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Geologically, phlogopite mica is typically found in ultramafic and mafic rocks, particularly in metamorphic environments. The presence of phlogopite often indicates specific conditions of temperature and pressure in the Earth's crust. It can form during the metamorphism of magnesium-rich rocks and is often associated with other minerals such as biotite and garnet. Geologists study these formations to gain insights into the geological history of regions, making phlogopite a valuable indicator mineral.


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what is a mica powder_video mica