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P-T route condition by itself will not offer a one of a kind interpretation of tectonic process or metamorphic driving forces. As an example, clockwise paths can sort in continental collision belts of subduction zones. In the same way, some subduction zone rocks document clockwise paths and several report counterclockwise paths. However, the integration of P-T path attributes, time/rate data, structural facts, and also Discover More Here other petrologic data can offer considerable information regarding metamorphic and tectonic procedures.
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