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paths The idealized perspective of P-T paths is the fact that mineral assemblages equilibrate at every single phase of The trail from the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This look at ignores kinetic things related to the energetics of nucleation and development of minerals, Despite the fact that these components may be essential for many metamorphic phases and reactions. Such as, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated Discover More Here at P-T situations comparable to The steadiness field of sillimanite illustrates the sluggish kinetics with the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outside the house its steadiness field. It's important to acknowledge the affect of deformation on metamorphic reactions, plus the extent to which deformation (pressure Electrical power) may assist reactions.
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