Oxygen Fugacity Controls on Deep-Mantle Phase Transitions in Martian Mantle Composition
Published: 15 August 2025| Version 1 | DOI: 10.17632/rxb2sf8fxc.1
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New experimental results at 1500 °C from high-pressure experiments on a Khan-based Martian mantle composition quantify the fO₂-dependence of deep-mantle phase transitions.
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Geology