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paths The idealized view of P-T paths is mineral assemblages equilibrate at each individual stage of The trail within the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This check out ignores kinetic things associated with the energetics of nucleation and growth of minerals, Though these aspects could be essential 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 problems corresponding to The soundness industry of sillimanite illustrates which the sluggish kinetics from the andalusite-to-sillimanite transformation allowed andalusite to here persist metastably outside its steadiness subject. It is necessary to acknowledge the affect of deformation on metamorphic reactions, and also the extent to which deformation (pressure Strength) could assist reactions.

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