Mössbauer Spectroscopy with a High Velocity Resolution Applied to the Study of Iron-Bearing Phases in Meteorites

The results of our studies of iron-bearing phases in various meteorites using Mössbauer spectroscopy with a high velocity resolution were briefly reviewed. Examples of obtained Mössbauer spectra of meteorites and their fitting were considered and demonstrated advantages of this technique for revealing spectral components related to various iron-bearing phases that could not be observed in the spectra recorded by conventional Mössbauer spectroscopy. It was shown that the obtained results can be used for the phase identification, phase analysis, estimation of variations in the local microenvironment and parameters of 57Fe hyperfine interactions, determination of cation ordering in silicate crystals, and calculation of the temperatures of equilibrium cation distribution as well as for the systematization of ordinary chondrites.

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Journal
Geochemistry International
Published
2025-10-01
DOI
https://doi.org/10.1134/s0016702925600439
Primary Topic
Astro and Planetary Science
Type
article
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article

Mössbauer Spectroscopy with a High Velocity Resolution Applied to the Study of Iron-Bearing Phases in Meteorites

E. V. Petrova, M. V. Goryunov, М. И. Оштрах, A. A. Maksimova
Geochemistry International
Astro and Planetary Science
article

Mössbauer Spectroscopy with a High Velocity Resolution Applied to the Study of Iron-Bearing Phases in Meteorites

E. V. Petrova, M. V. Goryunov, М. И. Оштрах, A. A. Maksimova
article en

Abstract

The results of our studies of iron-bearing phases in various meteorites using Mössbauer spectroscopy with a high velocity resolution were briefly reviewed. Examples of obtained Mössbauer spectra of meteorites and their fitting were considered and demonstrated advantages of this technique for revealing spectral components related to various iron-bearing phases that could not be observed in the spectra recorded by conventional Mössbauer spectroscopy. It was shown that the obtained results can be used for the phase identification, phase analysis, estimation of variations in the local microenvironment and parameters of 57Fe hyperfine interactions, determination of cation ordering in silicate crystals, and calculation of the temperatures of equilibrium cation distribution as well as for the systematization of ordinary chondrites.

Geochemistry InternationalVol. 63(10)
Ural Federal University (RU), University of South Carolina (US)
Openalex Percentile: Top 77%
Astro and Planetary Science
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