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In Figure 3, kyanite inclusions manifest in garnet in a very rock which includes only sillimanite within the matrix, indicating which the rock was Formerly in the kyanite stability area but that P-T conditions changed. When the matrix of your rock (such as the garnet rim) equilibrated, the rock was while in the Clicking Here silliminate steadiness field (Fig. 4).

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than the circumstances of the peak of metamorphism signify disequilibrium. Usually, nonetheless, the evidence for disequilibrium can be extremely practical as it can be used to reconstruct P-T path segments.