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 (from Greek νησος nēsos, island), or orthosilicates, have isolated (insular) [SiO4]4− tetrahedra that are connected only by interstitial cations.
- Phenacite group
- Phenacite - Be2SiO4
- Willemite - Zn2SiO4
- Olivine group
- Forsterite - Mg2SiO4
- Fayalite - Fe2SiO4
- Garnet group
- Pyrope - Mg3Al2(SiO4)3
- Almandine - Fe3Al2(SiO4)3
- Spessartine - Mn3Al2(SiO4)3
- Grossular - Ca3Al2(SiO4)3
- Andradite - Ca3Fe2(SiO4)3
- Uvarovite - Ca3Cr2(SiO4)3
- Hydrogrossular - Ca3Al2Si2O8(SiO4)3-m(OH)4m
- Zircon group
- Zircon - ZrSiO4
- Thorite - (Th,U)SiO4
- Al2SiO5 group
- Andalusite - Al2SiO5
- Kyanite - Al2SiO5
- Sillimanite - Al2SiO5
- Dumortierite - Al6.5-7BO3(SiO4)3(O,OH)3
- Topaz - Al2SiO4(F,OH)2
- Staurolite - Fe2Al9(SiO4)4(O,OH)2
- Humite group - (Mg,Fe)7(SiO4)3(F,OH)2
- Norbergite - Mg3(SiO4)(F,OH)2
- Chondrodite - Mg5(SiO4)(F,OH)2
- Humite - Mg7(SiO4)(F,OH)2
- Clinohumite - Mg9(SiO4)(F,OH)2
- Datolite - CaBSiO4(OH)
- Titanite - CaTiSiO5
- Chloritoid - (Fe,Mg,Mn)2Al4Si2O10(OH)4
Sorosilicates[]
Sorosilicates have isolated double tetrahedra groups with (Si2O7)6− or a ratio of 2:7.
- Hemimorphite (calamine) - Zn4(Si2O7)(OH)2·H2O
- Lawsonite - CaAl2(Si2O7)(OH)2·H2O
- Ilvaite - CaFe2+2Fe3+O(Si2O7)(OH)
- Epidote group (has both (SiO4)4− and (Si2O7)6− groups)
- Epidote - Ca2(Al,Fe)3O(SiO4)(Si2O7)(OH)
- Zoisite - Ca2Al3O(SiO4)(Si2O7)(OH)
- Clinozoisite - Ca2Al3O(SiO4)(Si2O7)(OH)
- Tanzanite - Ca2Al3O(SiO4)(Si2O7)(OH)
- Allanite - Ca(Ce,La,Y,Ca)Al2(Fe2+,Fe3+)O(SiO4)(Si2O7)(OH)
- Dollaseite-(Ce) - CaCeMg2AlSi3O11F(OH)
- Vesuvianite (idocrase) - Ca10(Mg,Fe)2Al4(SiO4)5(Si2O7)2(OH)4
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
- Benitoite - BaTi(Si3O9)
- 4-member ring
- Axinite - (Ca,Fe,Mn)3Al2(BO3)(Si4O12)(OH)
- 6-member ring
- Beryl/Emerald - Be3Al2(Si6O18)
- Cordierite - (Mg,Fe)2Al3(Si5AlO18)
- Tourmaline - (Na,Ca)(Al,Li,Mg)3-(Al,Fe,Mn)6(Si6O18)(BO3)3(OH)4
Inosilicates[]
Inosilicates (from Greek ις [genitive: ινος inos], fibre), 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
- Enstatite - MgSiO3
- Ferrosilite - FeSiO3
- Pigeonite - Ca0.25(Mg,Fe)1.75Si2O6
- Diopside - hedenbergite series
- Diopside - CaMgSi2O6
- Hedenbergite - CaFeSi2O6
- Augite - (Ca,Na)(Mg,Fe,Al)(Si,Al)2O6
- Sodium pyroxene series
- Jadeite - NaAlSi2O6
- Aegirine (Acmite) - NaFe3+Si2O6
- Spodumene - LiAlSi2O6
- Enstatite - orthoferrosilite series
- Pyroxenoid group
- Wollastonite - CaSiO3
- Rhodonite - MnSiO3
- Pectolite - NaCa2(Si3O8)(OH)
Double chain inosilicates[]
