Nature Communications (Aug 2018)
Oxidising agents in sub-arc mantle melts link slab devolatilisation and arc magmas
Abstract
The oxidised nature of arc magmas is either attributed to recycling from the slab or magma differentiation. Here, the authors show that oxidised iron and sulfur, respectively in sub-arc mantle spinel and glass inclusions with elevated U/Th, Pb/Ce, Sr/Nd and δ34S, trace dehydration products of slab serpentinites.