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Aspect zoning Metamorphic (and igneous) minerals could adjust composition in reaction to transforming chemical and physical situations, for example adjustments click here in tension-temperature circumstances, deformation variables, or chemical elements (e.g., existence of fluids). The chemical reaction of the mineral to those adjustments could possibly be recorded in minerals which have crystal chemical and structural traits that permit compositions acquired early inside the mineral's advancement record to be preserved during later stages of growth at different ailments.

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compared to disorders of the peak of metamorphism depict disequilibrium. Most often, however, the evidence for disequilibrium can be very helpful since it can be used to reconstruct P-T path segments.