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For some rocks, the only Element of the P-T route recorded inside the mineral assemblage and texture of the rock is definitely the 'peak' of metamorphism -- the disorders in the thermal maximum (i.e., the maximum 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 which the rock commenced on the surface, arrived at peak problems at some temperature and depth more info within the Earth, and returned to the floor (in which the rock was collected).

At the peak of metamorphism, the mineral assemblage presumably equilibrated, and no (or minor) even further response happened since the rock cooled and decompressed en path to the Earth's floor.

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