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paths The idealized see of P-T paths is the fact mineral assemblages equilibrate at each phase of the path through the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This view ignores kinetic variables connected to the energetics of nucleation and progress of minerals, Whilst these aspects may very well be crucial for some metamorphic phases and reactions. For example, the presence of coexisting andalusite and sillimanite (Fig. 6a) in a very rock that equilibrated at P-T circumstances comparable to the stability discipline of sillimanite illustrates that the sluggish kinetics in the andalusite-to-sillimanite transformation authorized Continue Reading andalusite to persist metastably outside its security field. It is necessary to acknowledge the affect of deformation on metamorphic reactions, plus the extent to which deformation (strain Electricity) may aid reactions.
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