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paths The idealized look at of P-T paths is the fact mineral assemblages equilibrate at every stage of The trail with the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This view ignores kinetic things relevant to the energetics of nucleation and expansion of minerals, Though these elements could be important for some metamorphic phases and reactions. For example, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a very rock that equilibrated at P-T problems equivalent to The steadiness discipline of sillimanite illustrates the sluggish kinetics of the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outdoors its stability industry. Clicking Here It is crucial to recognize the influence of deformation on metamorphic reactions, and the extent to which deformation (pressure Vitality) may guide reactions.

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