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Hence, Even though subduction zone rocks can comply with many paths during subduction and exhumation, analyzing the specific route that a certain exhumed subduction zone rock adopted is significant for being familiar with subduction dynamics.

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For many rocks, the one A part of the P-T path recorded during the mineral assemblage and texture in the rock is the 'peak' of metamorphism -- the circumstances of your thermal utmost (i.e., the utmost temperature and also the pressure at the most temperature). In case the rock had a sedimentary or volcanic protolith, you are able to infer which the rock begun within the area, achieved peak circumstances at some temperature and depth in the Earth, and returned to your floor (exactly where the rock was Continued gathered).

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