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Silicate minerals are rock-forming minerals made up of silicate groups. They are the largest and most important class of minerals and make up approximately 90 percent of Earth's crust.
The analysis highlights Art, Nesosilicates or orthosilicates and Inosilicates as prominent areas in the source structure around Silicate mineral.
Source areas are shown by the number of related topics found in each part of the analysis. Use smaller areas too: they can reveal specialized angles and content gaps.
Smaller areas are not necessarily less important. They contain fewer connections in this analysis and can be useful for finding specialized angles or coverage gaps.
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The extracted context around Silicate mineral shows recurring relationship patterns in the source. For example, Silicate mineral → Al, Al10Si35O90, Al2Si4O12, Al2Si6O16, Al4Si4O16, Al6, Al6Si6O24, Al7Si17O48, Al8, Al8Si40, AlSi2O6, AlSi3O8Sanidine, Andesine, Anorthite, Ba, BaAl2Si2O8Hyalophane, BeAlSi4O12, Bytownite, Ca, Ca1 Another extracted example is Silicate mineral → Ajoite, Al, Al2, Al2Mg2, Al2Si2, Al2Si2O10, Al2Si2O5, Al2Si4O10, Al2SiO3, AlSi3, AlSi3O10, AlSiO5, Ca, Ca0, Ca10Si18O46, Ca2ThSi8O20Gyrolite, CaAl2, CaAlMg2, Chamosite, Chlorite. Use these groups to spot repeated connection types before inspecting the individual relationships.
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silicate minerals tetrahedra silica classification silicon double nickel strunz tectosilicates cations earth al si oh group single groups silicates na
TTTA extracted 200 structured relationships around Silicate mineral. Examples in this analysis include aluminum → instance of → Tectosilicates can only have additional cations if some of the silicon is replaced by an atom of lower valence and Silicate mineral → related to General structure → SiO2. The table shows each extracted connection, where it came from and its confidence.
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| aluminum | instance of | Tectosilicates can only have additional cations if some of the silicon is replaced by an atom of lower valence | 0.80 | text |
| Silicate mineral | related to General structure | SiO2 | 0.60 | section |
| Silicate mineral | related to General structure | Although | 0.60 | section |
| Silicate mineral | related to General structure | Balancing | 0.60 | section |
| Silicate mineral | related to General structure | Mx | 0.60 | section |
| Silicate mineral | related to General structure | Typical | 0.60 | section |
| Silicate mineral | related to General structure | Mg2 | 0.60 | section |
| Silicate mineral | related to General structure | Fe2 | 0.60 | section |
| Silicate mineral | related to General structure | Na | 0.60 | section |
| Silicate mineral | related to General structure | The Si-O-M | 0.60 | section |
| Silicate mineral | related to General structure | Silicate | 0.60 | section |
| Silicate mineral | related to Main groups | Tectosilicates | 0.60 | section |
The concept neighborhoods around Silicate mineral bring nearby vocabulary together. In this analysis, examples include Major, Earth and Quartz. Use the clusters to find adjacent concepts and terminology that may deserve separate research.
For Silicate mineral, one of the stronger structural bridges in this analysis connects Silicate mineral with Tectosilicates. Bridges highlight paths between different parts of the map and can reveal research angles that are easy to miss in a flat list.
TTTA analyzes the structure around Silicate mineral to surface related topics, entities, relationships, concept neighborhoods and bridge connections. Use the map to explore areas such as Art, Nesosilicates or orthosilicates & Inosilicates, including less central topics that may reveal useful research gaps. Automatically extracted connections are research leads rather than rewritten encyclopedia content.
Source: Wikipedia — Silicate mineral · EN edition · Analysis: TopicsToTalkAbout
