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of other minerals. Such as, garnets normally incorporate inclusions of minerals which were present in the rock matrix given that the garnet grew, but which were not fully eliminated by metamorphic reactions throughout progressive metamorphism.

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because we wish as much P-T route facts as you possibly can, so as to have the ability to interpret the thermal/tectonic procedures and background in addition as is possible. This can be bad

in comparison to the situations of the height of metamorphism characterize disequilibrium. In most cases, nonetheless, the proof for disequilibrium can be extremely helpful since it can be employed to reconstruct P-T 台中硬碟救援 route segments.