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Mica is a silicate mineral that primarily forms in metamorphic rock environments. It is created through the alteration of granitic rocks under high pressure and temperature conditions, leading to its characteristic flaky structure. White mica, particularly muscovite, is one of the most abundant forms of mica found in nature. Its formation can be traced back millions of years to a time when the Earth’s crust was undergoing significant geological changes.


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muscovite mica_muscovite mica