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The silicate minerals make up the largest and most important class of rock-forming minerals, constituting approximately 90 percent of the crust of the Earth. They are classified based on the structure of their silicate group. Silicate minerals all contain silicon and oxygen.
[edit] Nesosilicates or orthosilicatesNesosilicates, or orthosilicates, have isolated (insular) [SiO4]4− tetrahedra that are connected only by interstitial cations.
Kyanite crystals (unknown scale)
[edit] SorosilicatesSorosilicates have isolated double tetrahedra groups with (Si2O7)6− or a ratio of 2:7.
[edit] CyclosilicatesCyclosilicates, or ring silicates, have linked tetrahedra with (SixO3x)2x- or a ratio of 1:3. These exists as 3-member (Si3O9)6-, 4-member (Si4O12)8- and 6-member (Si6O18)12- rings.
[edit] InosilicatesInosilicates, or 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] PhyllosilicatesPhyllosilicates (from Greek φύλλον phyllon, leaf), or sheet silicates, form parallel sheets of silicate tetrahedra with Si2O5 or a 2:5 ratio.
[edit] TectosilicatesTectosilicates, or "framework silicates", have a three-dimensional framework of silicate tetrahedra with SiO2 or a 1:2 ratio. This group comprises nearly 75% of the crust of the Earth. Tectosilicates, with the exception of the quartz group, are aluminosilicates. Lunar Ferroan Anorthosite #60025 (Plagioclase Feldspar). Collected by Apollo 16 from the Lunar Highlands near Descartes Crater.
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