Comparative Planetology of the Highly Siderophile Elements: Implications for the Accretion of the Terrestrial Planets

Details Comparative Planetology of the Highly Siderophile Elements: Implications for the Accretion of the Terrestrial Planets Comparative Planetology of the Highly Siderophile Elements: Implications for the Accretion of the Terrestrial Planets

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1194j&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1194

Physics

1

Scientific paper

Of the highly siderophile elements, Pt fractionates least during igneous
processess. Currently, Pt abundances in the Earth, Moon, and Mars are
indistinguishable. This constancy casts doubt on the late veneer model
of planetary accretion.

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