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Volume 33 Issue 2
Apr 2022
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Journal of Earth Science  > 2022  >  33(2): 409-421.
Liqun Wu, Yangquan Jiao, Yunbiao Peng, Hui Rong. Uranium Metallogeny in Fault-Depression Transition Region: A Case Study of the Tamusu Uranium Deposit in the Bayingobi Basin. Journal of Earth Science, 2022, 33(2): 409-421. doi: 10.1007/s12583-021-1553-5
Citation: Liqun Wu, Yangquan Jiao, Yunbiao Peng, Hui Rong. Uranium Metallogeny in Fault-Depression Transition Region: A Case Study of the Tamusu Uranium Deposit in the Bayingobi Basin. Journal of Earth Science, 2022, 33(2): 409-421. doi: 10.1007/s12583-021-1553-5
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Uranium Metallogeny in Fault-Depression Transition Region: A Case Study of the Tamusu Uranium Deposit in the Bayingobi Basin

doi: 10.1007/s12583-021-1553-5
  • 1.

    Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China

  • 2.

    Geologic Party No. 208, BOG, CNNC, Baotou 014040, China

More Information
  • Corresponding author: Liqun Wu, lqwu@cug.edu.cn
  • Received Date: 03 Aug 2020
  • Accepted Date: 22 Sep 2021
  • Publish Date: 30 Apr 2022
    Abstract
  • Compared to the sandstone-type uranium deposits in the Ordos Basin and the Songliao Basin, the Tamusu uranium deposit in the Bayingobi Basin formed in fault-depression transition region displays distinctive features. First, the uranium-bearing sandstones and their interlayer oxidation zone extend longitudinally no more than ten kilometers. Second, gravity flow sediments are more common in the uranium-bearing strata. Comprehensive facies analysis indicates that the Upper Member (ore-bearing horizon) of the Bayingobi Formation was largely deposited in fan deltas that prograded into lakes during period of relatively dry paleoclimate. Spatial distribution patterns of five facies associations along with two depositional environments (fan delta, lake) were reconstructed in this study. The results demonstrated that the depositional systems and their inner genetic facies played different roles in uranium reservoir sandstone, confining beds (isolated barrier beds) and reduction geologic bodies during uranium mineralization process.

     

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