“…Numerous studies have suggested that the high-MgO anhydrous or slightly hydrous tholeiite HAB can be generated by some extents of crystal fractionation from primary magma with higher Mg# at high pressure (5-10 kbar) near the arc crust-mantle boundary (Bartels et al, 1991;Falloon and Green, 1987;Fujii and Scarfe, 1985;Green et al, 1967;Gust and Perfit, 1987). This contrasts with the low crystallization pressure (1-2 kbar) and high water content (2-4 wt%) proposed for low-MgO calc-alkaline HAB (Sisson and Grove, 1993a).…”