Linked from

The 37 pages that link to Solid solution, each with the reason it gives.

• OlivineRelated: Magnesium and iron substitute for one another across olivine’s main compositional series.

• FeldsparRelated: Feldspar series form as potassium, sodium, and calcium vary in compatible structures.

• Bowen's reaction seriesRelated: Plagioclase's sodium-calcium substitution is what makes its branch continuous.

• PlagioclaseRelated: Substitution of sodium and silicon for calcium and aluminum allows plagioclase compositions between its end-members.

• PyroxeneRelated: Magnesium, iron, calcium, and other elements substitute across many pyroxene compositions.

• Eutectic systemRelated: Whether solid phases form solutions or separate compounds shapes eutectic diagrams.

• Iron–carbon phase diagramRelated: Ferrite and austenite are iron-based solid solutions with different carbon solubilities.

• ApatiteRelated: Apatite forms compositional series rather than only perfectly pure end-members.

• AmphiboleRelated: Element substitutions create much of amphibole’s compositional diversity.

• Mineral speciesRelated: Substitution can vary composition without necessarily creating a different species.

• Alkali feldsparRelated: Potassium and sodium substitute across much of the alkali-feldspar composition range.

• PerthiteRelated: High-temperature alkali feldspar can accommodate sodium and potassium before they separate.

• ActinoliteRelated: Magnesium and iron substitute for one another in actinolite’s principal compositional series.

• DiopsideRelated: Diopside forms compositional series as magnesium and iron substitute for one another.

• HornblendeRelated: Substitution among iron, magnesium, calcium, and other elements produces varied hornblende chemistry.

• Phosphate mineralRelated: Ion substitution creates continuous compositional variation in several phosphate mineral groups.

• AugiteRelated: Element substitutions let augite vary in composition without changing its basic structure.

• CobaltiteRelated: Iron can substitute for cobalt in natural cobaltite compositions.

• EnstatiteRelated: Iron can replace magnesium in enstatite’s crystal structure, producing compositions along the orthopyroxene series.

• HedenbergiteRelated: Iron and magnesium can exchange in pyroxene structures without changing the basic mineral framework.

• RhodochrositeRelated: Iron, calcium, and magnesium can substitute for manganese in natural rhodochrosite.

• SodaliteRelated: Substitution among framework and cage occupants accounts for compositional variation in sodalite.

• Spinel groupRelated: Element substitution links many compositions within the spinel group.

• TantaliteRelated: Iron, manganese, niobium, and tantalum vary through substitution in tantalite.

• ConstantanRelated: Copper and nickel can form a continuous solid solution across their compositions.

• PigeoniteRelated: Magnesium and iron substitute extensively in pigeonite’s crystal lattice.

• ThorianiteRelated: Thorianite accommodates compositional variation through substitutions in its lattice.

• AllaniteRelated: Substitution produces compositional variation across allanite species.

• CummingtoniteRelated: Iron and magnesium substitute across cummingtonite’s compositional range.