Consequently, Even though subduction zone rocks can adhere to numerous paths throughout subduction and exhumation, figuring out the specific path that a particular exhumed subduction zone rock adopted is significant for comprehension subduction dynamics.
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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 trail from your onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This look at ignores kinetic aspects associated with the energetics of nucleation and development of minerals, Despite the fact that these aspects may be vital for a few metamorphic phases and reactions. As an example, the presence of coexisting andalusite and sillimanite (Fig. 6a) in the å°ä¸ç¡¬ç¢Ÿæ•‘æ´ rock that equilibrated at P-T situations corresponding to The steadiness subject of sillimanite illustrates that the sluggish kinetics of the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outside its security discipline. It's important to acknowledge the affect of deformation on metamorphic reactions, as well as the extent to which deformation (pressure Electricity) may possibly help reactions.
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