亮 ;鹿波 ;赵体群 |
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| 作者单位： | [1]天津华北地质勘查总院,天津300181; [2]山东省第一地质矿产勘查院,山东济南250014 |
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| 摘 要： | 安妥岭钼矿位于燕辽钼（铜）成矿带南端,与附近的野弧斑岩型钼矿等具有相同的地质背景和成矿条件。文章阐述了古结晶基底、中生代岩体以及NNE、NW和近EW向构造与成矿的关系,提出安妥岭钼矿是在斑岩型矿床基础上,叠加了主要沿NW向构造发育的岩浆热液成矿作用所形成的具有复杂成矿系列的非典型斑岩钼矿床。
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| 关 键 词： | 钼矿 燕辽钼(铜)成矿带 斑岩型矿床 成矿系列 叠加成矿作用 冀西安妥岭 |
Primary Study on Mineralization Geological Condition of Porphyry--type Molybdenum Deposit in Antuoling of Western Hebei Province |
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| Institution: | LI Hui-- kai , QIAO Zeng-- bao , HAN Liang , LU Bo , ZHAO Ti-- qu (1. Tianjin Northern China Geological Exploration Institute,Tianjin 300181, China; 2. No. 1 Exploration Institute of Geology and Mineral Resources,Shandong Jinan 250014, China) |
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| Abstract: | Antuoling molybdenum deposit locates in south part ol Yanllao Molybdenum（Cu） minerailzauon belt. It has the same geological background and mineralization condition with the nearby Yehu porphyrite molybdenum deposit. Relationship among mineralization, ancient crystal basement, the Mesozoic rockbody and the structures with the trend of NNE, NW and nearly EW are illustrated in this paper. It points out that Antuoling molybdenum deposit is untypical porphyry--type deposit with complex mineralization series, which is stacked by the magma hydrothermal mineralization occuring along the NW trend structure. |
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| Keywords: | Molybdenum deposit Yanliao Mo（Cu） mineralization belt porphyry- type deposit minerali-zation series stacking mineralization Antuoling in estern Hebei province |
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