Non-chondritic sulphur isotope composition of the terrestrial mantle

J. Labidi (), P. Cartigny and M. Moreira
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J. Labidi: Laboratoire de Géochimie des Isotopes Stables, Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRS, 1 rue Jussieu, 75005 Paris, France
P. Cartigny: Laboratoire de Géochimie des Isotopes Stables, Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRS, 1 rue Jussieu, 75005 Paris, France
M. Moreira: Laboratoire de Géochimie et Cosmochimie, Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRS, 1 rue Jussieu, 75005 Paris, France

Nature, 2013, vol. 501, issue 7466, 208-211

Abstract: Earth’s mantle is shown to display heterogeneous sulphur isotope ratios, with a depleted end-member that is not chondritic as has been thought; the mantle’s inferred composition can be accounted for by fractionation during core–mantle differentiation.

Date: 2013
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DOI: 10.1038/nature12490

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