Origin of K-rich diamond-forming immiscible melts and CO2 fluid via partial melting of carbonated pelites at a depth of 180

Carbonate-silicate liquid immiscibility, Diamond formation, Earth's mantle, High-density fluids, High-pressure experiment

ID: 23288780

Origin of K-rich diamond-forming immiscible melts and CO2 fluid via partial melting of carbonated pelites at a depth of 180–200 km