ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
鄂尔多斯盆地东胜砂岩型铀矿床成矿水化学过程探讨
  
关键词:Ordos Basin  sandstone-type uranium deposit  hydrochemical process  uranium mineralization
基金项目:国家高技术研究发展计划(863计划)项目(编号: 2012AA061801)
作者单位E-mail
吴兆剑 中国地质大学(北京)地球科学与资源学院
中国煤炭地质总局特种技术勘探中心 
wuzhj06@126.com 
易超 核工业北京地质研究院  
韩效忠 中国煤炭地质总局特种技术勘探中心  
祁才吉 中化地质矿山总局地质研究院  
惠小朝 核工业北京地质研究院  
摘要点击次数: 3518
全文下载次数: 3926
摘要:
The Water-rock Interaction Process of the Dongsheng Sandstone-type Uranium Deposit, Ordos Basin
      In order to investigate the relationship of the hydrochemical process to the uranium metallogenic mechanism of the Dongsheng uranium deposit in Ordos basin, the authors conducted contrastive mineralogical and REE geochemical analysis of non-mineralized samples in the oxidation zone and mineralized samples in the redox transitional zone by means of general slice, electron microprobe, clay mineral X-diffraction, SEM and chemical testing. Mineralogical studies show that argillic alteration and sericitization of plagioclase can be observed in all samples, and coffinite is the main uranium mineral and is always adsorbed by fragments or carbon dust. Another interesting phenomenon is that the mineralized samples in the redox transitional zone contain more carbon dust and carbonate than those in the oxidation zone. Geochemical studies indicate that non-mineralized samples in the oxidation zone and low mineralization samples in the redox transitional zone show flat REE patterns in PAAS-normalized rare earth element plots. However, samples with high uranium content in the redox transitional zone show two different REE patterns: samples with carbon dust show a MREE enrichment pattern and those with carbonate show a HREE enrichment pattern. Mineralogical and geochemical differences of samples from different zones indicate that aqueous chemical reaction is the main uranium mineralization rather than carbon absorption. In the aqueous chemical process, CO32- which prefers combining UO22+ and HRE3+ is the main inorganic complex anion in the mineralized hydrothermal water, and argillic alteration and sericitization of plagioclase with Ca2+ and SiO44- play an important role in the metallogenic process.
WU Zhao-jian,YI Chao,HAN Xiao-zhong,QI Cai-ji,HUI Xiao-chao.2014.The Water-rock Interaction Process of the Dongsheng Sandstone-type Uranium Deposit, Ordos Basin[J].Acta Geoscientica Sinica,35(3):329-337.
查看全文  查看/发表评论  下载PDF阅读器
Copyright©2008 All Rights Reserved
Sponsored by:
Address:: PostCode: Tel: E-mail: