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Micas are a group of silicate minerals known for their unique ability to split into thin, elastic sheets, termed as perfect basal cleavage. Found commonly in igneous and metamorphic rocks, they sometimes occur as small flakes in sedimentary rocks. Mica is prominent in granites, pegmatites, and schists, where large individual crystals, called "books," are commonly found.
Micas are a group of silicate minerals known for their unique ability to split into thin, elastic sheets, termed as perfect basal cleavage. Found commonly in igneous and metamorphic rocks, they sometimes occur as small flakes in sedimentary rocks. Mica is prominent in granites, pegmatites, and schists, where large individual crystals, called "books," are commonly found.
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Micas are a group of silicate minerals known for their unique ability to split into thin, elastic sheets, termed as perfect basal cleavage. Found commonly in igneous and metamorphic rocks, they sometimes occur as small flakes in sedimentary rocks. Mica is prominent in granites, pegmatites, and schists, where large individual crystals, called "books," are commonly found.
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Micas are a group of silicate minerals known for their unique ability to split into thin, elastic sheets, termed as perfect basal cleavage. Found commonly in igneous and metamorphic rocks, they sometimes occur as small flakes in sedimentary rocks. Mica is prominent in granites, pegmatites, and schists, where large individual crystals, called "books," are commonly found.
Micas are a group of silicate minerals known for their unique ability to split into thin, elastic sheets, termed as perfect basal cleavage. Found commonly in igneous and metamorphic rocks, they sometimes occur as small flakes in sedimentary rocks. Mica is prominent in granites, pegmatites, and schists, where large individual crystals, called "books," are commonly found.
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Micas are a group of silicate minerals known for their unique ability to split into thin, elastic sheets, termed as perfect basal cleavage. Found commonly in igneous and metamorphic rocks, they sometimes occur as small flakes in sedimentary rocks. Mica is prominent in granites, pegmatites, and schists, where large individual crystals, called "books," are commonly found.
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