Abstract
Resolution of the iron sites in the Mössbauer spectra of Ca-Fe pyroxenoids is only partial, two doublets being apparent in each case, whereas there are up to nine cation sites in each structure. Thus the inner and outer doublets represent, respectively: two sites and two sites in Ca0.5Fe0.5SiO3 (ferrobustamite); five sites and two sites in Ca0.15Fe0.85SiO3 (pyroxferroite); and five sites and four sites in FeSiO3 (ferrosolite III). Disorder of iron and calcium which exists in the two calcium-bearing pyroxenoids is not readily apparent in the spectra.
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Dowty, E., Lindsley, D.H. Mössbauer spectra of synthetic Ca-Fe pyroxenoids and lunar pyroxferroite. Contr. Mineral. and Petrol. 48, 229–232 (1974). https://doi.org/10.1007/BF00383358
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DOI: https://doi.org/10.1007/BF00383358