Abstract: High Pressure Phase Relations of a Depleted Peridotite Fluxed by a CO<sub>2</sub>‐H<sub>2</sub>O bearing fluid and Stability of Partial Melts in the Cratonic Mantle (AGU Fall Meeting 2018)

High Pressure Phase Relations of a Depleted Peridotite Fluxed by a CO₂‐H₂O bearing fluid and Stability of Partial Melts in the Cratonic Mantle

Sriparna Saha, Rice University, Department of Earth, Environmental and Planetary Sciences, Houston, TX, United States and Rajdeep Dasgupta, Rice University, Department of Earth, Environmental and Planetary Sciences, Houston, United States

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High Pressure Phase Relations of a Depleted Peridotite Fluxed by a CO2‐H2O bearing fluid and Stability of Partial Melts in the Cratonic Mantle

High Pressure Phase Relations of a Depleted Peridotite Fluxed by a CO₂‐H₂O bearing fluid and Stability of Partial Melts in the Cratonic Mantle