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...
| Main Authors: | , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
1990
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