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• W2024762148 abstract "We have equilibrated carbon-saturated FeNiCoS melts in a San-Carlos olivine matrix between 1350 and 1570°C at 2 GPa, to measure the median dihedral angles of metallic core melts in a silicate mantle matrix as a function of temperature and sulfur fugacity. The angles increase from about 68° for the most oxidized monosulfide liquid solutions (metal-sulfur ratio ∼ 0.97), to ∼ 115° for the most reduced metal-rich melts (MS ∼ 100). Temperature effects are small. These angles preclude that metallic core melts could have segregated efficiently from a crystalline silicate mantle by grain boundary percolation. We suggest that core formation must have occurred from a magma ocean." @default.
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• W2024762148 date "1996-09-01" @default.
• W2024762148 modified "2023-10-17" @default.
• W2024762148 title "Mobility of core melts during Earth's accretion" @default.
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• W2024762148 doi "https://doi.org/10.1016/0012-821x(96)00135-5" @default.
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