Redox state of early magmas

Bruno Scaillet () and Fabrice Gaillard ()
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Bruno Scaillet: Bruno Scaillet and Fabrice Gaillard are at the CNRS/INSU-Université d'Orléans, ISTO, UMR 6113, 1a rue de la Férollerie, 45071 Orléans, France.
Fabrice Gaillard: Bruno Scaillet and Fabrice Gaillard are at the CNRS/INSU-Université d'Orléans, ISTO, UMR 6113, 1a rue de la Férollerie, 45071 Orléans, France.

Nature, 2011, vol. 480, issue 7375, 48-49

Abstract: A study of cerium in zircon minerals has allowed an assessment of the redox conditions that prevailed when Earth's earliest magmas formed. The results suggest that the mantle became oxidized sooner than had been thought. See Letter p.79

Date: 2011
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DOI: 10.1038/480048a

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