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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 in the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic things connected with the energetics of nucleation and growth of minerals, although these elements can be crucial for a few metamorphic phases and reactions. As an example, the presence check here of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T disorders comparable to The soundness discipline of sillimanite illustrates which the sluggish kinetics of the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside its stability industry. It is important to acknowledge the influence of deformation on metamorphic reactions, as well as the extent to which deformation (pressure Power) may guide reactions.

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