| 720铀矿床围岩蚀变及地球化学特征 |
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| 引用本文： | 王隆秋.720铀矿床围岩蚀变及地球化学特征[J].湖南地质,1994,13(1):11-16. |
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| 作者姓名： | 王隆秋 |
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| 作者单位： | 中南地质勘探局３０１大队 |
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| 摘 要： | 通过对蚀变带地球化学特征的研究，发现矿床的硅质热液源于岩浆残余热液，而碳酸盐热液则主要源于下降热水；并阐明了形成该铀矿床的某些特定物理化学条件。
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| 关 键 词： | 铀矿床 围岩蚀变 地球化学 |
Geochemical Characteristic and Wallrock Alteration in No:720 Uranium Deposit |
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| WazngLongqiu.Geochemical Characteristic and Wallrock Alteration in No:720 Uranium Deposit[J].Hunan Geology,1994,13(1):11-16. |
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| Authors: | WazngLongqiu |
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| Institution: | 301 Brigade of Central South Bureau of Geology and Prospecting |
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| Abstract: | Through the study of geochemical characteristic of altered zone,it is found that the siliceous hy drothermal solution originates from survival magma aqueous fluid,and the carbOnate solutiOn is mainly derlved from supergene hot water.This paper descrlbes some speclal physiochemical conditions which give important in-fluence to the formation of the deposit. |
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| Keywords: | geochemistry in altered zone the source of hydrothermal solution criteria of prospecting |
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