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- W2073456062 abstract "The partitioning of Mg and Fe between olivine and mafic-ultramafic melts has been examined based on previous and new experimental data. We find that the exchange partition coefficient, KD, changes primarily as a function of melt composition, expressed either as MgO+FeO content or degree of polymerization, NBO/T, rather than temperature or pressure. KD increases from about 0.23±0.02 at an NBO/T of ∼0 to a maximum of 0.35±0.02 at an NBO/T of ∼ 2, and then decreases to 0.23±0.02 for the pure olivine system (NBO/T=4). We suggest that the following empirical relation yields a reliable estimate of KD for mantle derived melts: KD = 0.235 + 0.120·(NBO/T) - 0.031·(NBO/T)². The change of KD shown here should be taken into account when calculating the composition of olivine coexisting with basaltic to ultramafic melts." @default.
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- W2073456062 date "1998-07-01" @default.
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- W2073456062 title "Mg-Fe partitioning between olivine and mafic-ultramafic melts" @default.
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- W2073456062 doi "https://doi.org/10.1029/98gl01844" @default.
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