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For many rocks, the sole Element of the P-T path recorded during the mineral assemblage and texture of your rock could be the 'peak' of metamorphism -- the problems of the thermal highest (i.e., the maximum temperature plus the pressure at the utmost temperature). In case the rock had a sedimentary or volcanic protolith, you may infer which the rock begun at the area, reached peak ailments at some temperature and depth while in the Earth, and returned for the floor (the place the rock was collected).

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since we want just as Click Here much P-T route info as feasible, In order to be able to interpret the thermal/tectonic procedures and heritage also as possible. This is often terrible

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