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Analysis of Metallogenic Conditions of InSitu Leachable Sandstone Type Uranium Deposit in the Southeastern Margin of Songliao Basin

YU Wen-bin1,2, DONG Qing-shui1, ZOU Ji-bin2, FENG Ben-zhi1   

  1. 1.College of Earth Sciences, Jilin University, Changchun 130061, China；2.The No.243 Team of China Nuclear Industry, Chifeng,Inner Mongolia 024006,China
  • Received:2005-11-26 Revised:1900-01-01 Online:2006-07-26 Published:2006-07-26
  • Contact: YU Wen-bin

Abstract: The analyses of the sedimentary facies, rock geochemistry and reformation after the sedimentation from the Upper Cretaceous Quantou Formation to Nenjiang Formation indicate that the beneficial sandbodies of the uranium deposit are mainly Quantou Formation’s braided channel and Qingshankou Formation’s delta sandstone types. By summarizing and analyzing the geological setting, uranium source, paleoclimate, hydrology, lithologiclithofacies conditions in the region, it is indicated that the Quantou Formation in Fanjiatun-Jiutai area and the Qingshankou Formation in Yangdachenzi area are potential metallogenic prospective areas for insitu leachable sandstone type uranium deposit in the region, which develop braided channel or delta marginal sandstones, and possess favorable forming conditions of interlayer oxidation zone, and constituting supply-passage-discharge system of abundant uranium source.

Key words: Songliao Basin, Upper Cretaceous, suti leachable sandstone type uranium deposit, metallogenic condition

CLC Number: 

  • P619.14
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