W Partitioning Between Liquid Metal and Liquid Silicate as a Function of P, T, fO2, Xcarbon, and Melt Structure: Implications for the Earth, Moon, Mars, and Vesta

Details W Partitioning Between Liquid Metal and Liquid Silicate as a Function of P, T, fO2, Xcarbon, and Melt Structure: Implications for the Earth, Moon, Mars, and Vesta W Partitioning Between Liquid Metal and Liquid Silicate as a Function of P, T, fO2, Xcarbon, and Melt Structure: Implications for the Earth, Moon, Mars, and Vesta

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.2238c&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Physics

2

Scientific paper

We present 103W partitioning experiments between liquid metal
and liquid silicate as a function of P, T, fO2,
Xcarbon, and silicate melt structure from 1723-2673 K and
0.5-18 GPa.

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