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Comparison of the 57Fe hyperfine parameters for iron-bearing phases in some undifferentiated and differentiated meteorites

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Abstract

A comparison of the 57Fe hyperfine parameters obtained for the iron-bearing phases in some undifferentiated and differentiated meteorites using Mössbauer spectroscopy demonstrate some similarities and small differences for the same phases in different meteorites. These differences were related to small variations in the iron local microenvironments in these phases that may be a result of some variations in the chemical compositions and thermal metamorphism. The latter variations can be associated with these phases’ formation and thermal evolution in space.

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Acknowledgements

This work was supported by the Ministry of Science and Higher Education of the Russian Federation, project № FEUZ-2020-0060. The Zavaritsky Institute of Geology and Geochemistry of the Ural Branch of the Russian Academy of Sciences is supported by the Ministry of Science and Higher Education of the Russian Federation, project № AAAA-A19-119071090011-6 (A.A.M.).

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Authors and Affiliations

  1. Institute of Physics and Technology, Ural Federal University, Ekaterinburg, Russian Federation, 620002

    M. I. Oshtrakh & A.A. Maksimova

  2. The Zavaritsky Institute of Geology and Geochemistry of the Ural Branch of the Russian Academy of Sciences, Ekaterinburg, Russian Federation, 620110

    A.A. Maksimova

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  1. M. I. Oshtrakh
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Correspondence to M. I. Oshtrakh.

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This article is part of the Topical Collection on Proceedings of the International Conference on Hyperfine Interactions (HYPERFINE 2021), 5-10 September 2021, Brasov, RomaniaEdited by Ovidiu Crisan

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Oshtrakh, M.I., Maksimova, A. Comparison of the 57Fe hyperfine parameters for iron-bearing phases in some undifferentiated and differentiated meteorites. Hyperfine Interact 242, 16 (2021). https://doi.org/10.1007/s10751-021-01732-8

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