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P-T path shape by alone doesn't provide a one of a kind interpretation of tectonic course of action or metamorphic driving forces. By way of example, clockwise paths can form in continental collision belts of subduction zones. In the same way, some subduction zone rocks file clockwise paths plus some file counterclockwise paths. Nevertheless, The mixing of P-T path attributes, time/rate information and facts, structural data, along with other petrologic info can provide substantial information about metamorphic and tectonic processes.

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paths The idealized view of P-T paths is usually that mineral assemblages equilibrate at every single stage of The trail Check Out Your URL through the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic things connected with the energetics of nucleation and development of minerals, although these variables could possibly be essential for a few metamorphic phases and reactions. For instance, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T conditions similar to the stability industry of sillimanite illustrates that the sluggish kinetics of the andalusite-to-sillimanite transformation permitted andalusite to persist metastably exterior its stability subject. It's important to acknowledge the influence of deformation on metamorphic reactions, as well as extent to which deformation (strain Electrical power) could guide reactions.

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