Figure 8From: Water-melt interaction in hydrous magmatic systems at high temperature and pressure Solubility of silica (SiO 2 ) in fluid. Coexisting with enstatite + forsterite (0.49 to 1.7 GPa pressure, closed symbols) and with enstatite (3.6 GPa pressure, closed symbols) in MgO-SiO2-H2O fluid calculated with the algorithm of Newton and Manning (2002) (results from Mysen et al. 2013).Back to article page