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For a few rocks, the only Portion of the P-T route recorded Discover More inside the mineral assemblage and texture of the rock may be the 'peak' of metamorphism -- the disorders with the thermal maximum (i.e., the utmost temperature plus the force at the most temperature). When the rock had a sedimentary or volcanic protolith, you'll be able to infer which the rock started out in the surface, achieved peak problems at some temperature and depth within the Earth, and returned into the floor (in which the rock was collected).

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