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of a metamorphic rock could be the list of all P-T situations professional by a rock during its metamorphic history (Determine 1).

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paths The idealized view of P-T paths is always that mineral assemblages equilibrate at every stage of The trail from your onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This watch ignores kinetic factors connected with the energetics of nucleation and growth of minerals, Despite the fact that these factors could be vital for a few metamorphic phases and reactions. Such as, the presence of coexisting andalusite and sillimanite check here (Fig. 6a) in a very rock that equilibrated at P-T circumstances comparable to the stability discipline of sillimanite illustrates that the sluggish kinetics in the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outside its security industry. It is vital to acknowledge the influence of deformation on metamorphic reactions, along with the extent to which deformation (pressure Power) may possibly assist reactions.

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