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Černý, P. (1963) Epididymite and milarite—alteration products of beryl from Věžná, Czechoslovakia. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (261) 450-457 doi:10.1180/minmag.1963.033.261.02

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Reference TypeJournal (article/letter/editorial)
TitleEpididymite and milarite—alteration products of beryl from Věžná, Czechoslovakia
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsČerný, P.Author
Year1963 (June)Volume33
Issue261
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_33/33-261-450.pdf+
DOIdoi:10.1180/minmag.1963.033.261.02Search in ResearchGate
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Mindat Ref. ID5727Long-form Identifiermindat:1:5:5727:5
GUID0
Full ReferenceČerný, P. (1963) Epididymite and milarite—alteration products of beryl from Věžná, Czechoslovakia. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (261) 450-457 doi:10.1180/minmag.1963.033.261.02
Plain TextČerný, P. (1963) Epididymite and milarite—alteration products of beryl from Věžná, Czechoslovakia. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (261) 450-457 doi:10.1180/minmag.1963.033.261.02
In(1962) Mineralogical Magazine Vol. 33 (261) Mineralogical Society
Abstract/NotesSummaryEpididymite, determined by means of its optical properties, X-ray powder pattern, and spectrographic analysis, was found in a desilicated pegmatite near Věžná, Western Moravia, Czechoslovakia. It was formed contemporaneously with minor amounts of milarite in a late hydrothermal stage by the action of sodium-rich solutions on beryl. This is the first occurrence of epididymite and milarite as alteration products of beryl and the first findings of epididymite in any other paragenesis than that of alkaline pegmatites. The optical properties of epididymite are re-examined and older data rejected.


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