Silicate Minerals Article Index for
Silicate
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Silicate Minerals




Subclasses:

NESOSILICATES OR ISOSILICATES

''Nesosilicates'' (or ''orthosilicates'') have isolated {Link without Title} 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'', 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

  • --- 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'', 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:



Double chain inosilicates:



PHYLLOSILICATES

''Phyllosilicates'', sheet silicates (from Greek φύλλον ''phyllon'', leaf), form parallel sheets of silicate tetrahedra with Si2O5 or a 2:5 ratio.



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 Aluminosilicate s.

]]
Ferroan Anorthosite #60025 ( Plagioclase Feldspar). Collected by Apollo 16 from the Lunar Highlands near Descartes Crater . ]]



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