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For some rocks, the sole part of the P-T route recorded from the mineral assemblage and texture on the rock may be the 'peak' of metamorphism -- the situations on the thermal highest (i.e., the maximum temperature and also the pressure at the most temperature). When the rock experienced a sedimentary or Check This Out volcanic protolith, you may infer the rock began within the floor, achieved peak disorders at some temperature and depth inside the Earth, and returned to the area (where the rock was collected).

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