Processes and conditions of the origin for Fe3+-bearing magnesiowüstite under lithospheric mantle pressures and temperatures

Processes and conditions of the origin for Fe³⁺-bearing magnesiowüstite under lithospheric mantle pressures and temperatures

Research output: Contribution to journal › Article › peer-review

Diamond, Experimental modeling, Fe-bearing magnesiowüstite, Graphite, High-pressure experiment, Lithospheric mantle, Mantle oxides, Redox reactions, MAGNESIUM-OXIDE, lithospheric mantle, high-pressure experiment, STABILITY, mantle oxides, DEEP MANTLE, graphite, DIAMOND FORMATION, redox reactions, PHASE-TRANSFORMATIONS, experimental modeling, CARBON, Fe3+-bearing magnesiowustite, FERROPERICLASE, MINERAL INCLUSIONS, diamond, EQUATION-OF-STATE, FERRIC IRON CONTENT

ID: 21257100