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For that reason, the shape of the path, coupled with time details, provides specifics of the driving forces

paths The idealized check out of P-T paths is always that mineral assemblages equilibrate at every single phase of The trail from your onset of click here metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This check out ignores kinetic elements linked to the energetics of nucleation and progress of minerals, While these things may be important for some metamorphic phases and reactions. For instance, the presence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T problems akin to The soundness discipline of sillimanite illustrates the sluggish kinetics on the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outdoors its stability industry. It can be crucial to recognize the impact of deformation on metamorphic reactions, and also the extent to which deformation (strain Power) may well aid reactions.

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