Chemical elemental impurities in talc are mainly transition metal ions such as Fe, Mn, and Ti, which are mostly introduced by wall rock weathering, hydrothermal activities, and other processes, and exist in the form of isomorphism or interstitial occupancy. Although their content is low (0.01%–1%), they can alter electron transitions in crystals, selectively absorb visible light, significantly affect the color of talc, and different elements exhibit distinct coloration mechanisms.