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Loveland, P. J., Bendelow, V. C. (1984) Celadonite-aluminous-glauconite: an example from the Lake District, UK. Mineralogical Magazine, 48 (346) 113-117 doi:10.1180/minmag.1984.048.346.15

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Reference TypeJournal (article/letter/editorial)
TitleCeladonite-aluminous-glauconite: an example from the Lake District, UK
JournalMineralogical MagazineISSN0026-461X
AuthorsLoveland, P. J.Author
Bendelow, V. C.Author
Year1984 (March)Volume48
Issue346
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_48/48-346-113.pdf+
DOIdoi:10.1180/minmag.1984.048.346.15Search in ResearchGate
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Mindat Ref. ID3595Long-form Identifiermindat:1:5:3595:2
GUID0
Full ReferenceLoveland, P. J., Bendelow, V. C. (1984) Celadonite-aluminous-glauconite: an example from the Lake District, UK. Mineralogical Magazine, 48 (346) 113-117 doi:10.1180/minmag.1984.048.346.15
Plain TextLoveland, P. J., Bendelow, V. C. (1984) Celadonite-aluminous-glauconite: an example from the Lake District, UK. Mineralogical Magazine, 48 (346) 113-117 doi:10.1180/minmag.1984.048.346.15
In(1984, March) Mineralogical Magazine Vol. 48 (346) Mineralogical Society
Abstract/NotesAbstractAn occurrence of a celadonite-like mineral in a weathered basalt in the Lake District has been investigated by X-ray diffraction, X-ray fluorescence, electron microprobe, and infra-red spectroscopic methods. The bulk composition of the mineral corresponds to an aluminous-glauconite. The data show that the mineral is most probably a celadonite-muscovite or celadonite-illite mixture, although a celadonite-phengite cannot be entirely discounted. Approximately 10% smectite layers are also present. The results suggest that re-examination of many aluminous glauconites may show them to be mixtures of this type.

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