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*Subject description:* The evolution of redox conditions in subduction zones is a major challenge for understanding the exchanges of matter "magma-crust-mantle". Fluids released from the subducting oceanic crust recycle lithophile elements back into the mantle wedge, facilitate melting of peridotites, and lead to prolific subduction-zone arc volcanism. According to their chemical properties (e.g. oxygen fugacity) these fluids are the main vehicle for understanding the mechanisms of partial melti...
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