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Gibbsite and kaolinite in the biological pedoturbation zone of the lateritic profile: A different fate (exemplified by deposits of Siberia, India, Guinea, and Brazil)

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Authors and Affiliations

  1. Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry (IGEM), Russian Academy of Sciences, Moscow, Russia

    A. D. Slukin, N. S. Bortnikov, A. P. Zhukhlistov & N. M. Boeva

  2. Borisyak Paleontological Institute, Russian Academy of Sciences, Moscow, Russia

    E. A. Zhegallo

Authors
  1. A. D. Slukin
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  2. N. S. Bortnikov
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  3. E. A. Zhegallo
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  4. A. P. Zhukhlistov
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  5. N. M. Boeva
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Corresponding author

Correspondence to N. M. Boeva.

Additional information

Original Russian Text © A.D. Slukin, N.S. Bortnikov, E.A. Zhegallo, A.P. Zhukhlistov, N.M. Boeva, 2014, published in Doklady Akademii Nauk, 2014, Vol. 458, No. 5, pp. 572–577.

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Slukin, A.D., Bortnikov, N.S., Zhegallo, E.A. et al. Gibbsite and kaolinite in the biological pedoturbation zone of the lateritic profile: A different fate (exemplified by deposits of Siberia, India, Guinea, and Brazil). Dokl. Earth Sc. 458, 1220–1225 (2014). https://doi.org/10.1134/S1028334X14100213

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  • DOI: https://doi.org/10.1134/S1028334X14100213

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