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paths The idealized look at of P-T paths is mineral assemblages equilibrate at every stage of the path in the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This see ignores kinetic elements connected with the energetics of nucleation and progress of minerals, Despite the fact that these factors can be vital for many metamorphic phases and reactions. For instance, the existence of coexisting andalusite and sillimanite (Fig. 6a) in the rock that equilibrated at P-T problems akin to The soundness area of sillimanite illustrates which the sluggish kinetics on the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outdoors its balance discipline. It's important to recognize the influence of deformation on metamorphic reactions, as well as extent to which deformation (pressure energy) may help reactions.

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