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The trajectory and shape from the P-T route, the premiums of metamorphic processes, and the period of metamorphism can be a function in the source of warmth as well as the mechanisms of burial and unroofing (if strain improve is associated).

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paths The idealized view of P-T paths is usually that mineral assemblages equilibrate at just about every phase of the path from the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This view ignores kinetic elements associated with the energetics of nucleation and expansion of minerals, Despite the fact that these elements could possibly be crucial for some metamorphic phases and reactions. Such as, the existence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T circumstances equivalent to the stability field of sillimanite Do you agree illustrates which the sluggish kinetics in the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside the house its steadiness discipline. It's important to acknowledge the affect of deformation on metamorphic reactions, as well as the extent to which deformation (pressure Electricity) could assist reactions.

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