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For many rocks, the only real A part of the P-T route recorded in the mineral assemblage and texture in the rock is definitely the 'peak' of metamorphism -- the situations of the thermal greatest (i.e., the most temperature and also the force at the most temperature). In the event the Click Here rock experienced a sedimentary or volcanic protolith, you'll be able to infer which the rock started with the area, reached peak problems at some temperature and depth within the Earth, and returned on the area (exactly where the rock was gathered).

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