- Amphibole group
- Anthophyllite - (Mg,Fe)7Si8O22(OH)2
- Cumingtonite series
- Cummingtonite - Fe2Mg5Si8O22(OH)2
- Grunerite - Fe7Si8O22(OH)2
- Tremolite series
- Tremolite - Ca2Mg5Si8O22(OH)2
- Actinolite - Ca2(Mg,Fe)5Si8O22(OH)2
- Hornblende - (Ca,Na)2-3(Mg,Fe,Al)5Si6(Al,Si)2O22(OH)2
- Sodium amphibole group
- Glaucophane - Na2Mg3Al2Si8O22(OH)2
- Riebeckite (asbestos) - Na2Fe2+3Fe3+2Si8O22(OH)2
- Arfvedsonite - Na3(Fe,Mg)4FeSi8O22(OH)2
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
- Antigorite - Mg3Si2O5(OH)4
- Chrysotile - Mg3Si2O5(OH)4
- Lizardite - Mg3Si2O5(OH)4
- 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
- Biotite - K(Mg,Fe)3(AlSi3O10)(OH)2
- Muscovite - KAl2(AlSi3O10)(OH)2
- Phlogopite - KMg3Si4O10(OH)2
- Lepidolite - K(Li,Al)2-3(AlSi3O10)(OH)2
- Margarite - CaAl2(Al2Si2O10)(OH)2
- Glauconite - (K,Na)(Al,Mg,Fe)2(Si,Al)4O10(OH)2
- 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.
- Quartz group
- Quartz - SiO2
- Tridymite - SiO2
- Cristobalite - SiO2
- Feldspar group
- Alkali-feldspars
- Potassium-feldspars
- Microcline - KAlSi3O8
- Orthoclase - KAlSi3O8
- Sanidine - KAlSi3O8
- Anorthoclase - (Na,K)AlSi3O8
- Potassium-feldspars
- Plagioclase feldspars
- Albite - NaAlSi3O8
- Oligoclase - (Na,Ca)(Si,Al)4O8 (Na:Ca 4:1)
- Andesine - (Na,Ca)(Si,Al)4O8 (Na:Ca 3:2)
- Labradorite - (Na,Ca)(Si,Al)4O8 (Na:Ca 2:3)
- Bytownite - (Na,Ca)(Si,Al)4O8 (Na:Ca 1:4)
- Anorthite - CaAl2Si2O8
- Alkali-feldspars
- Feldspathoid group
- Nosean - Na8Al6Si6O24(SO4)
- Cancrinite - Na6Ca2(CO3,Al6Si6O24).2H2O
- Leucite - KAlSi2O6
- Nepheline - (Na,K)AlSiO4
- Sodalite - Na8(AlSiO4)6Cl2
- Hauyne - (Na,Ca)4-8Al6Si6(O,S)24(SO4,Cl)1-2
- Lazurite - (Na,Ca)8(AlSiO4)6(SO4,S,Cl)2
- Petalite - LiAlSi4O10
- Scapolite group
- Marialite - Na4(AlSi3O8)3(Cl2,CO3,SO4)
- Meionite - Ca4(Al2Si2O8)3(Cl2CO3,SO4)
- Analcime - NaAlSi2O6•H2O
- Zeolite group
- Natrolite - Na2Al2Si3O10•2H2O
- Chabazite - CaAl2Si4O12•6H2O
- Heulandite - CaAl2Si7O18•6H2O
- Stilbite - NaCa2Al5Si13O36•17H2O
References[]
- Deer, W.A.; Howie, R.A., & Zussman, J. (1992). An introduction to the rock-forming minerals (2nd ed.). London: Longman. ISBN 0582300940.
- 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 ed.). London: Geological Society of London. p. 982 pp.
- Hurlbut, Cornelius S. (1966). Dana's Manual of Mineralogy (17th ed.). ISBN 0-471-03288-3.
- Hurlbut, Cornelius S.; Klein, Cornelis (1985). Manual of Mineralogy (20th ed.). Wiley. ISBN 0-471-80580-7.
External links[]
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