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Pattiaratchi, D. B., Saari, Esko, Sahama, Th. G. (1967) Anandite, a new barium iron silicate from Wilagedera, North Western Province, Ceylon. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 1-4 doi:10.1180/minmag.1967.036.277.01

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Reference TypeJournal (article/letter/editorial)
TitleAnandite, a new barium iron silicate from Wilagedera, North Western Province, Ceylon
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsPattiaratchi, D. B.Author
Saari, EskoAuthor
Sahama, Th. G.Author
Year1967 (March)Volume36
Issue277
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_36/36-277-1.pdf+
DOIdoi:10.1180/minmag.1967.036.277.01Search in ResearchGate
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Mindat Ref. ID6027Long-form Identifiermindat:1:5:6027:5
GUID0
Full ReferencePattiaratchi, D. B., Saari, Esko, Sahama, Th. G. (1967) Anandite, a new barium iron silicate from Wilagedera, North Western Province, Ceylon. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 1-4 doi:10.1180/minmag.1967.036.277.01
Plain TextPattiaratchi, D. B., Saari, Esko, Sahama, Th. G. (1967) Anandite, a new barium iron silicate from Wilagedera, North Western Province, Ceylon. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 1-4 doi:10.1180/minmag.1967.036.277.01
In(1966) Mineralogical Magazine Vol. 36 (277) Mineralogical Society
Abstract/NotesSummaryAnandite is a new barium iron silicate found in the magnetite ore zone of the Wilagedera iron ore body, in the North Western Province of Ceylon. The mineral is named after the late Dr. Ananda Coomaraswamy, the first director of the Mineral Survey of Ceylon.Anandite is monoclinic, with a 5·412, b 9·434, c 19·953 Å, β 94° 52′, space group C2/c. D 3·94, hardness 3–4. Optically positive, b ‖ β, γ ∧ a 12°, β 1·855, γ > 1·88. Pleochroism: β green, γ brown. Chemical composition corresponds to the simplified formula (Ba,K) (Fe,Mg)a (Si,Al,Fe)4O10 (O,OH)2 with Z = 2. The data available indicate that the mineral has the trioctahedral structure of the brittle micas.


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