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A number of typical solutions for inferring P-T route segments are: Mineral inclusions Some minerals include inclusions

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For a few rocks, the one part of the P-T route recorded during the mineral assemblage and texture in the rock could be the 'peak' of metamorphism -- the circumstances on the thermal maximum (i.e., the utmost temperature plus the pressure at the utmost temperature). If your rock had a sedimentary or volcanic protolith, you'll be able to infer which the rock started with the surface, attained peak ailments at some temperature and depth in the Earth, and returned for the floor (where the rock was collected).

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