In silicate minerals,the SiO₄ tetrahedron can be chemically bonded to form all of the following EXCEPT A) sheets. B) independent tetrahedra. C) double chains. D) triple chains.

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Silicate minerals can form various structures including sheets, independent tetrahedra, and double chains, but they do not form triple chains. Triple chains are not a recognized structural arrangement in silicate mineralogy.

In Silicate Minerals,the SiO4 Tetrahedron Can Be Chemically Bonded to Form

In Silicate Minerals,the SiO₄ Tetrahedron Can Be Chemically Bonded to Form