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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 path through the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This watch ignores kinetic elements relevant to the energetics of nucleation and growth of minerals, Despite the fact that these things could be significant for some metamorphic phases and reactions. By way of Do you agree example, the existence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T ailments equivalent to The soundness field of sillimanite illustrates the sluggish kinetics with the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outdoors its steadiness field. It is necessary to acknowledge the influence of deformation on metamorphic reactions, along with the extent to which deformation (pressure Power) may well assist reactions.

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