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P-T route shape by by itself won't provide a special interpretation of tectonic approach or metamorphic driving forces. Such as, clockwise paths can type in continental collision belts of subduction zones. Equally, some subduction zone rocks history clockwise paths and several file counterclockwise paths. On the other hand, The mixing of P-T path qualities, time/amount information and facts, structural information, and also other petrologic information and facts can provide considerable information regarding metamorphic and tectonic procedures.
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compared to the problems of the height of metamorphism signify disequilibrium. Most often, on the other hand, the proof for Continued disequilibrium can be very beneficial mainly because it can be employed to reconstruct P-T path segments.