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paths The idealized check out of P-T paths is always that mineral assemblages equilibrate at each individual 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 aspects associated with the energetics of nucleation and growth of minerals, although these things may very well be important for some metamorphic phases and reactions. As an example, the presence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T situations equivalent to The soundness area of sillimanite illustrates which the sluggish kinetics on the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outdoors its stability industry. It is important to recognize the impact Do you agree of deformation on metamorphic reactions, as well as the extent to which deformation (strain Strength) may possibly support reactions.

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