| 某花岗伟晶岩型铀矿床铀迁移沉淀机制探讨 |
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| 引用本文： | 曾令交 金景福. 某花岗伟晶岩型铀矿床铀迁移沉淀机制探讨[J]. 华东地质学院学报, 1994, 17(3): 264-269 |
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| 作者姓名： | 曾令交 金景福 |
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| 作者单位： | 四川省地矿局科研所，成都理工学院 |
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| 摘 要： |
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| 关 键 词： | 铀矿床 铀迁移 沉淀机制 伟晶岩型 |
DISCUSSION ON THE MIGRATION AND PRECIPITATION MECHANISM OF THE URANIUM IN SOME GRANITE-PEGMATITE TYPE URANIUM DEPOSIT |
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| Zeng Lingjiao. DISCUSSION ON THE MIGRATION AND PRECIPITATION MECHANISM OF THE URANIUM IN SOME GRANITE-PEGMATITE TYPE URANIUM DEPOSIT[J]. Journal of East China Institute of Technology, 1994, 17(3): 264-269 |
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| Authors: | Zeng Lingjiao |
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| Affiliation: | Zeng Lingjiao(Sichuan Research Institute of the Bureau of Geology and Mineral Resources)Jin Jingfu(Chengdu Institute of Science and Engineering) |
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| Abstract: | This papre focuses on the physicochemical conditions of uranium mineralization inGuangshigou granite-pegmatite type uranium deposit and the mechanism of migration and precip-itation of uranium in the pneumatolytic hydrothermal solution according to the theories and meth-ods of thermodynamics. The studies show that U-bearing pneumato hydrothermal fluid is a re-ductive and acidic medium. Among it is a predominant form of uranium migration. In themineralized period,the formation of biotite reduce the content of fluorine and make in thestate of hydrolysis and form uraninite. |
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| Keywords: | Pneumatolytic hydrothermal fluid migrational form hydrolysis |
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