Abstract
Single crystal samples of natural olivine, Mg1.82Fe0.17Ni0.01SiO4, have been oxidized in air at temperatures of 600 and 800°C, respectively, and studied by conversion electron and transmission Mössbauer spectroscopy. Oxidation of olivine was found to result in ferriolivine and spinel ferrite formation; the corresponding kinetic data also were discussed.
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Meyer, M., Rüffler, R. Conversion Electron Mössbauer Spectroscopic Study of Subsolidus Oxidation of Olivine. Hyperfine Interactions 141, 351–355 (2002). https://doi.org/10.1023/A:1021228119983
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DOI: https://doi.org/10.1023/A:1021228119983