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In Determine 3, kyanite inclusions manifest in garnet inside of a rock which has only sillimanite in the matrix, indicating which the rock was Earlier within the kyanite steadiness subject but that P-T situations improved. When the matrix with the rock (including the garnet rim) equilibrated, the rock was in the silliminate stability subject (Fig. 4).

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For a few rocks, the one Portion of the P-T path recorded during the mineral assemblage and texture from the rock would be the 'peak' of metamorphism -- the conditions of your thermal greatest (i.e., the most temperature and the tension at the maximum temperature). In the event the rock had a sedimentary or volcanic protolith, it is possible to infer the rock started on the floor, achieved peak conditions at some temperature and depth within the Earth, and returned for the surface (in which the rock was collected).

At the height of metamorphism, the mineral assemblage presumably equilibrated, and no (or very little) even further response occurred Discover More because the rock cooled and decompressed en route to the Earth's surface.

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