Figure 1
From: Water-melt interaction in hydrous magmatic systems at high temperature and pressure
Pressure/temperature trajectories. (A) Granite with and without H2O (granite-H2O and anhydrous granite) and peridotite with and without H2O (peridotite-H2O and anhydrous peridotite) solidi (Stern et al. 1975; Kushiro et al. 1968a ) and (B) silica polymorphs and enstatite with and without H2O (cristobalite-H2O, enstatite-H2O, anhydrous cristobalite, and anhydrous enstatite) (Boyd et al. 1964; Kushiro et al. 1968a; Jackson 1976; Boettcher 1984).