| 火山岩型铀矿中基性岩与铀成矿作用研究 |
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| 引用本文： | 饶泽煌,方欣.火山岩型铀矿中基性岩与铀成矿作用研究[J].科技广场,2011(10). |
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| 作者姓名： | 饶泽煌 方欣 |
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| 作者单位： | 东华理工大学地球科学学院,江西抚州,344000 |
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| 摘 要： | 传统地球化学理论认为火山岩型铀矿的热液铀矿床中的铀都是通过氧化溶液搬运的,并由六价还原成四价而沉淀成矿;或者是是碱交代作用形成的。但大量的文献表明,铀的成矿不仅与火山岩和次火山岩有关,还与深源的中基性岩有关。
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| 关 键 词： | 火山岩型铀矿 中基性岩 铀成矿作用 |
Study of Volcanic Type Uranium Deposits Neutra and Mafic Rocks with Uranium Mineralization |
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| Rao Zehuang Fang Xin.Study of Volcanic Type Uranium Deposits Neutra and Mafic Rocks with Uranium Mineralization[J].Science Mosaic,2011(10). |
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| Authors: | Rao Zehuang Fang Xin |
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| Institution: | Rao Zehuang Fang Xin(Faculty of Geoscience,East China Institute of Technology,Jiangxi Fuzhou 344000) |
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| Abstract: | Conventional geochemical theory suggests that Volcanic hydrothermal uranium deposits of uranium are uranium oxide solution by handling,Price reduced by six tetravalent and ore deposits;or the formation of alkali metasomatism.But a lot of literature suggests that uranium mineralization not only with the volcanic and subvolcanic rocks,but also with deep source of the mafic rocks. |
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| Keywords: | Volcanic Type Uranium Deposits Neutra and Mafic Rock Uranium Mineralization |
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