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Silicate minerals Totally Explained
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Everything about The Silicate Minerals totally explainedThe 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. Silicate minerals all contain silicon and oxygen.
Subclasses:
Nesosilicates or Isosilicates
Nesosilicates (or orthosilicates) have isolated [SiO 4] 4−
tetrahedra that are connected only by interstitial cations.
Sorosilicates
Sorosilicates have isolated double tetrahedra groups with (Si 2O 7) 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)
Vesuvianite (idocrase) - Ca10(Mg,Fe)2Al4(SiO4)5(Si2O7)2(OH)4
Cyclosilicates
Cyclosilicates, 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.
3-member ring
4-member ring
- Axinite - (Ca,Fe,Mn)3Al2(BO3)(Si4O12)(OH)
6-member ring
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.
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, sheet silicates (from Greek φύλλον phyllon, leaf), form parallel sheets of silicate tetrahedra with Si2O5 or a 2:5 ratio.
Serpentine group
Clay mineral group
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.
Quartz group
Feldspar group
References
Further Information
Get more info on 'Silicate Minerals'.
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