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Several widespread approaches for inferring P-T route segments are: Mineral inclusions Some minerals comprise inclusions
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of other minerals. For example, garnets typically include inclusions of minerals that were existing from the rock matrix as being the garnet å°åŒ—ç¡¬ç¢Ÿæ•‘æ´ grew, but which were not absolutely eradicated by metamorphic reactions in the course of progressive metamorphism.
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