The Isotope Geochemistry of Nickel in Chondrites and Iron Meteorites

Details The Isotope Geochemistry of Nickel in Chondrites and Iron Meteorites The Isotope Geochemistry of Nickel in Chondrites and Iron Meteorites

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1286m&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1286

Physics

2

Scientific paper

Ni in ordinary chondrites becomes isotopically heavier in the order LL,
L, H. This trend reflects mass-dependent fractionation during
vaporisation. No strong ^60Ni anomaly is detected. Segregation of the
Earth's core started after the decay of ^60Fe.

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