Effects of geodynamic setting on the redox state of fluids released by subducted mantle lithosphere

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Effects of geodynamic setting on the redox state of fluids released by subducted mantle lithosphere

Magnetite breakdown during subduction of serpentinised ultramafic rocks may produce oxidised fluids that oxidise the deep Earth and/or the sub-arc mantle, either via direct transport of ferric iron, or via redox reactions between ferric iron and other elements, such as sulfur. However, so far, there...

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Bibliographic Details
Main Authors:	Evans, Katy, Reddy, Steven, Tomkins, A., Crossley, Rosalind, Frost, B.
Format:	Journal Article
Published:	Elsevier BV 2017
Online Access:	http://hdl.handle.net/20.500.11937/50424

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