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The most common mineral group is the silicates, which are primarily composed of silicon and oxygen. The basic structural component of silicates is the silica tetrahedron (SiO₄), where a silicon atom is surrounded by four oxygen atoms arranged in a tetrahedral shape. These tetrahedra can link together in various ways—sharing oxygen atoms—to form different silicate structures, such as chains, sheets, or three-dimensional frameworks, leading to a wide variety of silicate minerals.

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