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Henderson, C. M. B., Taylor, D. (1984) Thermal expansion behaviour of beryllonite [Na(BePO4)] and trimerite [CaMn(BeSiO4)3]. Mineralogical Magazine, 48 (348) 431-436 doi:10.1180/minmag.1984.048.348.14

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Reference TypeJournal (article/letter/editorial)
TitleThermal expansion behaviour of beryllonite [Na(BePO4)] and trimerite [CaMn(BeSiO4)3]
JournalMineralogical MagazineISSN0026-461X
AuthorsHenderson, C. M. B.Author
Taylor, D.Author
Year1984 (September)Volume48
Page(s)431-436Issue348
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_48/48-348-431.pdf+
DOIdoi:10.1180/minmag.1984.048.348.14Search in ResearchGate
Mindat Ref. ID3650Long-form Identifiermindat:1:5:3650:8
GUIDd0cacc46-d79a-4ca7-98fc-1f6f95f1d09c
Full ReferenceHenderson, C. M. B., Taylor, D. (1984) Thermal expansion behaviour of beryllonite [Na(BePO4)] and trimerite [CaMn(BeSiO4)3]. Mineralogical Magazine, 48 (348) 431-436 doi:10.1180/minmag.1984.048.348.14
Plain TextHenderson, C. M. B., Taylor, D. (1984) Thermal expansion behaviour of beryllonite [Na(BePO4)] and trimerite [CaMn(BeSiO4)3]. Mineralogical Magazine, 48 (348) 431-436 doi:10.1180/minmag.1984.048.348.14
In(1984, September) Mineralogical Magazine Vol. 48 (348) Mineralogical Society
Abstract/NotesAbstract
The thermal expansions of trimerite and beryllonite have been determined up to 800°C. No anomalies were observed in the thermal expansion curves but the expansion coefficients for beryllonite are approximately twice those of trimerite. The thermal expansion behaviour of the minerals is interpreted in terms of a tetrahedral tilting model with the main change in apparent tilting being about the monoclinic 010 plane, i.e. the 0001 pseudo-hexagonal plane.

Mineral Pages

MineralCitation Details
Beryllonite
Trimerite


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