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A number of widespread techniques for inferring P-T path segments are: Mineral inclusions Some minerals incorporate inclusions
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In Figure 3, kyanite inclusions come about in garnet inside a rock which has only sillimanite while in the matrix, indicating the rock was previously during å°ä¸ç¡¬ç¢Ÿæ•‘æ´ the kyanite security area but that P-T disorders adjusted. In the event the matrix in the rock (including the garnet rim) equilibrated, the rock was in the silliminate steadiness subject (Fig. 4).
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At the peak of metamorphism, the mineral assemblage presumably equilibrated, and no (or tiny) even further response came about given that the rock cooled and decompressed en route to the Earth's area.
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