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For some rocks, the sole Section of the P-T path recorded during the mineral assemblage and texture in the rock could be the 'peak' of metamorphism -- the problems of your thermal most (i.e., the utmost temperature and also the strain at the utmost temperature). Should the rock had a sedimentary or volcanic protolith, you are able to infer the rock commenced for the area, arrived more info at peak circumstances at some temperature and depth inside the Earth, and returned for the area (where the rock was gathered).
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