Iron isotope differences between Earth, Moon, Mars and Vesta as possible records of contrasted accretion mechanisms

By F. Poitrasson, A. Halliday, Der-Chuen Lee, S. Levasseur, N. Teutsch. 2004

308 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Ecology

View Paper: https://www.semanticscholar.org/paper/522362cff4e1ccb8a4c8752f9df5b069988d08bc

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Citations in the corpus

Planetary and meteoritic Mg/Si and δ30Si variations inherited from solar nebula chemistry (2015, background): “Large impacts were also invoked to explain the Fe and Zn stable isotopic fractionations in the Earth-Moon system (Poitrasson et al., 2004; Paniello et al., 2012).”
Equilibrium Iron Isotope Fractionation Factors of Minerals: Reevaluation from the Data of Nuclear Inelastic Resonant X-ray Scattering and Mossbauer Spectroscopy (2007, unknown): “…Rouxel et al., 2003, 2004, 2005; Anbar, 2004; Beard and Johnson, 2004a,b; Croal et al., 2004; Dauphas et al., 2004, 2007; Jarzęcki et al., 2004; Poitrasson et al., 2004, 2005; Schoenberg and Von Blanckenburg, 2004, 2006; Williams et al., 2004, 2005; Anbar et al., 2005; Balci et al., 2006;…”
Abyssal peridotites reveal the near-chondritic Fe isotopic composition of the Earth (2013, background): “1% relative to chondrites and to basalts from other planetary bodies, including Mars and Vesta (Craddock and Dauphas, 2010; Poitrasson et al., 2004; Schoenberg and von Blanckenburg, 2006; Teng et al., 2013; Weyer et al., 2005; Weyer and Ionov, 2007).”
Spinel–olivine magnesium isotope thermometry in the mantle and implications for the Mg isotopic composition of Earth (2009, background): “Isotope ratios of major rock-forming elements comprising rocky planets and asteroids can be useful tracers of planet-forming processes (Poitrasson et al., 2004; Poitrasson et al., 2005; Georg et al., 2007; Poitrasson, 2007; Weyer et al., 2007).”