Fillosilikaat: Verskil tussen weergawes

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k Naudefj het bladsy Filo-silikate na Filosilikaat oor 'n aanstuur geskuif
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Lyn 27: Lyn 27:
** [[Chloriet]] – (Mg,Fe)<sub>3</sub>(Si,Al)<sub>4</sub>O<sub>10</sub>(OH)<sub>2</sub>·(Mg,Fe)<sub>3</sub>(OH)<sub>6</sub>
** [[Chloriet]] – (Mg,Fe)<sub>3</sub>(Si,Al)<sub>4</sub>O<sub>10</sub>(OH)<sub>2</sub>·(Mg,Fe)<sub>3</sub>(OH)<sub>6</sub>


==Verwysings==
== Verwysings ==
*{{Cite book
* {{Cite book
| last = Deer
| last = Deer
| first = W.A.
| first = W.A.
|author2=Howie, R.A. |author3=Zussman, J.
|author2=Howie, R.A. |author3=Zussman, J.
| year = 1992
| year = 1992
| title = [[An introduction to the rock-forming minerals]]
| title = [[An introduction to the rock-forming minerals]]
Lyn 40: Lyn 40:
}}
}}


*{{Cite book
* {{Cite book
| last = Deer
| last = Deer
| first = W.A. |author2=Howie, R.A. |author3=Wise, W.S. |author4=Zussman, J.
| first = W.A. |author2=Howie, R.A. |author3=Wise, W.S. |author4=Zussman, J.
Lyn 51: Lyn 51:
}}
}}


*{{Cite book
* {{Cite book
| last = Hurlbut
| last = Hurlbut
| first = Cornelius S.
| first = Cornelius S.
Lyn 60: Lyn 60:
}}
}}


*{{Cite book
* {{Cite book
| last = Hurlbut
| last = Hurlbut
| first = Cornelius S.
| first = Cornelius S.
Lyn 71: Lyn 71:
}}
}}


*[http://www.mindat.org/dana.php Mindat.org, Dana classification]
* [http://www.mindat.org/dana.php Mindat.org, Dana classification]
*[http://webmineral.com/dana/8_Silicates.shtml Webmineral : Dana's New Silicate Classification]
* [http://webmineral.com/dana/8_Silicates.shtml Webmineral : Dana's New Silicate Classification]


{{Silikaat}}
==Sien ook==
*[[Silikaatminerale]]
*[[Sorosilikaat]]
*[[Tekto-silikate]]
*[[Siklo-silikate]]
*[[Neso-silikate]]
*[[Ino-silikate]]


[[Kategorie:Silikaatminerale]]
[[Kategorie:Silikaatminerale]]

Wysiging soos op 11:05, 15 Augustus 2017

Filo-silikate (vanaf die Grieks φύλλον phyllon, blaar), vorm paralelle velle (blaaie) van silikaat tetraeders. Hierdie tetraeders vorm 'n 2-dimensionele raamwerk, waar die individuele tetraeders met mekaar verbind is. In hierdie 2-dimensionele raamwerk of vel, is die bindings tussen die tetraeders sterk, maar die bindings tussen die verskillende velle is swak, aangesien die SiO trtraeders nie tussen velle met mekaar verbind is nie. Die Si:O verhouding is Si2O5 of a 2:5.

Nickel–Strunz classification: 09.E. Alle Filo-silikate is gehidreer met of water of hidroksiel groepe aangeheg.

Verwysings

  • Deer, W.A.; Howie, R.A.; Zussman, J. (1992). An introduction to the rock-forming minerals (2nd uitg.). London: Longman. ISBN 0-582-30094-0.
  • 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 uitg.). London: Geological Society of London. p. 982 pp.
  • Hurlbut, Cornelius S. (1966). Dana's Manual of Mineralogy (17th uitg.). ISBN 0-471-03288-3.
  • Hurlbut, Cornelius S.; Klein, Cornelis (1985). Manual of Mineralogy (20th uitg.). Wiley. ISBN 0-471-80580-7.
Silikate

Nesosilikaat -- Inosilikaat -- Sorosilikaat -- Siklosilikaat -- Tektosilikaat -- Filosilikaat

  Silica