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of a metamorphic rock could be the set of all P-T disorders knowledgeable by a rock during its metamorphic record (Determine one).

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paths The idealized watch of P-T paths is the fact mineral assemblages equilibrate at read more every single stage of the path from the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic elements related to the energetics of nucleation and advancement of minerals, Whilst these components could possibly be crucial for some metamorphic phases and reactions. For example, the existence of coexisting andalusite and sillimanite (Fig. 6a) in the rock that equilibrated at P-T problems equivalent to the stability field of sillimanite illustrates which the sluggish kinetics from the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outside its steadiness area. It is crucial to recognize the affect of deformation on metamorphic reactions, as well as extent to which deformation (strain energy) may possibly guide reactions.

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