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Determination of quadrupole splitting for 57Fe in M1 and M2 sites of both olivine and pyroxene in ordinary chondrites using Mössbauer spectroscopy with high velocity resolution

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Abstract

Study of 11 ordinary chondrites using Mössbauer spectroscopy with high velocity resolution revealed two crystallographically non-equivalent octahedral sites M1 and M2 in subspectra of olivine and pyroxene which were observed previously in pure natural or synthetic silicates only. Mössbauer hyperfine parameters related to M1 and M2 sites in olivine and pyroxene determined from Mössbauer spectra of ordinary chondrites were analyzed and compared with parameters of pure natural and synthetic silicates.

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Authors and Affiliations

  1. Faculty of Physical Techniques and Devices for Quality Control, Ural State Technical University—UPI, Ekaterinburg, 620002, Russian Federation

    M. I. Oshtrakh, E. V. Petrova & V. I. Grokhovsky

  2. Faculty of Experimental Physics, Ural State Technical University—UPI, Ekaterinburg, 620002, Russian Federation

    V. A. Semionkin

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  1. M. I. Oshtrakh
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  2. E. V. Petrova
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  3. V. I. Grokhovsky
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  4. V. A. Semionkin
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Correspondence to M. I. Oshtrakh.

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Oshtrakh, M.I., Petrova, E.V., Grokhovsky, V.I. et al. Determination of quadrupole splitting for 57Fe in M1 and M2 sites of both olivine and pyroxene in ordinary chondrites using Mössbauer spectroscopy with high velocity resolution. Hyperfine Interact 177, 65–71 (2007). https://doi.org/10.1007/s10751-008-9646-4

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  • DOI: https://doi.org/10.1007/s10751-008-9646-4

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