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paths The idealized check out of P-T paths is mineral assemblages equilibrate at each stage of The trail with the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This view ignores kinetic things relevant to the energetics of nucleation and progress get more info of minerals, Though these things can be crucial for some metamorphic phases and reactions. As an example, the existence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T situations akin to The steadiness subject of sillimanite illustrates which the sluggish kinetics in the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outdoors its security area. It can be crucial to recognize the affect of deformation on metamorphic reactions, as well as extent to which deformation (strain Strength) may perhaps help reactions.

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