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Silicate minerals

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The silicate minerals make up the largest and most important class of rock-forming minerals. They are classified based on the structure of their silicate ion group.

Subclasses:

Contents

[edit] Nesosilicates

Nesosilicates (or orthosilicates) have SiO4 tetrahedra that are isolated and connected by interstitial cations.

[edit] Sorosilicates

Sorosilicates have isolated double tetrahedra groups with Si2O7 or a ratio of 2:7.

[edit] Cyclosilicates

Cyclosilicates, ring silicates, have linked tetrahedra with SixO3x or a ratio of 1:3.

[edit] Inosilicates

Inosilicates, chain silicates, have interlocking chains of silicate tetrahedra with either SiO3, 1:3 ratio, for single chains or Si4O11, 4:11 ratio, for double chains.

[edit] Single chain inosilicates:

[edit] Double chain inosilicates:

[edit] Phyllosilicates

Phyllosilicates, sheet silicates, form parallel sheets of silicate tetrahedra with Si2O5 or a 2:5 ratio.

[edit] Tectosilicates

Tectosilicates, or "framework silicates", have a three-dimensional framework of silicate tetrahedra with SiO2 or a 1:2 ratio. This is the largest group, comprising nearly 75% of the crust of the Earth.

[edit] References and external links

fr:Pyroxénoïde he:מינרלים סיליקטיים hr:Silikati lv:Silikātu minerāls lt:Silikatai pt:Silicato (minerais) fi:Silikaattimineraali sv:Silikatmineral

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