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Magma oceans, iron and chromium redox, and the origin of comparatively oxidized planetary mantles

M. M. Hirschmann

2022Geochimica et Cosmochimica Acta59 citationsDOI

Topics & Concepts

Mineral redox bufferSilicateMantle (geology)BasaltGeologyMagmaMars Exploration ProgramFugacityPeridotiteMelt inclusionsOxygenTerrestrial planetGeochemistryMineralogyAstrobiologyChemistryVolcanoPlanetPhysical chemistryPhysicsOrganic chemistryAstrophysicsGeological and Geochemical AnalysisHigh-pressure geophysics and materialsearthquake and tectonic studies
Magma oceans, iron and chromium redox, and the origin of comparatively oxidized planetary mantles | Litcius