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- W128633689 abstract "A limited degree of solid solution in a partially-ordered lM micaceous mineral has been inferred from results of XRD, TG, IRA and TEM on samples of bulk composition varying between muscovite (KAl3Si3) and pyrophyllite (Al2Si4). Illite is the term that may be used, in a restricted sense, for the end-member of the series with a composition of about K0.8Al2(Si3.2Al0.8)O10(OH)2xH2O, although it is not intended to limit the use of the term illite to aluminous micaceous minerals only. It has a b cell dimension of 8.97å, which is more similar to that of K-saturated beidellite (8.95å) than to that of synthetic muscovite (9.00å). Compositions more pyrophyllite-rich than 80% muscovite contain illite-beidellite interstratifications. We think that the similarity of cell dimensions between illite and beidellite may be necessary for interlayering to occur between them and that it is the higher Si and lower K content of illite compared to muscovite that controls this small but important change in cell dimensions." @default.
- W128633689 created "2016-06-24" @default.
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- W128633689 date "1979-01-01" @default.
- W128633689 modified "2023-09-25" @default.
- W128633689 title "Synthetic Illite in the Chemical System K2O-Al2O3-SiO2-H2O at 300°C and 2Kb" @default.
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- W128633689 doi "https://doi.org/10.1016/s0070-4571(08)70736-2" @default.
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