Litcius/Paper detail

Partitioning of Fe2+ and Fe3+ between bridgmanite and silicate melt: Implications for redox evolution of the Earth's mantle

H. Kuwahara, Ryoichi Nakada

2023Earth and Planetary Science Letters13 citationsDOI

Topics & Concepts

Silicate perovskiteMantle (geology)GeologySilicateTransition zonePlanetary differentiationGeochemistryPost-perovskiteMantle plumeMantle convectionSubductionLithosphereChemistryPaleontologyOrganic chemistryTectonicsGeological and Geochemical AnalysisHigh-pressure geophysics and materialsearthquake and tectonic studies
Partitioning of Fe2+ and Fe3+ between bridgmanite and silicate melt: Implications for redox evolution of the Earth's mantle | Litcius