Earth Science Frontiers ›› 2018, Vol. 25 ›› Issue (6): 290-295.DOI: 10.13745/j.esf.sf.2018.11.5

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Research on the current status and future of U-Pb chronology study of uranium minerals from the sandstone-type uranium deposits.

ZHOU Hongying,TU Jiarun,LI Guozhan,XIAO Zhibin,GENG Jianzhen,GUO Hu,YE Lijuan,XU Yawen,ZHANG Jian,LI Huimin   

  1. 1. Tianjin Center of Geological Survey, China Geological Survey, Tianjin 300170, China 
    2. Key Laboratory of Muddy Coast Geo-Environment, China Geological Survey, Tianjin 300170, China
  • Received:2018-07-08 Revised:2018-09-07 Online:2018-11-30 Published:2018-11-30
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Abstract: In recent years we have conducted in-depth studies on the genetic mineralogy and U-Pb geochronology of uranium minerals (uraninite, coffinite, brannerite, etc.) and U-bearing minerals (rutile, apatite, etc.) from sandstone-type uranium deposit, using jointly secondary ion mass spectrometry, laser ablation multi-collector inductively coupled plasma mass spectrometry, electron probe microanalysis and isotope dilution-thermal ionization mass spectrometry. New methods of U-Pb isotopic dating for uranium minerals, however, should be tested and established in order to acquire accurate formation time for rocks and minerals from sandstone-type uranium deposit. Such knowledge is important for a comprehensive and accurate understanding of the formation and evolutionary history of the sandstone-type uranium deposit and for developing a new mineralization theory for sandstone-type uranium deposit. The new isotopic dating methodology will also have a broad application in uranium geological exploration.

 

Key words: sandstone-type uranium deposit, uranium minerals, U-Pb chronology, in-situ, ID-TIMS

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