Core Formation and the Fe/FeO Ratio of the Earth, Mars and Vesta: Constraints from the 182Hf-182W System

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Scientific paper

A dynamic core-formation model with a deep magma ocean for the Hf-W
system, which can match the partitioning of Ni, Co and W in mantles of
Earth, Mars and Vesta and yield mean age of formation of these planets
of 12, 8 and 3 Myr respectively.

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