The effect of CO2 on the water-saturated solidus of K-poor peridotite between 4 and 6Â GPa

The H2O-CO2-bearing fluids found in this study at 900-1000 °C are similar in composition to low-Mg carbonatitic to silicic high-density fluids found in fluid inclusions in diamonds. With increasing temperature, the melts approach type II kimberlites. We propose that H2O-CO2-induced partial melting of metasomatized garnet lherzolite at 4-6 GPa is a possible origin for group II kimberlites.