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For some rocks, the only real Component of the P-T route recorded inside the mineral assemblage and texture from the rock is definitely the 'peak' of metamorphism -- the ailments on the thermal most (i.e., the utmost temperature as well as the pressure at the most temperature). In case the rock had a sedimentary or volcanic protolith, you are able to infer that the rock started off on the surface, arrived at peak ailments at Continue some temperature and depth inside the Earth, and returned towards the area (wherever the rock was collected).
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