New partitioning coefficients of first-transition row elements, Ga and Ge between olivine and silicate melt have been reported. New high-temperature experiments have investigated the effects of oxygen ...
Olivine is the earliest mineral to crystallize from basaltic magma, and accurate knowledge of olivine/melt partition coefficients (D Ol-melt) for first-transition row elements (FTREs) Ga and Ge, is ...
Some results have been hidden because they may be inaccessible to you
Show inaccessible results