It occurs in high temperature hydrothermal deposits and contact metamorphic rocks.
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Contact metamorphic rocks are usually known as hornfels.
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It typically occurs in contact metamorphic rocks.
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Muscovite is the most common mica, found in granites, pegmatites, gneisses, and schists, and as a contact metamorphic rock or as a secondary mineral resulting from the alteration of topaz, feldspar, kyanite, etc . In pegmatites, it is often found in immense sheets that are commercially valuable.
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