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paths The idealized view of P-T paths is that mineral assemblages equilibrate at each individual stage of The trail through the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This perspective ignores kinetic elements connected to the energetics of nucleation and progress of minerals, although these aspects might be important for many metamorphic phases and reactions. For example, the presence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T circumstances equivalent to The steadiness subject of sillimanite illustrates the sluggish kinetics of read more the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outdoors its stability industry. It is crucial to recognize the influence of deformation on metamorphic reactions, plus the extent to which deformation (strain Power) may perhaps support reactions.

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