The iron isotope composition of enstatite meteorites: Implications for their origin and the metal/sulfide Fe isotopic fractionation factor

Kun Wang; Paul Savage; Frédéric Moynier

doi:10.1016/j.gca.2014.07.019

Journal articles

The iron isotope composition of enstatite meteorites: Implications for their origin and the metal/sulfide Fe isotopic fractionation factor

Kun Wang ^{1, 2, 3} Paul Savage ^{4, 5, 2, 6} Frédéric Moynier ^{1, 7, 6}

1 Department of Earth and Planetary Sciences [St Louis]

2 Washington Univ, McDonnell Ctr Space Sci, St Louis, MO 63130 USA

3 ‎ Harvard Univ, Dept Earth & Planetary Sci, Cambridge

4 University of St Andrews [Scotland]

5 Washington Univ, Dept Earth & Planetary Sci, St Louis, MO 63130 USA

6 IPGP - Institut de Physique du Globe de Paris

7 Washington Univ, McDonnell Ctr Space Sci, One Brookings Dr, St Louis, MO 63130 USA

Keywords : SHOCK METAMORPHISM IGNEOUS SYSTEMS EL CHONDRITES EARTHS MANTLE METAL HETEROGENEITY EVAPORATION KeyWords Plus:SULFIDES CONSTRAINTS CHEMICAL-COMPOSITION LITHOSPHERIC MANTLE

Document type :

Journal articles

Domain :

Sciences of the Universe [physics]

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https://hal-insu.archives-ouvertes.fr/insu-02917650
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Submitted on : Wednesday, August 19, 2020 - 3:55:50 PM
Last modification on : Wednesday, October 27, 2021 - 4:03:24 PM

The iron isotope composition of enstatite meteorites: Implications for their origin and the metal/sulfide Fe isotopic fractionation factor

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The iron isotope composition of enstatite meteorites: Implications for their origin and the metal/sulfide Fe isotopic fractionation factor

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