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P-T path shape by alone doesn't give a special interpretation of tectonic system or metamorphic driving forces. For instance, clockwise paths can variety in continental collision belts of subduction zones. Likewise, some subduction zone rocks record clockwise paths and a few report counterclockwise paths. On the other hand, The combination of P-T route characteristics, time/amount facts, structural info, and other petrologic data can offer sizeable information about metamorphic and tectonic processes.
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compared to the disorders of the height of metamorphism signify disequilibrium. Usually, nevertheless, the proof for disequilibrium can Do you agree be quite useful as it can be utilized to reconstruct P-T path segments.