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The Redox state of the asthenospheric mantle and the onset of melting beneath mid‐ocean ridges
The redox state of the convective asthenospheric mantle governs the speciation of volatile
elements such as carbon and, therefore, influences the depth at which (redox) melting can …
elements such as carbon and, therefore, influences the depth at which (redox) melting can …
A predictive model for divalent element partitioning between clinopyroxene and basaltic melt and an europium-in-plagioclase-clinopyroxene oxybarometer for …
Under geologically relevant conditions, Eu is a multivalent element, exhibiting divalent
character in reduced systems and trivalent character in oxidized systems. Its mineral-melt …
character in reduced systems and trivalent character in oxidized systems. Its mineral-melt …
PT-ƒO2-X constraints on the partitioning behavior of trace elements between clinopyroxene and alkali melts: An experimental study
Abstract Titanian Ca-clinopyroxene (Ti-Cpx) is one of the most characteristic phases and
main carriers of trace elements in alkali ultrabasic to intermediate magmas, making it a key …
main carriers of trace elements in alkali ultrabasic to intermediate magmas, making it a key …