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In Figure 3, kyanite inclusions manifest in garnet inside a rock which includes only sillimanite from the matrix, indicating which the rock was Formerly during the kyanite stability subject but that P-T disorders modified. When the matrix from the rock (including the garnet rim) equilibrated, the rock was while in the silliminate stability industry (Fig. four).

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of other minerals. For instance, garnets generally contain inclusions of minerals which were current within the rock matrix as the garnet grew, but which were not here absolutely eradicated by metamorphic reactions in the course of progressive metamorphism.

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