Is Silicon a Light Component in the Earth's Core? - Constraints from Liquid Metal-Liquid Silicate Partitioning of Some Lithophile Elements

Details Is Silicon a Light Component in the Earth's Core? - Constraints from Liquid Metal-Liquid Silicate Partitioning of Some Lithophile Elements Is Silicon a Light Component in the Earth's Core? - Constraints from Liquid Metal-Liquid Silicate Partitioning of Some Lithophile Elements

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1161m&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1161

Physics

Scientific paper

Metal-silicate partitioning of the lithophile elements Ta, Ga, In and Zn
at 6-20 GPa and 2100°-2400°C show that they become more
siderophile than Si at low oxygen fugacities. Si is therefore unlikely
to be a major light element in the Earth's core.

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