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, 2, 2, 5} Frédéric Moynier ^{1, 2, 5}

1 Department of Earth and Planetary Sciences [St Louis]

2 WUSTL - Washington University in Saint Louis

3 ‎ Harvard Univ, Dept Earth & Planetary Sci, Cambridge

4 University of St Andrews [Scotland]

5 IPGP - Institut de Physique du Globe de Paris

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

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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 : Thursday, April 7, 2022 - 1:58:31 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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