Controls on Iron Isotope Variations in Planetary Magmas

Details Controls on Iron Isotope Variations in Planetary Magmas Controls on Iron Isotope Variations in Planetary Magmas

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1525d&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1525

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Using a synchrotron technique, we have measured the equilibrium
Fe-isotope fractionation factors of geological materials. This study
reveals the potency of Fe isotopes to trace redox variations and
magmatic differentiation in planets.

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