Ni Partitioning in the Terrestrial Magma Ocean: A Polybaric Numerical Model

Details Ni Partitioning in the Terrestrial Magma Ocean: A Polybaric Numerical Model Ni Partitioning in the Terrestrial Magma Ocean: A Polybaric Numerical Model

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1593m&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

2

Scientific paper

The differentiation of iron metal from molten silicate in the early
earth is studied with a novel numerical technique. We find that the Ni
abundance in the magma ocean is controlled by partition at high pressure
and temperature.

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