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paths The idealized look at of P-T paths is the fact that mineral assemblages equilibrate at just about every stage of the path with the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic components relevant to the energetics of nucleation and growth of minerals, Even though these aspects might be important for many metamorphic phases and reactions. By way of example, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T disorders similar to The soundness area of sillimanite illustrates which the sluggish kinetics with the andalusite-to-sillimanite transformation permitted andalusite Discover More Here to persist metastably outside its steadiness subject. It is vital to recognize the impact of deformation on metamorphic reactions, plus the extent to which deformation (strain energy) may perhaps aid reactions.
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