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At the peak of metamorphism, the mineral assemblage presumably equilibrated, and no (or tiny) even more reaction came about since the rock cooled and decompressed en route to the Earth's floor.

Component zoning Metamorphic (and igneous) minerals may perhaps adjust composition in reaction to shifting chemical and physical ailments, for instance adjustments in tension-temperature problems, deformation variables, or chemical factors (e.g., existence of fluids). The chemical response of the mineral to those adjustments may be recorded in minerals which have crystal chemical and structural traits that permit compositions acquired early within the mineral's expansion history for being preserved all through later on Click This Link levels of development at diverse situations.

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