In silicate minerals,the SiO₄ tetrahedron can be linked together by sharing: A) silicon atoms. B) cations. C) electrons. D) oxygen atoms.

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The SiO4 tetrahedron can be linked together by sharing oxygen atoms, forming various structures such as chains, sheets, and three-dimensional networks, which are the building blocks of silicate minerals. Cations and electrons are not directly involved in these linkages. Sharing silicon atoms is also possible, but less common.

In Silicate Minerals,the SiO4 Tetrahedron Can Be Linked Together by Sharing

In Silicate Minerals,the SiO₄ Tetrahedron Can Be Linked Together by Sharing