Conditions of Core Formation in the Early Earth: Single Stage or Heterogeneous Accretion?

Physics

Scientific paper

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Scientific paper

Combination of new and literature data for metal-silicate partition
coefficients for siderophile elements (Ni, Co, Mo, W, P, Ga, Cu, Mn, V,
Cr, Pd) show that Earth's mantle equilibrated with core forming Fe metal
at 32-42 GPa and 2500-2700 K.

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