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Everything about The Silicate Minerals totally explained

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. Silicate minerals all contain silicon and oxygen.

Subclasses:

Nesosilicates or Isosilicates

Nesosilicates (or orthosilicates) have isolated [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.
  • 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
  • Pyroxenoid group

    Double chain inosilicates

  • 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

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