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Mica is a group of silicate minerals known for their perfect cleavage, allowing them to be split into thin, flexible sheets. These minerals are typically found in igneous and metamorphic rocks. The most common types of mica are muscovite and phlogopite, both of which are prized for their light-reflecting properties. Natural mica flakes are produced by mechanically separating these minerals from their host rocks, resulting in thin sheets that can be ground into various sizes.


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