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Staples, Lloyd W., Gard, J. A. (1959) The fibrous zeolite erionite; its occurrence, unit cell, and structure. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (247) 261-281 doi:10.1180/minmag.1959.032.247.01

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Reference TypeJournal (article/letter/editorial)
TitleThe fibrous zeolite erionite; its occurrence, unit cell, and structure
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsStaples, Lloyd W.Author
Gard, J. A.Author
Year1959 (December)Volume32
Issue247
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_32/32-247-261.pdf+
DOIdoi:10.1180/minmag.1959.032.247.01
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Mindat Ref. ID5533Long-form Identifiermindat:1:5:5533:2
GUID0
Full ReferenceStaples, Lloyd W., Gard, J. A. (1959) The fibrous zeolite erionite; its occurrence, unit cell, and structure. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (247) 261-281 doi:10.1180/minmag.1959.032.247.01
Plain TextStaples, Lloyd W., Gard, J. A. (1959) The fibrous zeolite erionite; its occurrence, unit cell, and structure. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (247) 261-281 doi:10.1180/minmag.1959.032.247.01
In(1959) Mineralogical Magazine Vol. 32 (247) Mineralogical Society
Abstract/NotesSummaryThe type locality for erionite has been identified and specimens compared with Eakle's original material. New determinations of the physical properties and a chemical analysis have been made. Correlation of X-ray powder and fibre rotation data with electron diffraction of single crystals has shown that the unit cell is hexagonal with a 13·26, c 15·12 Å., space-group P31c, P¯31c, P63mc, P¯62c, or P63/mmc, giving a calculated sp. Gr. of 2·07 and atomic cell contents (Ca, Mg, Na2, K2)4·5Al9Si27O72.27H2O. A structure is proposed for the aluminosilicate frame, with space-group P63/mmc, which gives satisfactory correlation between observed and calculated structure factors for the X-ray fibre rotation pattern.


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