Figure 7. Variation curves for the distribution of mineral equilibrium temperatures of xenoliths in the Pamir fergusite. (A) Main types of nodules: (1) phlogopite-garnet websterite, (2) garnet clinopyroxenite, (3) eclogite, (4) garnet-orthopyroxene granulite; (B) eclogite types: (5) sanidine, (6) biotite, (7) bimineral, and (8) plagioclase eclogites. N denotes the number of T calculations.