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The length of The trail from start out (onset of metamorphism) to complete (publicity of your rock at the Earth's surface) will vary from rock to rock according to the tectonic historical past
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For many rocks, the one Portion of the P-T path recorded during the mineral assemblage and texture with the rock would be the 'peak' of metamorphism -- the situations with the thermal most (i.e., the utmost temperature as well as the tension at the most temperature). If the rock experienced a sedimentary or volcanic protolith, Click Here you could infer the rock commenced for the surface area, reached peak disorders at some temperature and depth while in the Earth, and returned for the surface area (the place the rock was gathered).
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