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paths The idealized check out of P-T paths is usually that mineral assemblages equilibrate at every stage of the path through the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic aspects relevant to the energetics of nucleation and advancement of minerals, although these elements could possibly be critical for many metamorphic phases and reactions. One get more info example is, the existence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T circumstances akin to The soundness discipline of sillimanite illustrates the sluggish kinetics on the andalusite-to-sillimanite transformation permitted andalusite to persist metastably exterior its balance subject. It is important to recognize the influence of deformation on metamorphic reactions, and the extent to which deformation (strain Electrical power) might assist reactions.
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