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paths The idealized look at of P-T paths is the fact mineral assemblages equilibrate at every single phase of the path from the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. 台中硬碟救援 This see ignores kinetic variables connected with the energetics of nucleation and progress of minerals, Though these factors can be significant for some metamorphic phases and reactions. For instance, the existence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T disorders comparable to the stability industry of sillimanite illustrates that the sluggish kinetics on the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside the house its balance discipline. It's important to acknowledge the affect of deformation on metamorphic reactions, and also the extent to which deformation (pressure Electricity) could help reactions.

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