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paths The idealized check out of P-T paths is the fact that mineral assemblages equilibrate at every phase of The trail within the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This check out ignores kinetic elements related to the energetics of nucleation and growth of minerals, Whilst these variables could be essential for many metamorphic phases and reactions. Such as, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a very rock that equilibrated at P-T situations akin to The steadiness field of sillimanite illustrates the sluggish kinetics from the andalusite-to-sillimanite transformation permitted andalusite to persist Continue metastably outdoors its stability field. It is vital to acknowledge the affect of deformation on metamorphic reactions, along with the extent to which deformation (pressure Electrical power) may well aid reactions.
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