Ordinary chondrites: What can we learn using Mössbauer spectroscopy?

Iron-bearing phases in ordinary chondrites are the subject of numerous studies by Mössbauer spectroscopy. This review considers useful information which can be obtained by means of this technique. Mössbauer spectroscopy permits to analyze the iron-bearing phase composition in meteorites and to do ro...

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Published inJournal of molecular structure Vol. 1186; pp. 104 - 117
Main Authors Maksimova, A.A., Oshtrakh, M.I.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 15.06.2019
Subjects
57Fe hyperfine parameters
Iron-bearing phases
Mössbauer spectroscopy
Ordinary chondrites
Ordinary chondrites
57Fe hyperfine parameters
Mössbauer spectroscopy
Iron-bearing phases
Online AccessGet full text
ISSN0022-2860
1872-8014
DOI10.1016/j.molstruc.2019.02.024

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Abstract Iron-bearing phases in ordinary chondrites are the subject of numerous studies by Mössbauer spectroscopy. This review considers useful information which can be obtained by means of this technique. Mössbauer spectroscopy permits to analyze the iron-bearing phase composition in meteorites and to do roughly the modal analysis; to investigate weathering products formation and estimate terrestrial age of meteorites; to evaluate the hyperfine parameters for the iron-bearing phases and compare variations in the local microenvironment of iron in the same iron-bearing crystals in different meteorites; to analyze the Fe2+ distribution between the M1 and M2 sites in silicate crystals and to estimate temperature of equilibrium cation distribution in olivine and orthopyroxene in bulk meteorite samples; to carry out classification of H, L and LL ordinary chondrites using Mössbauer parameters. Comparison of various results demonstrates advances of Mössbauer spectroscopy with a high velocity resolution in the study of ordinary chondrites in comparison with conventional technique. •Mössbauer spectroscopy can analyze the iron-bearing phase composition in ordinary chondrites.•Mössbauer spectroscopy helps to analyze the Fe2+ occupations of the M1 and M2 sites in silicates.•Mössbauer spectroscopy helps to estimate Teq of cation distribution in olivine and orthopyroxene.
AbstractList Iron-bearing phases in ordinary chondrites are the subject of numerous studies by Mössbauer spectroscopy. This review considers useful information which can be obtained by means of this technique. Mössbauer spectroscopy permits to analyze the iron-bearing phase composition in meteorites and to do roughly the modal analysis; to investigate weathering products formation and estimate terrestrial age of meteorites; to evaluate the hyperfine parameters for the iron-bearing phases and compare variations in the local microenvironment of iron in the same iron-bearing crystals in different meteorites; to analyze the Fe2+ distribution between the M1 and M2 sites in silicate crystals and to estimate temperature of equilibrium cation distribution in olivine and orthopyroxene in bulk meteorite samples; to carry out classification of H, L and LL ordinary chondrites using Mössbauer parameters. Comparison of various results demonstrates advances of Mössbauer spectroscopy with a high velocity resolution in the study of ordinary chondrites in comparison with conventional technique. •Mössbauer spectroscopy can analyze the iron-bearing phase composition in ordinary chondrites.•Mössbauer spectroscopy helps to analyze the Fe2+ occupations of the M1 and M2 sites in silicates.•Mössbauer spectroscopy helps to estimate Teq of cation distribution in olivine and orthopyroxene.
Author Maksimova, A.A.
Oshtrakh, M.I.
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Keywords Ordinary chondrites
57Fe hyperfine parameters
Mössbauer spectroscopy
Iron-bearing phases
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Snippet Iron-bearing phases in ordinary chondrites are the subject of numerous studies by Mössbauer spectroscopy. This review considers useful information which can be...
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StartPage 104
SubjectTerms 57Fe hyperfine parameters
Iron-bearing phases
Mössbauer spectroscopy
Ordinary chondrites
Title Ordinary chondrites: What can we learn using Mössbauer spectroscopy?
URI https://dx.doi.org/10.1016/j.molstruc.2019.02.024
Volume 1186
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