Oxygen controls on magmatism in rocky exoplanets.

ABSTRACT: Refractory oxygen bound to cations is a key component of the interior of rocky exoplanets. Its abundance controls planetary properties including metallic core fraction, core composition, and mantle and crust mineralogy. Interior oxygen abundance, quantified with the oxygen fugacity (fO₂), also determines the speciation of volatile species during planetary outgassing, affecting the composition of the atmosphere. Although melting drives planetary differentiation into core, mantle, crust, and atmosphere, the effect of fO₂ on rock melting has not been studied directly to date, with prior efforts focusing on fO₂-induced changes in the valence ratio of transition metals (particularly iron) in minerals and magma. Here, melting experiments were

SUBMITTER: Lin Y 

PROVIDER: S-EPMC8609297 | biostudies-literature | 2021 Nov

REPOSITORIES: biostudies-literature