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The trajectory and condition on the P-T path, the rates of metamorphic procedures, as well as duration of metamorphism can be a operate from the supply of warmth and also the mechanisms of burial and unroofing (if stress change is included).

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paths The idealized watch of P-T paths is always that mineral assemblages equilibrate at each and every stage of more info The trail with the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This see ignores kinetic factors relevant to the energetics of nucleation and progress of minerals, Though these elements may be significant for many metamorphic phases and reactions. For example, the existence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T disorders akin to The steadiness subject of sillimanite illustrates that the sluggish kinetics with the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outdoors its steadiness industry. It is crucial to recognize the impact of deformation on metamorphic reactions, along with the extent to which deformation (strain Electrical power) may help reactions.

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