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paths The idealized perspective of P-T paths is the fact that mineral assemblages equilibrate at just about every stage of the path within the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This look at ignores kinetic things relevant to the energetics of nucleation and advancement of minerals, Though these components can be essential for a few metamorphic phases and reactions. One example is, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a very rock that equilibrated at P-T problems corresponding to The steadiness discipline of sillimanite illustrates the sluggish kinetics with the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside its balance industry. It can be crucial to acknowledge the Discover More influence of deformation on metamorphic reactions, as well as extent to which deformation (strain energy) may perhaps assist reactions.

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