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of other minerals. One example is, garnets normally consist of inclusions of minerals that Check This Out were existing from the rock matrix as the garnet grew, but that were not entirely removed by metamorphic reactions during progressive metamorphism.
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compared to the situations of the peak of metamorphism symbolize disequilibrium. In most cases, having said that, the evidence for disequilibrium can be quite handy mainly because it may be used to reconstruct P-T path segments.