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Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas

Author

Listed:
  • Antoine Bénard

    (The Australian National University
    Monash University
    Institute of Earth Sciences, Géopolis)

  • Kevin Klimm

    (Goethe Universität Frankfurt)

  • Alan B. Woodland

    (Goethe Universität Frankfurt)

  • Richard J. Arculus

    (The Australian National University)

  • Max Wilke

    (Universität Potsdam)

  • Roman E. Botcharnikov

    (Leibniz Universität Hannover
    Gutenberg Universität Mainz)

  • Nobumichi Shimizu

    (Woods Hole Oceanographic Institution)

  • Oliver Nebel

    (Monash University)

  • Camille Rivard

    (European Synchrotron Radiation Facility)

  • Dmitri A. Ionov

    (Université de Montpellier and UMR-CNRS 5243)

Abstract

Subduction zone magmas are more oxidised on eruption than those at mid-ocean ridges. This is attributed either to oxidising components, derived from subducted lithosphere (slab) and added to the mantle wedge, or to oxidation processes occurring during magma ascent via differentiation. Here we provide direct evidence for contributions of oxidising slab agents to melts trapped in the sub-arc mantle. Measurements of sulfur (S) valence state in sub-arc mantle peridotites identify sulfate, both as crystalline anhydrite (CaSO4) and dissolved SO42− in spinel-hosted glass (formerly melt) inclusions. Copper-rich sulfide precipitates in the inclusions and increased Fe3+/∑Fe in spinel record a S6+–Fe2+ redox coupling during melt percolation through the sub-arc mantle. Sulfate-rich glass inclusions exhibit high U/Th, Pb/Ce, Sr/Nd and δ34S (+ 7 to + 11‰), indicating the involvement of dehydration products of serpentinised slab rocks in their parental melt sources. These observations provide a link between liberated slab components and oxidised arc magmas.

Suggested Citation

  • Antoine Bénard & Kevin Klimm & Alan B. Woodland & Richard J. Arculus & Max Wilke & Roman E. Botcharnikov & Nobumichi Shimizu & Oliver Nebel & Camille Rivard & Dmitri A. Ionov, 2018. "Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas," Nature Communications, Nature, vol. 9(1), pages 1-10, December.
  • Handle: RePEc:nat:natcom:v:9:y:2018:i:1:d:10.1038_s41467-018-05804-2
    DOI: 10.1038/s41467-018-05804-2
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    Cited by:

    1. Carter Grondahl & Zoltán Zajacz, 2022. "Sulfur and chlorine budgets control the ore fertility of arc magmas," Nature Communications, Nature, vol. 13(1), pages 1-11, December.

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