Linked from

The 11 pages that link to Isomorphous substitution, each with the reason it gives.

• Silicate mineralRelated: Such substitutions let aluminum and other elements enter silicate structures.

• Clay mineralRelated: Substitution creates much of the permanent negative charge on many clay-mineral layers.

• MicaRelated: Substitutions within mica layers create charge that is balanced by interlayer cations.

• AluminosilicateRelated: Aluminum commonly replaces silicon in tetrahedral sites, changing framework charge.

• PhyllosilicateRelated: Substitutions such as aluminum for silicon create much of the layer charge.

• ApatiteRelated: Apatite's anion channels allow fluorine, chlorine, and hydroxyl to substitute for one another.

• Chlorite groupRelated: Substitutions among iron, magnesium, aluminum, and other cations create chlorite compositional variation.

• FluorapatiteRelated: Fluoride can occupy apatite's anion sites in place of hydroxide or chloride.

• BiotiteRelated: Substitutions among iron, magnesium, aluminum, and other ions create biotite’s compositional range.

• EpidoteRelated: Iron substitutes for aluminium in epidote, creating compositional variation within the species.

• HectoriteRelated: Lithium-for-magnesium substitution creates the charge imbalance characteristic of hectorite.