An experimental determination of the effect of pressure on the Fe 3+ /ΣFe ratio of an anhydrous silicate melt to 3.0 GPa
The effect of pressure on the Fe3+/∑Fe ratio of an anhydrous andesitic melt was determined from 0.4 to 3.0 GPa at 1400 °C with oxygen fugacity controlled internally by the Ru + RuO2 buffer. Values of Fe3+/∑Fe were determined by Mössbauer spectroscop
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