Redox Freezing and Melting during Peridotite Interaction with Carbonated Metasediments and Metabasics: Experiments at 10 GPa

— The hypothesis of redox freezing is based on the assumption that a Fe–Ni metal phase becomes stable in the peridotite mantle at increasing pressure and can serve as a reducer for carbonate–silicate melts. reduction and formation of elementary C (graphite or diamond) result in an increase in the so...

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