Examples of kaolinite

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The clays are dominantly smectite with some illite and kaolinite.
Other clay minerals identified were illite and kaolinite.
For soil type, a positive parameter indicates an association with kaolinite.
It turns out that clay (montmorillonite/kaolinite) adsorbed nucleic acid undergoes less radiation damage than free nucleic acid.
The clay mineral spectrum is dominated by smectite; illite and kaolinite occur infrequently.
Mineral assemblages are dominated by illite followed by chlorite, often with minor amounts of smectite and/or kaolinite, and exceptionally paragonite.
The clay fraction of these samples comprises more or less equal proportions of kaolinite and mixed-layers illite-smectite.
Within the clay fraction, kaolinite, mixed-layers illite-smectite and illite are present in relevant proportions.
The latter (< 2 m) includes interstratified illite-smectite, illite and rare kaolinite.
Crystals of euhedral sanidine and marginally corroded plagioclase reach up to 500 m in size and are usually extensively altered to kaolinite.
As indicated by the reflections, there is very little difference in relative abundance of kaolinite and metahalloysite between the control samples and the ingested samples.
Soils are ferralitic and rich in kaolinite and iron oxides.
Kaolinite, chlorite and sericite are the secondary minerals.
Prehnite and kaolinite are seen as secondary products of plagioclases.
Said et al. (1980) showed that kaolinite could absorb bacteria and their toxins.
Carbonate, especially calcite, is present throughout the sediments, and the clay fraction includes variable portions of chlorite, kaolinite, illite and mixed layers illite-smectite.
Dolomite crystals occur suspended within kaolin, but also encapsulate kaolinite crystals, indicating coeval precipitation.

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