Fe3+/ΣFe ratios were determined from Mössbauer spectra recorded for a series of 17 anorthite-diopside eutectic glasses containing 1 wt% 57Fe2O3 quenched from melts equilibrated over a range of oxygen fugacities from fO2 ∼ 105 bars (Fe3+/ΣFe = 1) to 1
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Jayasuriya et al. (2004) studied this question.
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