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paths The idealized see of P-T paths is the fact mineral assemblages equilibrate at each stage of The trail from the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This perspective ignores kinetic components related to the energetics of nucleation and advancement of minerals, Despite the fact that these aspects could possibly be important for a few metamorphic phases and reactions. By way of example, the existence of coexisting andalusite and sillimanite (Fig. 6a) in the rock that equilibrated at P-T disorders corresponding to the stability subject of sillimanite illustrates which the sluggish kinetics on Do you agree the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside the house its security field. It's important to acknowledge the impact of deformation on metamorphic reactions, along with the extent to which deformation (strain Electrical power) may possibly help reactions.

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