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Rieder, M., Píchová, A., Fassová, M., Fediuková, E., Černý, P. (1971) Chemical composition and physical properties of lithium-iron micas from the Krušné hory (Erzgebirge), Czechoslovakia and Germany. Part B: Cell parameters and optical data. Mineralogical Magazine, 38 (294) 190-196 doi:10.1180/minmag.1971.038.294.08

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Reference TypeJournal (article/letter/editorial)
TitleChemical composition and physical properties of lithium-iron micas from the Krušné hory (Erzgebirge), Czechoslovakia and Germany. Part B: Cell parameters and optical data
JournalMineralogical Magazine
AuthorsRieder, M.Author
Píchová, A.Author
Fassová, M.Author
Fediuková, E.Author
Černý, P.Author
Year1971 (June)Volume38
Issue294
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_38/38-294-190.pdf+
DOIdoi:10.1180/minmag.1971.038.294.08Search in ResearchGate
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Mindat Ref. ID6459Long-form Identifiermindat:1:5:6459:4
GUID0
Full ReferenceRieder, M., Píchová, A., Fassová, M., Fediuková, E., Černý, P. (1971) Chemical composition and physical properties of lithium-iron micas from the Krušné hory (Erzgebirge), Czechoslovakia and Germany. Part B: Cell parameters and optical data. Mineralogical Magazine, 38 (294) 190-196 doi:10.1180/minmag.1971.038.294.08
Plain TextRieder, M., Píchová, A., Fassová, M., Fediuková, E., Černý, P. (1971) Chemical composition and physical properties of lithium-iron micas from the Krušné hory (Erzgebirge), Czechoslovakia and Germany. Part B: Cell parameters and optical data. Mineralogical Magazine, 38 (294) 190-196 doi:10.1180/minmag.1971.038.294.08
In(1971, June) Mineralogical Magazine Vol. 38 (294) Mineralogical Society
Abstract/NotesSummaryUnit-cell dimensions and refractive indices of lithium-iron micas decrease with decreasing iron and increasing lithium. Indices β and γ as well as parameters a and b can be used to estimate the composition of lithium-iron micas but basal spacing and 2Vα are poor indicators of composition.The chemical composition of natural lithium-iron micas from the Krušné hory and the Erzgebirge along the Czechoslovak—German border was discussed in Part A of this study (Rieder et al., 1970). It was concluded that the composition and crystallography of these micas fit best the series siderophyllite-polylithionite. The compositions were expressed by the ratio A′ = LR/(LR+‘Fe’). In this expression, LR is the subscript value of Li or octahedral R3+ (whichever is the smaller) in the crystallochemical formula, ‘Fe’ is the sum of the values in the formula of Fe2+ and Mn2+. A′ therefore defines the position of a particular mica on the siderophyllite-polylithionite join. This paper deals with the correlation between composition, cell dimensions, and refractive indices.


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