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For some rocks, the sole Section of the P-T route recorded from the mineral assemblage and texture of the rock will be the 'peak' of metamorphism -- the situations on the thermal utmost (i.e., the most temperature and the stress at the utmost temperature). In case the rock experienced a sedimentary or volcanic protolith, you could infer that the rock started in the surface area, achieved peak ailments at some temperature and depth from the Earth, and returned into the area (where the rock was collected).
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