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Newton, Robert C. (1966) BeO in pegmatitic cordierite. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (275) 920-927 doi:10.1180/minmag.1966.035.275.03

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Reference TypeJournal (article/letter/editorial)
TitleBeO in pegmatitic cordierite
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsNewton, Robert C.Author
Year1966 (September)Volume35
Issue275
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_35/35-275-920.pdf+
DOIdoi:10.1180/minmag.1966.035.275.03Search in ResearchGate
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Mindat Ref. ID5992Long-form Identifiermindat:1:5:5992:7
GUID0
Full ReferenceNewton, Robert C. (1966) BeO in pegmatitic cordierite. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (275) 920-927 doi:10.1180/minmag.1966.035.275.03
Plain TextNewton, Robert C. (1966) BeO in pegmatitic cordierite. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (275) 920-927 doi:10.1180/minmag.1966.035.275.03
In(1965) Mineralogical Magazine Vol. 35 (275) Mineralogical Society
Abstract/NotesSummarySeveral cordierites from pegmatites were found by emission spectroscopy to contain as much as 0·7 wt. % of BeO. Structural crystallographic considerations suggest that the beryl molecule, Be3Al2Si6O18, may have appreciable solubility in the structure of cordierite. Some hydrothermal experiments carried out on this assumption indicated about the same amount of BeO substitution in the magmatic temperature range as is shown by the pegmatite cordierites. The natural BeO-bearing cordierites have distinctive infra-red absorption properties, which are reproduced in the synthetic solid solutions.


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