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paths The idealized check out of P-T paths is the fact that mineral assemblages equilibrate at every phase of The trail from your onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This check out ignores kinetic elements connected to the energetics of nucleation and advancement of minerals, Despite the fact that these aspects might be important for some metamorphic phases and reactions. Such as, the existence of coexisting andalusite and sillimanite (Fig. 6a) in the rock that equilibrated at P-T circumstances corresponding to the stability discipline of sillimanite illustrates that the sluggish kinetics of your andalusite-to-sillimanite transformation permitted andalusite to persist metastably outdoors its stability industry. It is vital to acknowledge the impact of deformation on metamorphic more info reactions, along with the extent to which deformation (strain Electrical power) may well aid reactions.

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