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Silicate minerals

From Biocrawler, the free encyclopedia.

The silicate minerals make up the the largest and most important class of rock-forming minerals. They are classified based on the structure of their silicate anion group.

Subclasses:

Contents

Nesosilicates

Nesosilicates (or orthosilicates) have SiO4 tetrahedra that are isolated and connected by interstitial cations.

Sorosilicates

Sorosilicates have isolated double tetrahedra groups with Si2O7 or a ratio of 2:7.

Cyclosilicates

Cyclosilicates, ring silicates, have linked tetrahedra with SixO3x or a ratio of 1:3.

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, form parallel sheets of silicate tetrahedra with Si2O5 or a 2:5 ratio.

Tectosilicates

Tectosilicates, framework silicates, have a three dimensional framework of silicate tetrahedra with SiO2 or a 1:2 ratio. This is the largest group comprising nearly 75% of the crust of the Earth.

References and external links

Wikipedia (http://en.wikipedia.org/wiki/Main_Page) Silicate_minerals (http://en.wikipedia.org/wiki/Silicate_minerals) version history (http://en.wikipedia.org/w/index.php?title=Silicate_minerals&action=history) GNU Free Documentation Lizenz (http://en.wikipedia.org/wiki/Wikipedia:Text_of_the_GNU_Free_Documentation_License) CC-by-sa (http://creativecommons.org/licenses/by-sa/2.5/)

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