TY - GEN A1 - Bénard, Antoine A1 - Klimm, Kevin A1 - Woodland, Alan B. A1 - Arculus, Richard J. A1 - Wilke, Max A1 - Botcharnikov, Roman E. A1 - Shimizu, Nobumichi A1 - Nebel, Oliver A1 - Rivard, Camille A1 - Ionov, Dmitri A. T1 - Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas T2 - Postprints der Universität Potsdam Mathematisch-Naturwissenschaftliche Reihe N2 - 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. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 717 KW - Andesitic Avacha volcano KW - oxidation-state KW - oxygen fugacity KW - subduction zones KW - peridotite xenoliths KW - sulfur speciation KW - redox state KW - island-arc KW - dissolution mechanism KW - basaltic systems Y1 - 2019 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-426184 SN - 1866-8372 IS - 717 ER -