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of a metamorphic rock will be the set of all P-T problems skilled by a rock throughout its metamorphic heritage (Figure one).

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paths The idealized view of P-T paths is the fact that mineral assemblages equilibrate at each phase of the path with the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This view ignores kinetic elements connected with the energetics more info of nucleation and growth of minerals, Despite the fact that these things might be essential for many metamorphic phases and reactions. Such as, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a rock that equilibrated at P-T circumstances similar to The steadiness subject of sillimanite illustrates the sluggish kinetics of your andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside its stability subject. It is vital to acknowledge the influence of deformation on metamorphic reactions, along with the extent to which deformation (pressure Electrical power) may possibly assist reactions.

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