Separate zones of sulfate and sulfide release from subducted mafic oceanic crust

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Separate zones of sulfate and sulfide release from subducted mafic oceanic crust

Liberation of fluids during subduction of oceanic crust is thought to transfer sulfur into the overlying sub-arc mantle. However, despite the importance of sulfur cycling through magmatic arcs to climate change, magma oxidation and ore formation, there has been little investigation of the metamorphi...

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Bibliographic Details
Main Authors:	Tomkins, A., Evans, Katy
Format:	Journal Article
Published:	Elsevier 2015
Online Access:	http://hdl.handle.net/20.500.11937/35076

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