The Iron Isotopic Composition of the Silicate Earth: Clues from Chondrites, Peridotites, and Eoarchean Magmas

Details The Iron Isotopic Composition of the Silicate Earth: Clues from Chondrites, Peridotites, and Eoarchean Magmas The Iron Isotopic Composition of the Silicate Earth: Clues from Chondrites, Peridotites, and Eoarchean Magmas

Mar 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009lpi....40.1769d&link_type=abstract

40th Lunar and Planetary Science Conference, (Lunar and Planetary Science XL), held March 23-27, 2009 in The Woodlands, Texas, i

Computer Science

Scientific paper

While phanerozoic MORBs and OIBs have fractionated iron isotopic
compositions relative to chondrites (+0.1 ‰), >3.7 Ga
terrestrial magmas seem to have near chondritic iron isotopic
compositions.

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