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Aspect zoning Metamorphic (and igneous) minerals may possibly alter composition in reaction to switching chemical and physical circumstances, like alterations in tension-temperature disorders, deformation variables, or chemical factors (e.g., presence of fluids). The chemical response of a mineral to these alterations could possibly be recorded in minerals which have crystal chemical and structural features that allow for compositions obtained early during Continue the mineral's expansion heritage to generally be preserved all through later stages of growth at different situations.

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