Mössbauerite; polytypes in Tatkul Lake (Russia) marls and evidence in a Murray River reservoir (Australia)

Génin, J.-M. R.;Christi, A.;Garcia, Yann;Ksenofontov, V.;Shcherbakova, E.;et.al.
(2018) Hyperfine Interactions — Vol. 239, p. 24 (2018)

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Authors
  • Génin, J.-M. R.Université de Lorraine - CNRS (France)
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  • Christi, A.Australian Natonal University (Australia)
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  • Garcia, Yannorcid-logoUCLouvain
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  • Ksenofontov, V.Johannes Gütenberg Universität - Mainz (Germany)
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  • Shcherbakova, E.Russian Academy of Sciences (Russia)
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Abstract
M¨ossbauer spectroscopy characterizes “Green rust related minerals” of the foug`erite group within the hydrotalcite supergroup (Mills et al. Mineral. Mag. 76(5), 1289–1336, 2012) in locations on Earth quite different from the original studies done in a temperate climate such as Brittany- France, Western Europe. Two examples are described, the gley at the bottom of Tatkul Lake in South Urals (Russia), which is representative of permafrost conditions, and a gley at the bottom of Yanga Lake, a reservoir in the Murray River catchment (NSW-Australia), which is representative of warm and desert conditions. Complementary information is obtained from XRD patterns.
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Génin, J.-M. R., Christi, A., Garcia, Y., Ksenofontov, V., Mills, S., Ruby, C., & Shcherbakova, E. (2018). Mössbauerite; polytypes in Tatkul Lake (Russia) marls and evidence in a Murray River reservoir (Australia). Hyperfine Interactions, 239, 24. https://doi.org/10.1007/s10751-018-1497-z (Original work published 2018)