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For a few rocks, the sole part of the P-T route recorded from the mineral assemblage and texture of the rock is definitely the 'peak' of metamorphism -- the ailments from the thermal greatest (i.e., the most temperature as well as the force at the most temperature). When the rock had a sedimentary or volcanic protolith, you can infer that the rock started within the floor, attained peak situations at some temperature and depth in the Earth, and returned towards the floor (where the rock was gathered).

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