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paths The idealized view of P-T paths is that mineral assemblages click here equilibrate at each individual phase of the path in the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This look at ignores kinetic elements related to the energetics of nucleation and advancement of minerals, While these aspects might be important for many metamorphic phases and reactions. One example is, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T conditions similar to The soundness area of sillimanite illustrates which the sluggish kinetics from the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outdoors its balance area. It's important to acknowledge the influence of deformation on metamorphic reactions, as well as the extent to which deformation (strain Power) may possibly help reactions.

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