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Factor zoning Metamorphic (and igneous) minerals may possibly transform composition in response to altering chemical and Bodily situations, for example alterations in force-temperature conditions, deformation variables, or chemical factors (e.g., presence of fluids). The chemical response more info of a mineral to these modifications could be recorded in minerals that have crystal chemical and structural properties that make it possible for compositions obtained early in the mineral's development heritage to get preserved in the course of afterwards levels of growth at diverse disorders.
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in comparison to the conditions of the peak of metamorphism symbolize disequilibrium. Typically, having said that, the evidence for disequilibrium can be quite valuable mainly because it can be employed to reconstruct P-T path segments.