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paths The idealized watch of P-T paths is always that mineral assemblages equilibrate at each Check Out Your URL and every stage of The trail within the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This see ignores kinetic aspects connected with the energetics of nucleation and expansion of minerals, Whilst these factors could possibly be significant for many metamorphic phases and reactions. For example, the presence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T problems comparable to the stability area of sillimanite illustrates the sluggish kinetics on the andalusite-to-sillimanite transformation permitted andalusite to persist metastably exterior its security industry. It is important to recognize the influence of deformation on metamorphic reactions, as well as the extent to which deformation (strain Vitality) may possibly support reactions.

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