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For some rocks, the one A part of the P-T route recorded in the mineral assemblage and texture on the rock is definitely the 'peak' of Check This Out metamorphism -- the situations of your thermal optimum (i.e., the utmost temperature and the strain at the most temperature). When the rock experienced a sedimentary or volcanic protolith, you can infer the rock begun on the floor, reached peak problems at some temperature and depth during the Earth, and returned towards the floor (where the rock was collected).
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