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Isolated tetrahedra silicates do not link with other silicon or oxygen atoms

Ring Silicates form by sharing oxygen atoms

Single Chain Silicates form a chain when sharing oxygen atoms

Double Chain Silicates form when two or more single chains of tetrahedra bond to each other

Sheet Silicates form when each tetrahedron shares three of its oxygen atoms with other tetrahedra

Framework Silicates form when each tetrahedron is bonded to four other tetrahedras

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Q: Describe the six main crystalline structures of silicate minerals?
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If silicon bonded with three oxygen atoms how might the crystalline structures of silicate minerals?

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What are three common non silicate crystalline structures?

Non-silicate crystalline structures are tetrahedra, isolated, and chains.


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Non-silicate minerals contain oxygen and native elements. They have metallic and non-metallic lusters, and are very common.


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Non-silicate crystalline structures are tetrahedra, isolated, and chains.


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