Linked from

The 59 pages that link to Silicate mineral, each with the reason it gives.

• QuartzNarrower topic: Quartz shares silicon and oxygen chemistry with silicates but has a distinct framework structure.

• SiliconNarrower topic: Most crustal silicon occurs bound in this broad family rather than as pure element.

• Interstellar dustRelated: Silicate grains produce characteristic infrared features in interstellar spectra.

• Igneous rockNarrower topic: Most igneous rocks are dominated by minerals in this broad family.

• Chemical weatheringNarrower topic: Silicates dominate Earth's crust and are frequent targets of chemical weathering.

• Planetary differentiationRelated: Silicate chemistry determines the composition of the rocky layers left above a metallic core.

• GlassRelated: Their tetrahedral units also form the structural basis of silicate glass.

• MineralogyBroader topic: Silicates dominate Earth’s crust and illustrate structural diversity in minerals.

• OlivineNarrower topic: Olivine belongs to this broad mineral family, but has an unusually isolated tetrahedral structure.

• Silicon dioxideNarrower topic: Silicon dioxide is the simplest end-member composition within the broader silicate family.

• Clay mineralNarrower topic: Clay-mineral crystal frameworks are built from linked silicon–oxygen units.

• Hydrothermal alterationNarrower topic: Many common rock-forming minerals are silicates that hydrothermal fluids replace or transform.

• ZeoliteNarrower topic: Zeolites belong to the broad mineral class built from silicate frameworks.

• Bowen's reaction seriesRelated: Every mineral in the series is a silicate with a different polymerized structure.

• MicaNarrower topic: Mica’s chemistry and crystal structure place it among silicate minerals.

• PlagioclaseNarrower topic: Plagioclase belongs to the largest mineral class, built around linked silicate tetrahedra.

• PyroxeneNarrower topic: Pyroxene belongs to this broad mineral class because its structure is built from silica tetrahedra.

• LateriteRelated: Weathering of silicate minerals releases constituents that are selectively removed or retained in laterite.

• AluminosilicateNarrower topic: Aluminosilicates are a major family within silicate minerals.

• PhyllosilicateNarrower topic: Phyllosilicates are one structural class within the silicate minerals.

• PumiceNarrower topic: Pumice’s composition is largely silicate glass, whose chemistry varies with the magma.

• SiliconeCompared with: Silicates share silicon–oxygen chemistry but are not silicone polymers.

• Lunar magma oceanRelated: Silicate minerals made up most of the molten lunar material and its crystallized products.

• MoonstoneNarrower topic: Feldspars, including moonstone, belong to this broad mineral family.

• Silicate weatheringNarrower topic: They are the broad mineral family whose weathering defines this process.

• InosilicateNarrower topic: Inosilicates are one structural family within this broad mineral group.

• TalcNarrower topic: Talc’s magnesium and hydroxyl groups are arranged around a silicate framework.

• Cosmic dustRelated: Silicates make up a major component of cosmic grains and leave diagnostic infrared features.

• Igneous petrologyNarrower topic: Most igneous rocks consist chiefly of silicate minerals.

• Silicon–oxygen tetrahedronNarrower topic: The tetrahedron is the single unit from which every silicate mineral is assembled.

• AnorthiteNarrower topic: Anorthite’s framework is built from linked silicon–oxygen and aluminum–oxygen tetrahedra.

• James Dwight DanaRelated: Their structural variety made silicates central to Dana’s mineral classification.

• Mantle viscosityRelated: The mantle's dominant silicate minerals deform to produce its long-term flow.

• MuscoviteNarrower topic: Muscovite’s framework is built from linked silicon–oxygen tetrahedra.

• DiopsideNarrower topic: Diopside’s structure is built from linked silicon-oxygen tetrahedra.

• Egyptian blueNarrower topic: Cuprorivaite belongs to the broad mineral family built around silicate structures.

• HornblendeNarrower topic: Hornblende’s framework is made from linked silicon–oxygen tetrahedra.

• Oxide mineralCompared with: Silicates contain oxygen too, but their defining structural units include silicon.

• Phosphate mineralCompared with: Silicate minerals use silicon–oxygen units where phosphate minerals use phosphorus–oxygen units.

• TourmalineNarrower topic: Tourmaline belongs to this broad mineral class, whose structural units form its crystal framework.

• AugiteNarrower topic: Augite’s structure belongs to the largest mineral class in Earth’s crust.

• BiotiteNarrower topic: Biotite belongs to the largest and most diverse mineral class.

• PetaliteNarrower topic: Petalite's framework is built from linked silicon–oxygen and aluminum–oxygen units.

• EnstatiteNarrower topic: Enstatite’s silicate chains link silicon and oxygen atoms through its crystal structure.

• FeldspathoidNarrower topic: Feldspathoids are framework silicates, a structural family within this broader mineral group.

• ForsteriteNarrower topic: Forsterite belongs to the dominant mineral class in Earth’s crust and mantle.

• Carbon planetCompared with: Their abundance on Earth illustrates the oxygen-rich mineralogy carbon planets might lack.

• FayaliteNarrower topic: Fayalite’s structure is built from isolated silicon–oxygen tetrahedra.

• Goldschmidt classificationRelated: Silicate minerals host many lithophile elements in planetary mantles and crusts.

• StauroliteNarrower topic: Staurolite belongs to this broad mineral group, whose structures shape its composition.