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For many rocks, the only A part of the P-T path recorded while in the mineral assemblage and texture with the rock is definitely the 'peak' of metamorphism -- the circumstances in the thermal greatest (i.e., the utmost temperature as Click This Link well as tension at the maximum temperature). When the rock had a sedimentary or volcanic protolith, you'll be able to infer the rock started off within the area, arrived at peak circumstances at some temperature and depth in the Earth, and returned to the surface area (in which the rock was collected).
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