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At the height of metamorphism, the mineral assemblage presumably equilibrated, and no (or small) even more response took place because the rock cooled and decompressed en path to the Earth's area.
Aspect zoning Metamorphic (and igneous) minerals may well improve composition in reaction to changing chemical and physical situations, including alterations in force-temperature disorders, deformation variables, or chemical factors (e.g., presence of more info fluids). The chemical response of a mineral to these alterations can be recorded in minerals which have crystal chemical and structural features that enable compositions obtained early from the mineral's development background to become preserved for the duration of afterwards phases of progress at distinctive circumstances.
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