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In Figure three, kyanite inclusions occur in garnet in the rock that has only sillimanite within the matrix, indicating the rock was Beforehand while in the kyanite steadiness field but that P-T situations transformed. In the event the matrix from the rock (including the garnet rim) equilibrated, the rock was from the silliminate steadiness field (Fig. 4).

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For some rocks, the only Element of the P-T path recorded during the mineral assemblage and texture from the rock is definitely the 'peak' of metamorphism -- the problems from the thermal maximum (i.e., the most temperature along with the pressure at the utmost temperature). If your rock had a sedimentary or volcanic protolith, you'll be able to infer which the rock started out in the area, achieved peak situations at some temperature and depth within the Earth, and returned into the floor (in which the rock was collected).

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