Mantle oxidation state and its relationship to tectonic environment and fluid speciation.

The earth's mantle is degassed along mid-ocean ridges, while rehydration and possibly recarbonaton occurs at subduction zones. These processes and the speciation of C-H-O fluids in the mantle are related to the oxidation state of mantle peridotite. Peridotite xenoliths from continental localiti...

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Bibliographic Details
Main Authors: Wood, B, Bryndzia, LT, Johnson, K
Format: Journal article
Language:English
Published: 1990