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Component zoning Metamorphic (and igneous) minerals could alter composition in response Continue to modifying chemical and Actual physical conditions, for example variations in pressure-temperature circumstances, deformation variables, or chemical variables (e.g., existence of fluids). The chemical reaction of the mineral to these modifications could be recorded in minerals which have crystal chemical and structural features that permit compositions acquired early during the mineral's progress history being preserved during later levels of development at various circumstances.
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