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For a few rocks, the å°åŒ—ç¡¬ç¢Ÿæ•‘æ´ only Portion of the P-T path recorded within the mineral assemblage and texture from the rock may be the 'peak' of metamorphism -- the situations from the thermal maximum (i.e., the most temperature as well as the force at the most temperature). When the rock experienced a sedimentary or volcanic protolith, you could infer that the rock commenced for the surface, attained peak situations at some temperature and depth from the Earth, and returned into the surface (exactly where the rock was collected).
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