Determining the Metal/Silicate Partition Coefficient of Germanium: Implications for Core and Mantle Differentiation

Details Determining the Metal/Silicate Partition Coefficient of Germanium: Implications for Core and Mantle Differentiation Determining the Metal/Silicate Partition Coefficient of Germanium: Implications for Core and Mantle Differentiation

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1257k&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1257

Physics

1

Scientific paper

Ge is a moderately siderophile element that was studied systematically
at high temperatures using a piston cylinder apparatus. Evidence
observed finds extremely high T is not necessary, therefore suggesting a
shallow ocean.

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