
Also known as smectite, smectite group
thumb|Scanning electron microscope (SEM) photograph of smectite clay – magnification 23,500 – [[U.S. Geological Survey – Tuckup Canyon]] thumb|Typical cracks pattern of a smectite-rich bentonite after its desiccation and shrinkage
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thumb|Scanning electron microscope (SEM) photograph of smectite clay – magnification 23,500 – [[U.S. Geological Survey – Tuckup Canyon]] thumb|Typical cracks pattern of a smectite-rich bentonite after its desiccation and shrinkage
A smectite (; ; ) is a mineral mixture of various swelling sheet silicates (phyllosilicates), which have a three-layer 2:1 (TOT) structure and belong to the clay minerals. Smectites mainly consist of montmorillonite, but can often contain secondary minerals such as quartz and calcite.
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Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).