The redox state of subduction zones: insights from arc-peridotites.
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Parkinson, I J
Arculus, Richard
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Elsevier
Abstract
Spinel peridotites from a variety of island arcs have been utilised to calculate the redox state of the mantle wedge above subduction zones. Oxygen fugacities (f(O)2 values) calculated from the ferric iron content of spinels, measured by Electron Micropro
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Chemical Geology
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Restricted until
2037-12-31