Experimental investigations have been conducted on the partition coefficients of first-transition row elements between olivine and silicate melt. Olivine is the first mineral to crystallize from basaltic magma, and accurate knowledge of olivine/melt partition coefficients (DOl–melt) for first-transition row elements (FTREs) Ga and Ge, is required in quantitative modeling of petrogenetic processes in planetary basalts. […]
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