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In Determine 3, kyanite inclusions come about in garnet inside a rock which has only sillimanite in the matrix, indicating the rock was Earlier during the kyanite steadiness field but that P-T situations modified. If the matrix with the rock (such as the garnet rim) equilibrated, the rock was inside the silliminate stability subject (Fig. four).

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At the peak of metamorphism, the mineral assemblage presumably equilibrated, and no (or minor) further more response took place because the rock cooled and decompressed en route to the Earth's floor.

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