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In Determine three, kyanite inclusions manifest in garnet in the rock which includes only sillimanite from the matrix, indicating that the rock was previously from the kyanite here steadiness field but that P-T situations adjusted. When the matrix with the rock (such as the garnet rim) equilibrated, the rock was during the silliminate balance subject (Fig. four).
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when compared to the circumstances of the peak of metamorphism represent disequilibrium. Usually, however, the proof for disequilibrium can be quite practical as it can be utilized to reconstruct P-T route segments.