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57Fe hyperfine interactions in M1 and M2 sites of olivine from Omolon meteorite: study using Mössbauer spectroscopy

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Abstract

Study of olivine (Fe, Mg)2SiO4 from Omolon meteorite was performed using Mössbauer spectroscopy with a high velocity resolution at 295 and 90 K. Components related to 57Fe in crystallographically non-equivalent M1 and M2 sites in olivine were determined and its Mössbauer hyperfine parameters were evaluated at both temperatures. A Fe2 + –Mg2 +  distribution coefficient and a temperature of cation equilibrium distribution for olivine from Omolon were evaluated on the basis of Mössbauer parameters.

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Authors and Affiliations

  1. Faculty of Physical Techniques and Devices for Quality Control, Ural Federal University, Ekaterinburg, 620002, Russian Federation

    D. G. Patrusheva, M. I. Oshtrakh, E. V. Petrova, V. I. Grokhovsky & V. A. Semionkin

  2. Faculty of Experimental Physics, Ural Federal University, Ekaterinburg, 620002, Russian Federation

    V. A. Semionkin

Authors
  1. D. G. Patrusheva
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  2. M. I. Oshtrakh
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  3. E. V. Petrova
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  4. V. I. Grokhovsky
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  5. V. A. Semionkin
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Correspondence to M. I. Oshtrakh.

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Patrusheva, D.G., Oshtrakh, M.I., Petrova, E.V. et al. 57Fe hyperfine interactions in M1 and M2 sites of olivine from Omolon meteorite: study using Mössbauer spectroscopy. Hyperfine Interact 197, 295–300 (2010). https://doi.org/10.1007/s10751-010-0188-1

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  • DOI: https://doi.org/10.1007/s10751-010-0188-1

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