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- Kaolinite - Wikipedia
Kaolinite is a soft, earthy, usually white, mineral (dioctahedral phyllosilicate clay), produced by the chemical weathering of aluminium silicate minerals like feldspar It has a low shrink–swell capacity and a low cation-exchange capacity (1–15 meq 100 g)
- Kaolinite Properties, Occurrence and Uses Area - Geology Science
Kaolinite, common group of clay minerals that are hydrated aluminum silicates; they contain the main components of kaolin (china clay) The group includes kaolinite, which is chemically similar but amorphous to kaolinite, and its rarer forms, stalagmite and nacrite, halloysite and allophane
- Kaolinite: Mineral information, data and localities.
Kaolinite, by name, was known since the Yuan (Mongol) dynasty in the thirteenth century as "Kaolin earth" and was first properly described by Song Yingxing in 1637 in his book Tian Gong Kai Wu (translated: "Introduction to Heaven's Handicrafts" or "The Exploitation of the Works of Nature")
- Kaolinite | Clay Mineral, Aluminium Silicate, Hydrated . . .
Kaolinite, group of common clay minerals that are hydrous aluminum silicates; they comprise the principal ingredients of kaolin (china clay) The group includes kaolinite and its rarer forms, dickite and nacrite, halloysite, and allophane, which are chemically similar to kaolinite but amorphous
- Kaolinite Mineral Data
Secondary mineral derived from the wathering of alumino-silicate minerals Kao-Ling, China Link to MinDat org Location Data Named after the locality Comments: Authigenic kaolinite plates covering a quartz grain overgrown with authigenic quartz SEM image of a core sample Location: Unknown Scale: Picture size 50 µ-m
- Kaolinite - Minerals Education Coalition
Kaolinite is a layered silicate clay mineral which forms from the chemical weathering of feldspar or other aluminum silicate minerals It is usually white, with occasionally a red color impurity due to iron oxide, or blue or brown from other minerals
- Kaolinite – Virtual Museum of Molecules and Minerals
Kaolinite is a common 1:1 dioctahedral phyllosilicate (clay) mineral found in soils across the world, particularly in highly-weathered environments, as well as scattered monomineralic deposits that are mined for industry
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