Silicate minerals
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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.
Nesosilicates or orthosilicates
Nesosilicates, or orthosilicates, have isolated (insular) [SiO4]4− tetrahedra that are connected only by interstitial cations.
Sorosilicates
Sorosilicates have isolated double tetrahedra groups with (Si2O7)6− or a ratio of 2:7.
Cyclosilicates
Cyclosilicates, or ring silicates, have linked tetrahedra with (SixO3x)2x- or a ratio of 1:3. These exist as 3-member (Si3O9)6-, 4-member (Si4O12)8- and 6-member (Si6O18)12- rings.
- 3-member ring
- 4-member ring
- Axinite - (Ca,Fe,Mn)3Al2(BO3)(Si4O12)(OH)
- 6-member ring
Inosilicates
Inosilicates, 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.
Single chain inosilicates
- Pyroxene group
- Enstatite - orthoferrosilite series
- Pigeonite - Ca0.25(Mg,Fe)1.75Si2O6
- Diopside - hedenbergite series
- Sodium pyroxene series
- Spodumene - LiAlSi2O6
- Pyroxenoid group
Double chain inosilicates
- Amphibole group
- Anthophyllite - (Mg,Fe)7Si8O22(OH)2
- Cumingtonite series
- Tremolite series
- Hornblende - (Ca,Na)2-3(Mg,Fe,Al)5Si6(Al,Si)2O22(OH)2
- Sodium amphibole group
Phyllosilicates
Phyllosilicates (from Greek φύλλον phyllon, leaf), or sheet silicates, form parallel sheets of silicate tetrahedra with Si2O5 or a 2:5 ratio.
- Serpentine group
- Clay mineral group
- Halloysite - Al2Si2O5(OH)4
- Kaolinite - Al2Si2O5(OH)4
- Illite - (K,H3O)(Al,Mg,Fe)2(Si,Al)4O10[(OH)2,(H2O)]
- Montmorillonite - (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2·nH2O
- Vermiculite - (MgFe,Al)3(Al,Si)4O10(OH)2·4H2O
- Talc - Mg3Si4O10(OH)2
- Palygorskite - (Mg,Al)2Si4O10(OH)·4(H2O)
- Pyrophyllite - Al2Si4O10(OH)2
- Mica group
- Chlorite group
- Chlorite - (Mg,Fe)3(Si,Al)4O10(OH)2•(Mg,Fe)3(OH)6
Tectosilicates
Tectosilicates, 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.
References
- Deer, W.A.; Howie, R.A., & Zussman, J. (1992). An introduction to the rock forming minerals (2nd edition ed.). London: Longman.
- Deer, W.A.; Howie, R.A., Wise, W.S. & Zussman, J. (2004). Rock-forming minerals. Volume 4B. Framework silicates: silica minerals. Feldspathoids and the zeolites (2nd edition ed.). London: Geological Society of London. p. 982 pp.
- Hurlbut, Cornelius S. (1966). Dana's Manual of Mineralogy (17th edition ed.). ISBN 0-471-03288-3.
- Hurlbut, Cornelius S.; Klein, Cornelis (1985). Manual of Mineralogy (20th edition ed.). Wiley. ISBN 0-471-80580-7.
External links
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