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paths The idealized view of P-T paths is the fact mineral assemblages equilibrate at each phase of the path from the onset of metamorphism to Continue Reading the height of metamorphism, at which the final assemblage is locked in. This look at ignores kinetic factors relevant to the energetics of nucleation and growth of minerals, Despite the fact that these aspects may very well be crucial for many metamorphic phases and reactions. As an example, the existence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T disorders comparable to the stability discipline of sillimanite illustrates which the sluggish kinetics in the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outdoors its steadiness subject. It is important to recognize the impact of deformation on metamorphic reactions, as well as the extent to which deformation (pressure energy) may well help reactions.

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