Physics
Scientific paper
Dec 1991
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991metic..26..366l&link_type=abstract
Meteoritics, vol. 26, p. 366-366 (1991).
Physics
4
Scientific paper
Formation of a metal or metal-sulfide core in a planet or asteroid will cause removal of siderophile and/or chalcophile elements from the silicate mantle into the core. The absolute and relative abundances of siderophile and chalcophile elements in the residual mantle are, therefore, sensible indicators for the type and extent of core formation. To determine the involvement of sulfides during core formation, Fe-sulfide/silicate liquid partition coefficients of Mo, W. As, Sb, Co, Ga, Cu, Zn, Mn, Cr, Na, K, and Br were studied experimentally.
Lodders Katharina
Palme Herbert
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