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For some rocks, the one Element of the P-T route recorded from the mineral assemblage and texture with the rock may be the 'peak' of metamorphism -- the disorders in the thermal highest (i.e., the most temperature and the stress at the maximum temperature). In case the rock had a sedimentary or volcanic protolith, you could infer which the rock began within the area, arrived at peak disorders Check This Out at some temperature and depth in the Earth, and returned for the floor (exactly where the rock was collected).
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