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paths The idealized perspective of P-T paths is usually that mineral assemblages equilibrate at each stage of The trail in the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. here This watch ignores kinetic factors relevant to the energetics of nucleation and progress of minerals, Though these elements may be significant 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 problems akin to The steadiness subject of sillimanite illustrates the sluggish kinetics of the andalusite-to-sillimanite transformation authorized andalusite to persist metastably exterior its balance field. It is crucial to recognize the influence of deformation on metamorphic reactions, as well as extent to which deformation (pressure Vitality) may support reactions.
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