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paths The idealized view of P-T paths is always that mineral assemblages equilibrate at every stage of the path from the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This perspective ignores kinetic components linked to the energetics of nucleation and development of minerals, although these factors might be crucial for a few metamorphic phases and reactions. As an example, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated click here at P-T ailments akin to the stability industry of sillimanite illustrates the sluggish kinetics from the andalusite-to-sillimanite transformation authorized andalusite to persist metastably exterior its balance field. It can be crucial to acknowledge the influence of deformation on metamorphic reactions, and the extent to which deformation (pressure Vitality) might guide reactions.

compared to the situations of the height of metamorphism represent disequilibrium. Normally, on the other hand, the proof for disequilibrium can be very helpful since it may be used to reconstruct P-T route segments.

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