Non-silicate minerals have a simpler structure because they lack the silicate tetrahedral structure. They are classified into six kinds based on their composition and internal structure. The most common minerals on the earth are silicates, which contain silicon, oxygen, and magnesium. Furthermore, these minerals serve a variety of purposes and provide metallic resources. CaO is the chemical formula for quartz, for example.
The structure of silicates varies between silicates and these-silicates. In neosilicates, the atoms of silicon are arranged in tetrahedra and share three oxygen atoms. On the other hand, in sorosilicates, the atoms are stacked in rings of four tetrahedra and share two oxygen atoms with their neighbors.
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