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paths The idealized check out of P-T paths is the fact that mineral assemblages equilibrate at each and every stage of The trail with the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This view ignores kinetic factors related to the energetics of nucleation and development of minerals, although these things may very well be important for some metamorphic phases and reactions. For example, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T problems equivalent to The steadiness area of sillimanite illustrates which the sluggish kinetics from the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside its balance area. It is necessary to acknowledge the impact of deformation on metamorphic reactions, as well as extent to which deformation (pressure Strength) may possibly help reactions.

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