Element Partitioning Between Magnesiowuestite and Silicate Melt as a Function of Melt Composition and Temperature at High Pressure (original) (raw)
Partitioning of elements between silicate melt and H,O-NaCI fluids at 1.5 and 2.0 GPa pressure: Implications for mantle metasomatism
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Multivariable Dependence of Fe-Mg Partitioning in the Lower Mantle
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KEGLER, PH., HOLZHEID, A., FROST, D. J., RUBIE, D.C., PALME, H. (2008): New Ni and Co metal - silicate partition coefficients at elevated pressures and temperatures call an early Earth single stage magma ocean into question. Earth and Planetary Science Letters 268, 28-40
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Partitioning of elements between high-temperature, low-density aqueous fluid and silicate melt as derived from volcanic gas geochemistry
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Fe-Mg partitioning between (Mg, Fe)SiO3post-perovskite, perovskite, and magnesiowüstite in the Earth's lower mantle
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Inter-element fractionation of highly siderophile elements in the Tonga Arc due to flux melting of a depleted source
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