give the structure and bonding of silicates
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The basic building block, the structural unit, of silicate minerals is the SiO44- tetrahedron. In the SiO44- tetrahedron each Si atom is covalently bonded to 4 oxygen atoms. ... The tetrahedra can link together by sharing corners resulting in Si-O-Si covalent bonds. A number of different structures are therefore possible.
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Structure. The basic structural unit of all silicate minerals is the silicon tetrahedron in which one silicon atom is surrounded by and bonded to (i.e., coordinated with) four oxygen atoms, each at the corner of a regular tetrahedron.
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