(Table 4) Pyroxene compositions for temperature calculations of granulite grade metamorphism associated with ductile deformation of ODP Hole 118-735B

Pyroxene formulas were calculated using the formulas of Papike et al. (1974) and a program provided by P. Meyer. Analyses pairs are recrystallized grains that were in contact, apparently in equilibrium. Equilibrium temperatures calculated using Wells (1977) are as follows: For analyses pair 1 and 3, T = 894°C; for analyses pair 2 and 4, T = 908°C; for analyses pair 5 and 7, T = 852°C; for analyses pair 6 and 8, T = 849°C.