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paths The idealized watch of P-T paths is always that mineral assemblages equilibrate at each and every stage of The trail with the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This see ignores kinetic factors relevant to the energetics of nucleation and expansion of minerals, Though these elements may be vital 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 at P-T ailments akin to the stability industry of sillimanite illustrates which the sluggish kinetics on the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside its steadiness discipline. It Discover More Here is vital to recognize the impact of deformation on metamorphic reactions, along with the extent to which deformation (strain energy) may perhaps support reactions.

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