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"

Published: 11 January 2022| Version 1 | DOI: 10.17632/r2v2mv6n8n.1
Contributor:
zhongxing sun

Description

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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Institutions

Chinese Academy of Sciences, Guangzhou Institute of Geochemistry

Categories

Experimental Geochemistry

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