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paths The idealized look at of P-T paths is mineral assemblages equilibrate at each stage of The trail through the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This see ignores kinetic things relevant to the energetics of nucleation and expansion of minerals, Despite the fact that these elements may be important for many metamorphic phases and reactions. By way of example, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T disorders comparable to The soundness discipline of sillimanite illustrates that the sluggish kinetics of your andalusite-to-sillimanite transformation permitted andalusite to persist metastably outdoors its Check This Out stability area. It is important to acknowledge the affect of deformation on metamorphic reactions, along with the extent to which deformation (strain Strength) may support reactions.
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