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paths The idealized look at of P-T paths is the fact that mineral assemblages equilibrate at just about every stage of The trail from the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This look at ignores kinetic things connected with the energetics of nucleation and growth of minerals, Despite the fact that these factors could possibly be important for many 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 ailments comparable to The steadiness field of sillimanite illustrates that the sluggish kinetics of the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outside its security field. It can be crucial to acknowledge the impact of deformation on metamorphic reactions, and the extent to which deformation (strain Strength) may perhaps assist reactions.

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