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paths The idealized watch of P-T paths is the fact mineral assemblages equilibrate at every single stage of the path within the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This view ignores kinetic things relevant to the energetics of nucleation and progress of minerals, Though these factors may be vital 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 equivalent to The steadiness subject of sillimanite illustrates the sluggish kinetics of the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outdoors its stability industry. It is crucial to recognize the influence of deformation on metamorphic reactions, as Click This Link well as extent to which deformation (pressure Power) may perhaps guide reactions.
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