Implications for Core Formation of the Earth from High Pressure-Temperature Au Partitioning Experiments

Details Implications for Core Formation of the Earth from High Pressure-Temperature Au Partitioning Experiments Implications for Core Formation of the Earth from High Pressure-Temperature Au Partitioning Experiments

Mar 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005lpi....36.1955d&link_type=abstract

36th Annual Lunar and Planetary Science Conference, March 14-18, 2005, in League City, Texas, abstract no.1955

Physics

4

Scientific paper

The results of high P-T Au partitioning experiments and multi-variable
modeling are consistent with the equilibrium core formation hypothesis.
Metal-silicate equilibrium could have occurred in a magma ocean at
pressures of 27 GPa and 2127 °C.

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