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paths The idealized watch of P-T paths is always that mineral assemblages equilibrate at every single stage of The trail with the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This view ignores kinetic components connected with the energetics of nucleation and development of minerals, although these things can be crucial for some metamorphic phases and reactions. For example, the existence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T circumstances similar to The steadiness discipline of sillimanite illustrates that the sluggish kinetics of your andalusite-to-sillimanite transformation permitted andalusite to persist metastably outdoors its stability subject. It is necessary to recognize the impact of deformation on metamorphic reactions, along with the extent to Check Out Your URL which deformation (strain energy) may well aid reactions.

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