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paths The idealized see of P-T paths is that mineral assemblages equilibrate at each individual phase of The trail from your onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This look at ignores kinetic components associated with the energetics of nucleation and development of minerals, Even though these factors can Check This Out be critical for many metamorphic phases and reactions. By way of example, the presence of coexisting andalusite and sillimanite (Fig. 6a) in the rock that equilibrated at P-T circumstances equivalent to the stability subject of sillimanite illustrates the sluggish kinetics with the andalusite-to-sillimanite transformation permitted andalusite to persist metastably exterior its stability industry. It is important to recognize the influence of deformation on metamorphic reactions, and the extent to which deformation (pressure Vitality) could support reactions.
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