The Effects of Oxygen, Sulphur and Silicon on the Dihedral Angles Between Fe-rich Liquid Metal and Olivine, Ringwoodite and Silicate Perovskite: Implications for Planetary Core Formation

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Scientific paper

The effects of dissolved O, S, and Si on percolative core formation on
Earth and Mars have been studied experimentally. Complete metal-silicate
separation by percolation was not possible on either planet, indicating
the necessity of a magma ocean.

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