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Taylor, D. (1989) Thermal decomposition of Li8(Al6Si6O24)Cl2. Mineralogical Magazine, 53 (371) 380-382 doi:10.1180/minmag.1989.053.371.15

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Reference TypeJournal (article/letter/editorial)
TitleThermal decomposition of Li8(Al6Si6O24)Cl2
JournalMineralogical MagazineISSN0026-461X
AuthorsTaylor, D.Author
Year1989 (June)Volume53
Issue371
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_53/53-371-380.pdf+
DOIdoi:10.1180/minmag.1989.053.371.15Search in ResearchGate
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Mindat Ref. ID1517Long-form Identifiermindat:1:5:1517:6
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Full ReferenceTaylor, D. (1989) Thermal decomposition of Li8(Al6Si6O24)Cl2. Mineralogical Magazine, 53 (371) 380-382 doi:10.1180/minmag.1989.053.371.15
Plain TextTaylor, D. (1989) Thermal decomposition of Li8(Al6Si6O24)Cl2. Mineralogical Magazine, 53 (371) 380-382 doi:10.1180/minmag.1989.053.371.15
In(1989, June) Mineralogical Magazine Vol. 53 (371) Mineralogical Society
Abstract/NotesLi8(Al6Si6O24)Cl2, a synthetic member of the sodalite family (Henderson and Taylor, 1977), was prepared by heating natural sodalite, Na8(Al- 6Si6O24)Cl2 (from Låven, Norway), in molten LiC1 at 800 °C for 2h, washing uncombined LiC1 from the product and drying at 110 °C Chemical analyses of the natural sodalite and the Li-sodalite are given in Table 1. The cell edge of the Lisodalite was 8.4476(9) Å (Si as internal standard: a = 5.43065/Å at 25 °C in good agreement with literature values (Henderson and Taylor, 1977).


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