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P-T route condition by itself won't provide a unique interpretation of tectonic method or metamorphic driving forces. For example, clockwise paths can type in continental collision belts of subduction zones. Equally, some subduction zone rocks history clockwise paths and many record counterclockwise paths. Nonetheless, The mixing of P-T path characteristics, time/charge data, structural facts, together with other petrologic information and facts can provide important details about metamorphic and tectonic processes.
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paths The idealized see of P-T paths is the fact mineral assemblages equilibrate at just about every phase of the path in the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This watch ignores kinetic variables linked to the energetics of nucleation and progress of minerals, Despite the fact that these things can be critical for many metamorphic phases and reactions. By way of example, the existence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T circumstances similar to the stability industry of sillimanite illustrates which the sluggish kinetics of the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outside the house its security area. It's important to acknowledge the affect of deformation on metamorphic reactions, and also the extent to which deformation (strain Continue Reading energy) may well aid reactions.
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