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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 record clockwise paths and a few file counterclockwise paths. Discover More On the other hand, The mixing of P-T path qualities, time/fee facts, structural data, as well as other petrologic details can offer sizeable information about metamorphic and tectonic processes.

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