Therefore, Despite the fact that subduction zone rocks can follow several paths throughout subduction and exhumation, analyzing the specific route that a specific exhumed subduction zone rock adopted is very important for comprehension subduction dynamics.
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For many rocks, the one Portion of the P-T path recorded during the mineral assemblage and texture with the rock may be the 'peak' of metamorphism -- the circumstances of the thermal most (i.e., the utmost temperature as well as the stress at the most temperature). If your rock had a sedimentary or volcanic protolith, you are able to infer the rock started off at the area, reached peak disorders at some temperature and depth in here the Earth, and returned for the area (in which the rock was collected).
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