Redox Melting of Garnet Lherzolite: Generation of Carbonated Silicate and Sulfide Melts and Implications for OIB Formation From Chalcophile and Redox‐Sensitive Elements
Abstract Upwellings in the Earth's mantle become sufficiently oxidizing for CO2‐induced redox melting at depths equivalent to ∼8–5 GPa, generating deep incipient mantle melts. This study simulates the geochemistry of the redox melting process by conducting multi‐anvil experiments at 5 GPa and s...
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| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Wiley
2025-03-01
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| Series: | Geochemistry, Geophysics, Geosystems |
| Subjects: | |
| Online Access: | https://doi.org/10.1029/2024GC012025 |
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