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paths The idealized look at of P-T paths is that mineral assemblages equilibrate at just about every phase of the path from your onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. website This look at ignores kinetic things linked to the energetics of nucleation and advancement of minerals, Even though these factors can be essential for many metamorphic phases and reactions. For example, the existence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T disorders corresponding to The soundness area of sillimanite illustrates the sluggish kinetics with the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outside its security industry. It is vital to acknowledge the impact of deformation on metamorphic reactions, as well as the extent to which deformation (pressure Strength) may perhaps assist reactions.

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