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paths The idealized perspective of P-T paths is mineral assemblages equilibrate at each stage of The trail with Check Out Your URL the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This view ignores kinetic things relevant to the energetics of nucleation and progress of minerals, Even though these factors can be critical for a few metamorphic phases and reactions. For example, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a very rock that equilibrated at P-T situations corresponding to The steadiness subject of sillimanite illustrates the sluggish kinetics of the andalusite-to-sillimanite transformation authorized andalusite to persist metastably exterior its balance field. It can be crucial to acknowledge the influence of deformation on metamorphic reactions, and the extent to which deformation (pressure Vitality) may support reactions.

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