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paths The idealized check out of P-T paths is usually that mineral assemblages equilibrate at each and every phase of the path with the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This view ignores kinetic elements linked to the energetics of nucleation and advancement of minerals, Despite the fact that these factors could be important for some Continue metamorphic phases and reactions. As an example, the presence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T circumstances equivalent to the stability discipline of sillimanite illustrates that the sluggish kinetics on the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside its steadiness discipline. It's important to recognize the impact of deformation on metamorphic reactions, as well as the extent to which deformation (strain Electrical power) may possibly help reactions.

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