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The supporting information for "A new oxybarometer for basalts based on olivine-melt Mn-Fe2+ exchange coefficient and FeT/Mn ratios in olivine and melt"

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Mendeley Data2026-04-09 收录
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olivine-melt Mn-Fe2+ exchange coefficient is constant in basaltic magma system, which can be developed into a simple back calculation method for melt Fe3+/FeT.

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