Mössbauer and X-ray studies of an iron meteorite sample

Physics

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Scientific paper

Detailed analysis of the room temperature Mössbauer spectrum of an Fe-Ni (≈ 91.9% Fe, 7.5% Ni) meteorite from the Henbury crater region of northern Australia shows that it behaves identically to an Fe-Ni alloy. The enhanced resonance absorption is due to thickness effects, with the line broadening reflecting a range of atomic environments. The isotope ratio56Fe/57Fe for the meteorite agrees with the earth bound values.

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