Iron Isotope Fractionation During Planetary Differentiation

Details Iron Isotope Fractionation During Planetary Differentiation Iron Isotope Fractionation During Planetary Differentiation

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.2148t&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Computer Science

Scientific paper

Iron isotopes fractionate during basaltic differentiation at both
whole-rock (~0.2) and mineral (~1.1) scales, due to the change of Fe
oxidation states. This suggests that the Fe isotopic composition of
basalts may not represent that of their sources.

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