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P-T path condition by alone will not provide a exclusive interpretation of tectonic course of action or metamorphic driving forces. One example is, clockwise paths can form in continental collision belts of subduction zones. Likewise, some subduction zone rocks report clockwise paths and some record counterclockwise paths. Even so, the integration of P-T click here path features, time/level info, structural information, and also other petrologic details can provide major information about metamorphic and tectonic processes.
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