Table 1 Mineral-melt partition coefficients used in partial melting and fractional crystallization calculations
From: Europium in plagioclase-hosted melt inclusions reveals mantle melting modulates oxygen fugacity
\({D}_{{{Fe}}^{3+}}\) | \({D}_{{{Fe}}^{2+}}\) | DMg | DNd | |
|---|---|---|---|---|
\({D}_{{bulk}}\) (mantle melting) | 0.1-0.3 | 1 | 3.2 | 0.03 |
Olivine (fractional crystallization) | 0 | 1 | 4 | 0 |
Clinopyroxene (fractional crystallization) | 0.2 | 0.6 | 2 | 0.1878 |
Plagioclase (fractional crystallization) | 0 | 0 | 0 | 0.065 |
