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Gellens, L. R., Price, G. D., Smith, J. V. (1982) The structural relation between svetlozarite and dachiardite. Mineralogical Magazine, 45 (337) 157-161 doi:10.1180/minmag.1982.045.337.18

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Reference TypeJournal (article/letter/editorial)
TitleThe structural relation between svetlozarite and dachiardite
JournalMineralogical MagazineISSN0026-461X
AuthorsGellens, L. R.Author
Price, G. D.Author
Smith, J. V.Author
Year1982Volume45
Issue337
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_45/45-337-157.pdf+
DOIdoi:10.1180/minmag.1982.045.337.18Search in ResearchGate
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Mindat Ref. ID3328Long-form Identifiermindat:1:5:3328:6
GUID0
Full ReferenceGellens, L. R., Price, G. D., Smith, J. V. (1982) The structural relation between svetlozarite and dachiardite. Mineralogical Magazine, 45 (337) 157-161 doi:10.1180/minmag.1982.045.337.18
Plain TextGellens, L. R., Price, G. D., Smith, J. V. (1982) The structural relation between svetlozarite and dachiardite. Mineralogical Magazine, 45 (337) 157-161 doi:10.1180/minmag.1982.045.337.18
In(1982) Mineralogical Magazine Vol. 45 (337) Mineralogical Society
Abstract/NotesAbstractSvetlozarite, previously described as a new member of the mordenite group of zeolites, is reinterpreted as a multiply twinned and highly faulted dachiardite. X-ray diffraction study and transmission electron microscopy revealed (001) twins and (100) stacking faults. The former are attributed at least mainly to the insertion of a b glide plane between dachiardite sheets at each twin interface, which preserves the 5-ring linkages between the sheets. The latter are associated with loss of the C face-centring relation, and are attributed to replacement of shared 5-rings by linked 4-rings in the dachiardite sheets. Further study is needed to determine whether the structural faults in the dachiardite structures are chemically controlled.


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