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paths The idealized look at of P-T paths is the fact mineral assemblages equilibrate at every stage of the path with the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This see ignores kinetic elements connected with the energetics of nucleation and growth of minerals, although these elements may very well be critical for some metamorphic phases and reactions. By way of example, the presence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T ailments akin to The steadiness subject of sillimanite illustrates the sluggish kinetics from the andalusite-to-sillimanite transformation permitted andalusite to persist metastably exterior its security industry. It is important to acknowledge the affect of deformation on metamorphic Continued reactions, and the extent to which deformation (pressure Strength) could assist reactions.

as opposed to disorders of the peak of metamorphism depict disequilibrium. Typically, however, the evidence for disequilibrium can be quite valuable mainly because it can be used to reconstruct P-T route segments.