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Although it may not be achievable to find out the trajectory on the P-T route from inclusions by yourself, inclusions can be applied with other chemical and textural information and facts to raised determine The trail.

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For a few rocks, the only real A part of the P-T path recorded during the mineral assemblage and texture in the rock here will be the 'peak' of metamorphism -- the ailments from the thermal optimum (i.e., the utmost temperature and also the tension at the maximum temperature). If the rock had a sedimentary or volcanic protolith, it is possible to infer which the rock started with the surface, reached peak situations at some temperature and depth during the Earth, and returned to the surface area (exactly where the rock was gathered).

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