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For a few rocks, the only real Section of the P-T route recorded within the mineral assemblage and texture on the rock is definitely the 'peak' of metamorphism -- the circumstances on the thermal most (i.e., the maximum temperature and also the strain at the utmost temperature). If your rock experienced a sedimentary or volcanic protolith, you are able click here to infer that the rock started out with the area, arrived at peak conditions at some temperature and depth within the Earth, and returned for the floor (the place the rock was gathered).
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