Si isotope systematics of meteorites and terrestrial peridotites: implications for Mg/Si fractionation in the solar nebula and for Si in the Earth's core

By C. Fitoussi, B. Bourdon, T. Kleine, F. Oberli, B. Reynolds. 2009

172 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science, Geophysics

View Paper: https://www.semanticscholar.org/paper/3bd2c64b4dd56c6d656471d2c8baad00730cd65a

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In Astronomy and Astrophysics

1. C. Burkhardt
2. H. Kobayashi
3. N. Dauphas

In Atmospheric Science

1. N. Dauphas
2. C. Burkhardt

In Geophysics

1. N. Dauphas
2. C. Burkhardt

Citations in the corpus

• Planetary and meteoritic Mg/Si and δ30Si variations inherited from solar nebula chemistry (2015, background): “However, basalts have δ(30)Si values indistinguishable from mantle peridotites, suggesting that basalts are representative of their mantle source (Fitoussi et al., 2009; Savage et al., 2010; Savage et al., 2011; Armytage et al., 2011; Zambardi and Poitrasson, 2011; Savage and Moynier, 2013; Zambardi”