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For a few rocks, the only real part of the P-T path recorded from the mineral assemblage and texture from the rock could be the 'peak' of metamorphism -- the problems from the thermal maximum (i.e., the most temperature and the stress at the most temperature). In the event the rock experienced a sedimentary or volcanic protolith, you could infer the rock started for the surface area, attained peak circumstances at some temperature and depth in the Earth, and returned into the floor (the place the rock was gathered).
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