Effect of Pressure on the Partitioning of Highly Siderophile Elements Between Liquid Fe-Alloy and Peridotitic Liquid

Physics

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Scientific paper

This study evaluates metal-silicate equilibration in a magma ocean as a
possible explanation for the HSE inventory of the Earth's mantle.
Experimental results indicate that pressure decreases the siderophile
character of the HSE's Ru, Rh, Pd, Pt and Re.

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