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Dadák, V., Novák, F. (1965) Tin-containing andradite from Plavno mine in the Krušné Hory Mts., Czechoslovakia. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 379-385 doi:10.1180/minmag.1965.035.270.11

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Reference TypeJournal (article/letter/editorial)
TitleTin-containing andradite from Plavno mine in the Krušné Hory Mts., Czechoslovakia
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsDadák, V.Author
Novák, F.Author
Year1965 (June)Volume35
Issue270
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_35/35-270-379.pdf+
DOIdoi:10.1180/minmag.1965.035.270.11Search in ResearchGate
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Mindat Ref. ID5880Long-form Identifiermindat:1:5:5880:7
GUID0
Full ReferenceDadák, V., Novák, F. (1965) Tin-containing andradite from Plavno mine in the Krušné Hory Mts., Czechoslovakia. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 379-385 doi:10.1180/minmag.1965.035.270.11
Plain TextDadák, V., Novák, F. (1965) Tin-containing andradite from Plavno mine in the Krušné Hory Mts., Czechoslovakia. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 379-385 doi:10.1180/minmag.1965.035.270.11
In(1965) Mineralogical Magazine Vol. 35 (270) Mineralogical Society
Abstract/NotesSummaryStannian andradite occurs with pyroxene and carbonates, with blende and pyrite as accessories in a skarn deposit in the Plavno mine, Krušné Hory Mts., NW. Bohemia. The green crystals are rhombic dodecahedra up to 3 cm in size. Sp. gr. 3·78; n 1·879; a 12·079±0·002 Å. Quantitative chemical and spectrographic analyses are given; the composition is (Ca2·96Mg0·04Mn0·02)3·02 (Si2·95Sn0·04)2·99O12. The content of tin (SnO2 1·07 %) is isomorphously bound in the lattice, and according to crystallochemical calculations the entrance of tin into the garnet lattice is most probably due to substitution of The presence of tin in the andradite shows that this element was already present in the metasomatic solutions during the process of skarnization.


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