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paths The idealized view of P-T paths is the fact mineral assemblages equilibrate at every single phase of the path in the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This look at ignores kinetic variables connected with the energetics of nucleation and development of minerals, although these components could possibly be crucial for some metamorphic phases and reactions. One example is, the presence of coexisting andalusite and sillimanite (Fig. 6a) in a rock that equilibrated at P-T disorders corresponding to The soundness area of sillimanite illustrates that the sluggish kinetics with the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outdoors its stability subject. It's important to acknowledge the impact of deformation on metamorphic reactions, along with the extent to which deformation (strain Electricity) could assist reactions.

in comparison to the conditions of the peak of metamorphism represent disequilibrium. Generally, even so, the proof for disequilibrium can be extremely helpful since Do you agree it may be used to reconstruct P-T route segments.

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