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paths The idealized check out of P-T paths is usually that mineral assemblages equilibrate at each and every phase of The trail from the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic things linked to the energetics of nucleation and advancement of minerals, Though these things could be significant for some metamorphic phases and reactions. By way of example, the existence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T problems equivalent to The soundness industry of sillimanite illustrates the sluggish kinetics with the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside the house its balance subject. It is important to recognize the impact of deformation on metamorphic reactions, and the extent to which deformation Continue (strain energy) could aid reactions.

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