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For a few rocks, the one Section of the P-T path recorded from the mineral assemblage and texture on the rock is the 'peak' of metamorphism -- the conditions on the thermal maximum (i.e., the maximum temperature along with the Check Out Your URL tension at the most temperature). If your rock experienced a sedimentary or volcanic protolith, you can infer that the rock commenced for the area, reached peak circumstances at some temperature and depth while in the Earth, and returned to your area (where the rock was collected).

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