| 302铀矿床热液的混合和沸腾及其地质意义 |
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| 引用本文： | 倪师军,金景福.302铀矿床热液的混合和沸腾及其地质意义[J].成都理工大学学报(自然科学版),1992(4). |
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| 作者姓名： | 倪师军 金景福 |
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| 作者单位： | 中国科学院地球化学研究所
(倪师军)，成都地质学院(金景福) |
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| 摘 要： | 302铀矿床是在区域性地壳拉张构造背景下形成的。该矿床经历过两次热浪混合作用和一次热浪沸腾作用。热液的混合和沸腾界面与矿床垂直分带界面一致,这对于确定矿床侵蚀截面有较大的地质意义。
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| 关 键 词： | 热液的混合 热液的沸腾 铀矿床 侵蚀截面 |
THE MIXING AND BOILING OF HYDROTHERMAL SOLUTION OF URANIUM DEPOSIT No. 302 AND THE GEOLOGICAL INTERPRETATION |
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| Ni Shijun,Jin Jingfu.THE MIXING AND BOILING OF HYDROTHERMAL SOLUTION OF URANIUM DEPOSIT No. 302 AND THE GEOLOGICAL INTERPRETATION[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1992(4). |
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| Authors: | Ni Shijun Jin Jingfu |
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| Institution: | Ni Shijun;Jin Jingfu |
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| Abstract: | The mixing and boiling of hydrothermal solution of uranium deposit No. 302 occurred onthe background of regional extension of the crust. The boundary plane of the mixing and boiling ofthermal solution is consistent with that of the vertical zoning in the deposit. Therefore, this boundaryplane plays an importment part in determining the base level of erosion surface of the deposit. |
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| Keywords: | mixing of hydrothermal solution boiling of hydrothermal solution the erosion surface of the uranium deposit |
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