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Doklady Earth Sciences

, Volume 479, Issue 2, pp 511–517 | Cite as

The Main Factors of Uranium Accumulation in the Ishim Plain Saline Lakes (Western Siberia)

  • A. G. Vladimirov
  • S. K. Krivonogov
  • A. V. Karpov
  • I. V. Nikolaeva
  • L. I. Razvorotneva
  • M. N. Kolpakova
  • E. N. Moroz
Geochemistry

Abstract

Hydrochemical analysis of the high-salinity lakes in the Ishim Plain (>250–300 g/L) located at the border with the Northern Kazakhstan uranium ore province is performed. The studies have shown that the main factor of concentration and redistribution of uranium in the lake basins of the Ishim Plain are the processes of intense salt deflation causing sanding of lakes and uranium depletion in the near-surface layer of the bottom deposits. The correlation between the hydroxide forms of uranium binding in the bottom lacustrine deposits of the Ishim Plain and the coffinite composition of the Semizbai deposit makes it possible to consider this province to be promising for the discovery of hydromineral uranium deposits.

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Copyright information

© Pleiades Publishing, Ltd. 2018

Authors and Affiliations

  • A. G. Vladimirov
    • 1
    • 2
  • S. K. Krivonogov
    • 1
    • 3
  • A. V. Karpov
    • 1
  • I. V. Nikolaeva
    • 1
  • L. I. Razvorotneva
    • 1
  • M. N. Kolpakova
    • 1
    • 4
  • E. N. Moroz
    • 1
  1. 1.Sobolev Institute of Geology and Mineralogy, Siberian BranchRussian Academy of SciencesNovosibirskRussia
  2. 2.Tomsk State UniversityTomskRussia
  3. 3.Novosibirsk State UniversityNovosibirskRussia
  4. 4.Tomsk Department of the Institute of Petroleum-Gas Geology and Geophysics, Siberian BranchRussian Academy of SciencesTomskRussia

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