Valence State Partitioning of Cr and V Between Pyroxene-Melt: Estimates of Oxygen Fugacity for Martian Basalt QUE 94201

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Based on DCr and DV between pigeonite cores and bulk composition, we
estimate QUE 94201 crystallized at an fO2 between IW+0.2 and IW+0.9,
with DCr/DV suggesting IW+0.6.

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