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

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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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Authors and Affiliations

  1. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, 630090, Russia

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

  2. Tomsk State University, Tomsk, 634050, Russia

    A. G. Vladimirov

  3. Novosibirsk State University, Novosibirsk, 630073, Russia

    S. K. Krivonogov

  4. Tomsk Department of the Institute of Petroleum-Gas Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, Tomsk, 630090, Russia

    M. N. Kolpakova

Authors
  1. A. G. Vladimirov
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  2. S. K. Krivonogov
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  3. A. V. Karpov
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  4. I. V. Nikolaeva
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  5. L. I. Razvorotneva
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  6. M. N. Kolpakova
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  7. E. N. Moroz
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Corresponding author

Correspondence to A. G. Vladimirov.

Additional information

Original Russian Text © A.G. Vladimirov, S.K. Krivonogov, A.V. Karpov, I.V. Nikolaeva, L.I. Razvorotneva, M.N. Kolpakova, E.N. Moroz, 2018, published in Doklady Akademii Nauk, 2018, Vol. 479, No. 6, pp. 659–665.

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Vladimirov, A.G., Krivonogov, S.K., Karpov, A.V. et al. The Main Factors of Uranium Accumulation in the Ishim Plain Saline Lakes (Western Siberia). Dokl. Earth Sc. 479, 511–517 (2018). https://doi.org/10.1134/S1028334X18040281

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  • DOI: https://doi.org/10.1134/S1028334X18040281

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