ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
广西花山铀矿床氧化带中铀酰矿物特征、成因及其勘查指示意义
  
关键词:uranyl minerals  U deposit  oxidized belt  Huashan  Guangxi
基金项目:国家自然科学青年基金项目(编号: 41102051);广西自然科学基金项目(编号: 2012GXNSFAA053187; 2013GXNSFBA019209);广西大规模地质矿产勘查项目(编号: 桂财建函[2010]130号);广西重点实验室建设项目(编号: 11-031-20; 12-071-20)
作者单位E-mail
付伟 桂林理工大学广西矿冶与环境科学实验中心
桂林理工大学地球科学学院 
fuwei@glut.edu.cn 
冯佐海 桂林理工大学广西矿冶与环境科学实验中心
桂林理工大学地球科学学院 
 
黄永高 桂林理工大学地球科学学院  
柴明春 桂林理工大学地球科学学院  
康志强 桂林理工大学广西矿冶与环境科学实验中心
桂林理工大学地球科学学院 
 
余勇 桂林理工大学广西矿冶与环境科学实验中心
桂林理工大学地球科学学院 
 
杨梦力 桂林理工大学地球科学学院  
江超强 桂林理工大学地球科学学院  
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摘要:
Mineralogical Characteristics and Genesis of the Uranyl Minerals in the Oxidized Zone of the Huashan Deposit, Guangxi, and Their Implications for Deep Ore Exploration
      This study aims at revealing the mineralogical characteristics of the uranyl minerals from the oxidized zone of the Huashan deposit in Guangxi and investigating their genetic mechanism in relation to deep ore exploration. The authors have found that there are different mineral assemblages in the three ore spots of the study area, with the assemblage of meta-autunite, autunite and uranophane in the Changchong ore spot, that of kasolite and parsonsite in the Baishijiao ore spot, and that of zeunerite, torbernite and gummite in the Zhaomiping ore spot. These uranyl minerals were derived from the primary U-bearing mineral (uraninite) and formed by the secondary precipitation process in an oxidation environment. Different uranyl mineral assemblages in the three ore spots are attributed to element geochemical backgrounds of the primary ore bodies, types of the complex anions in the groundwater solutions, and Ph values of the U-bearing groundwater. This study indicates that the uranyl minerals can provide important clues for deep exploration; for example, the uranyl minerals are extensively developed along the faults, and their characteristics have recorded the location of the primary ore body and the information of the primary ore grade and sulfide content. It is held that there are good potentials for further prospecting in the Baishijiao and Zhaomiping ore spots.
FU Wei,FENG Zuo-hai,HUANG Yong-gao,CHAI Ming-chun,KANG Zhi-qiang,YU Yong,YANG Meng-li,JIANG Chao-qiang.2014.Mineralogical Characteristics and Genesis of the Uranyl Minerals in the Oxidized Zone of the Huashan Deposit, Guangxi, and Their Implications for Deep Ore Exploration[J].Acta Geoscientica Sinica,35(3):295-304.
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