Significance of iron isotope mineral fractionation in pallasites and iron meteorites for the core-mantle differentiation of terrestrial planets

Earth and Planetary Science Letters

Volumn 234, Issue 1-2, 2005, Pages 151-164

  Poitrasson, Franck ^a,b   Levasseur, Sylvain ^b   Teutsch, Nadya ^b,c  

^a CNRS   (France)

^b ETH ZURICH   (Switzerland)

^c SWISS FEDERAL INSTITUTE OF AQUATIC SCIENCE AND TECHNOLOGY   (Switzerland)

Author keywords

Chondrites; Core mantle differentiation; Fe isotopes; Iron meteorites; Pallasites; Protoplanetary accretion disk

Indexed keywords

CORE-MANTLE INTERFACES; IRON ISOTOPES; IRON METEORITES; PALLASITES;

COMPOSITION; COORDINATION REACTIONS; INTERFACES (MATERIALS); IRON; ISOTOPES; MINERALS;

PLANETS;

CORE (PLANETARY); IRON; IRON METEORITE; ISOTOPIC FRACTIONATION; MANTLE; PLANETARY EVOLUTION;

ASTEROIDEA; CICONIIFORMES; TOLUCA;

EID: 18444417996     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2005.02.010     Document Type: Article

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