Carbon-fluid equilibria and the oxidation state of the upper mantle

Carbon-fluid equilibria and the oxidation state of the upper mantle

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IT has been proposed that the oxidation state of the Earth's upper mantle is buffered by C-O fluids in equilibrium with elemental carbon1,2. A large body of data on the oxygen fugacities (fo2) recorded by mantle rocks and their derivative melts now allows us to test this proposal. By comparing...

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Bibliographische Detailangaben
Hauptverfasser:	Blundy, J, Brodholt, J, Wood, B
Format:	Journal article
Sprache:	English
Veröffentlicht:	1991

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