Can Core Formation in Planetesimals Fractionate Iron Isotopes? Clues from a Study of Metal-Silicate Assemblages in Disko Basalt, Greenland

Details Can Core Formation in Planetesimals Fractionate Iron Isotopes? Clues from a Study of Metal-Silicate Assemblages in Disko Basalt, Greenland Can Core Formation in Planetesimals Fractionate Iron Isotopes? Clues from a Study of Metal-Silicate Assemblages in Disko Basalt, Greenland

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1467s&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1467

Computer Science

Scientific paper

Iron isotopes are found to be fractionated in terrestrial metal-silicate
assemblages in Disko basalts. Measurements are compared to theoretical
predictions of Polyakov and Mineev (2000). Discussions involved kinetic
and equilibrium fractionation.

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