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paths The idealized look at of P-T paths is mineral assemblages equilibrate at each and every stage of the path within the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This see ignores kinetic elements connected to the energetics of nucleation and expansion of minerals, Despite the fact that these aspects may be vital for some metamorphic phases and reactions. For instance, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T problems akin to the stability industry of sillimanite illustrates the sluggish kinetics in the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside the house its balance field. It is important to acknowledge the affect of deformation on metamorphic reactions, as well as the extent to which deformation (strain Electricity) could help reactions.

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