Diffusion-driven Kinetic Isotope Fractionation of Fe and Ni in Iron Meteorites: A New Dimension to the Analysis of Cooling Rates

Details Diffusion-driven Kinetic Isotope Fractionation of Fe and Ni in Iron Meteorites: A New Dimension to the Analysis of Cooling Rates Diffusion-driven Kinetic Isotope Fractionation of Fe and Ni in Iron Meteorites: A New Dimension to the Analysis of Cooling Rates

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1178d&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

Scientific paper

Iron meteorites show Fe and Ni isotopic fractionation between taenite
and kamacite. This can be explained by diffusion-driven kinetic isotope
fractionation during phase growth.

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