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paths The idealized perspective of P-T paths is the fact that mineral assemblages equilibrate at each and every phase of The trail from the onset of metamorphism to the peak of metamorphism, at which å°åŒ—ç¡¬ç¢Ÿæ•‘æ´ the final assemblage is locked in. This look at ignores kinetic components related to the energetics of nucleation and development of minerals, Though these variables may very well be vital for a few metamorphic phases and reactions. One example is, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a rock that equilibrated at P-T circumstances comparable to The steadiness subject of sillimanite illustrates which the sluggish kinetics of your andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside its stability discipline. It is necessary to acknowledge the impact of deformation on metamorphic reactions, plus the extent to which deformation (pressure Electrical power) might aid reactions.
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