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Component zoning Metamorphic (and igneous) minerals may perhaps change composition in response to switching chemical and physical situations, for instance changes in strain-temperature ailments, deformation variables, or chemical factors (e.g., presence of fluids). The chemical response of a mineral to those variations might be recorded in minerals that have crystal chemical and structural features that allow for compositions acquired early inside the mineral's expansion record to generally be preserved in the course of afterwards stages of advancement at distinctive problems.

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