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Factor zoning Metamorphic (and igneous) minerals could change composition in reaction to shifting chemical and Bodily conditions, which include alterations in pressure-temperature situations, deformation variables, or chemical components (e.g., existence of fluids). The chemical reaction of the mineral to those alterations may be recorded in minerals that have crystal chemical and structural attributes that permit compositions acquired early in the mineral's advancement historical past to be preserved through afterwards stages of expansion at different circumstances.
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