Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (4): 1030-1041.doi: 10.13278/j.cnki.jjuese.20200167

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Control of Tectonic Evolution on Mineralization of Sandstone Type Uranium Deposits in Northern Songliao Basin

Xi Haiyin1, Fan Yueye2, Wang Guangting2, Zhang Yang2   

  1. 1. Hunan Mining and Metallurgy Bureau of Nuclear Industry, Changsha 410016, China;
    2. Research Institute No. 240, CNNC, Shenyang 110032, China
  • Received:2020-07-21 Online:2021-07-26 Published:2021-08-02
  • Supported by:
    Supported by the Uranium Geological Exploration Project of China Nuclear Geological Bureau (202024)

Abstract: The structural evolution of Songliao basin can be divided into seven evolution stages:The pre Mesozoic craton basement evolution, the Late Jurassic compressional volcanic dome evolution, the Early Cretaceous extensional fault depression, the early stage of Upper Cretaceous cooling depression, the late stage of Upper Cretaceous reverse fold uplift and atrophy, the uplift and denudation of Paleogene extensional fault,and the Neogene Quaternary compression depression.The relationship between the structural evolutions and the uranium mineralization in the North of Songliao basin was studied systematically. The results show that the main stages of uranium mineralization are in the early stage of Upper Cretaceous cooling depression, late stage of Upper Cretaceous reverse fold uplift and atrophy, uplift, and denudation,and Paleogene extensional fault depression uplifting and denuding. The distribution of uranium mineralization is jointly controlled by the basement fracture and the reverse tectonic zone.The uranium metallogenic types of each tectonic division are controlled by the structural evolutions:The "paleo-interlayer oxidation" and interlayer oxidation sandstone type uranium deposit are the main types in the western slope area.The type of "Qianjiadian sandstone type uranium deposit" should be searched in the structural denudation skylight of Changqi Placantieline and Suileng anticline belt of central depression and northeastern uplift area; While the interlayer oxidation type sandstone type uranium deposit is the main type in the northern tilted area and the basin margins of the northeastern uplift area.

Key words: Northern Songliao basin, tectonic evolution, basement fracture, structural inversion, sandstone type uranium deposit

CLC Number: 

  • P542
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