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Cann, J. R. (1965) Gyrolite and reyerite from ’S Airde Beinn, northern Mull. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (269) 1-4 doi:10.1180/minmag.1965.035.269.03

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Reference TypeJournal (article/letter/editorial)
TitleGyrolite and reyerite from ’S Airde Beinn, northern Mull
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsCann, J. R.Author
Year1965 (March)Volume35
Page(s)1-4Issue269
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_35/35-269-1.pdf+
DOIdoi:10.1180/minmag.1965.035.269.03Search in ResearchGate
Mindat Ref. ID5838Long-form Identifiermindat:1:5:5838:8
GUIDb9960580-c3dd-49b4-a4a6-758284ec396c
Full ReferenceCann, J. R. (1965) Gyrolite and reyerite from ’S Airde Beinn, northern Mull. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (269) 1-4 doi:10.1180/minmag.1965.035.269.03
Plain TextCann, J. R. (1965) Gyrolite and reyerite from ’S Airde Beinn, northern Mull. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (269) 1-4 doi:10.1180/minmag.1965.035.269.03
In(1965) Mineralogical Magazine Vol. 35 (269) Mineralogical Society
Abstract/NotesSummaryReyerite is found in close association with gyrolite in the metamorphic aureole of the volcanic plug of 'S Airde Beinn, northern Mull, and has apparently been formed by metamorphism of the gyrolite. The gyrolite, with a composition close to Ca16Si24O60(OH)3.14H2O, closely approaches trigonal symmetry with a 9·76±0·02 Å and c 3 × 22·26±0·1 Å; biaxial with a small 2V and α 1·537, β 1·547, γ 1·549. The reyerite is trigonal with a 9·76±0·02 Å, c 19·10±0·04 Å and space group Pω 1·568 and ε 1·563, and the unit cell contains about 14 atoms of Ca, 24 of Si (with some substitution by 4(OH)−), and 14H2O as (OH)− and H2O.

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MineralCitation Details
Gyrolite
Reyerite


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