Fig. 5From: Fluids and physicochemical properties and processes in the EarthModified from Botcharnikov et al. (2015) and Beermann et al. (2015)Fluid/melt partition coefficient of Cl A. as a function of pressure for two different magma compositions as indicated. B. As a function of Cl concentration in andesitic melt at two different temperatures as indicated, and C. as a function of SiO2 concentration in melt. Back to article page