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The length of the path from start off (onset of metamorphism) to complete (publicity with the rock within the Earth's area) will vary Click Here from rock to rock based on the tectonic background
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For many rocks, the only Portion of the P-T path recorded while in the mineral assemblage and texture of the rock may be the 'peak' of metamorphism -- the disorders from the thermal utmost (i.e., the utmost temperature as well as stress at the utmost temperature). If the rock had a sedimentary or volcanic protolith, you may infer the rock begun in the floor, arrived at peak situations at some temperature and depth from the Earth, and returned to the area (exactly where the rock was collected).
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