| 211地区铀矿床的稳定同位素地球化学特征 |
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| 引用本文： | 黄锦培. 211地区铀矿床的稳定同位素地球化学特征[J]. 物探化探计算技术, 1996, 0(S5) |
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| 作者姓名： | 黄锦培 |
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| 作者单位： | 新会市金星管柱有限公司 |
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| 摘 要： | 本文在讨论了 2 11地区花岗岩型铀矿床的稳定同位素组成的基础上 ,提出该区铀成矿热液可能主要来自晚期花岗岩浆 ,部分来自大气降水
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| 关 键 词： | 稳定同位素 热液来源 铀矿床 |
THE GEOCHEMICAL CHARACTERISTIC OF STABLE ISOTOPE OF URANIUM DEPOSITS IN 211 AREA |
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| Huang Jinpei. THE GEOCHEMICAL CHARACTERISTIC OF STABLE ISOTOPE OF URANIUM DEPOSITS IN 211 AREA[J]. Computing Techniques For Geophysical and Geochemical Explorationxploration, 1996, 0(S5) |
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| Authors: | Huang Jinpei |
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| Abstract: | After discussing the composition of the stable isotope of Uranium deposits in 211 area, this paper suggests that the mineral-formation hydrothermal solution of uranium many comes from the late granite magma, partly from the rain on the surface. |
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| Keywords: | stable isotope mineral-formation hydrothermal solution uranium deposits. |
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