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长城堡岩体西段放射性水文地质特征及其找矿方向
引用本文:董光国,戴永久.长城堡岩体西段放射性水文地质特征及其找矿方向[J].铀矿地质,2006,22(2):104-109,128.
作者姓名:董光国  戴永久
作者单位:甘肃省核工业地质局,甘肃,兰州,730000
摘    要:文章论述了长城堡岩体西段放射性水文地质特征、水化学异常特征和铀矿化特征,探讨了三者之问的相关关系;指出该区铀矿化受水化学异常区和水文地球化学垂直分带的控制,铀主要富集在氧化-还原过渡带;根据该区铀易浸出的特点,认为适合于用溶浸和地浸法开采。

关 键 词:长城堡岩体  放射性水文地质  水化学异常  铀矿化  溶浸  堆浸
文章编号:1000-0658(2006)02-0104-07
收稿时间:2005-11-30
修稿时间:2005-11-302006-01-16

Radioactive hydrogeologic features and uranium prospecting direction in western Changchengbao massif
DONG Guang-guo,DAI Yong-jiu.Radioactive hydrogeologic features and uranium prospecting direction in western Changchengbao massif[J].Uranium Geology,2006,22(2):104-109,128.
Authors:DONG Guang-guo  DAI Yong-jiu
Institution:Bureau of Geology, Gansu Nuclear Industry, Lanzhou , Gansu 730000, China
Abstract:Radioactive hydrogeologic and hydrochemical anomaly features and characteristics of uranium mineralization are introduced in this paper. The mutural relationship among the above three factors is discussed in detail. It is proposed that uranium mineralization in this area are controlled by hydrochemical anomaly areas and hydrogeochemical vertical zonation in this area. Uranium is mainly concentrated in the transitional zone of oxidation-reduction. Because the uranium in the working area is easily leachable, it is suggested that uranium deposits to be explored would be suitable for solution leaehing and in situ leach mining
Keywords:Changchengbao massif  radioactive hydrogeology  hydrochemical anomaly  solution leaching  heap leaching
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