Hostname: page-component-669899f699-8p65j Total loading time: 0 Render date: 2025-04-28T18:05:45.087Z Has data issue: false hasContentIssue false
  • English
  • Français

Celadonite-aluminous-glauconite: an example from the Lake District, UK

Published online by Cambridge University Press:  05 July 2018

P. J. Loveland  and
V. C. Bendelow
P. J. Loveland
Affiliation:
Soil Survey of England and Wales, Rothamsted Experimental Station, Harpenden, Herts. AL5 2JQ
V. C. Bendelow
Affiliation:
Soil Survey of England and Wales, Rothamsted Experimental Station, Harpenden, Herts. AL5 2JQ
Get access Rights & Permissions [Opens in a new window]

Abstract

An 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.

Type
Research Article
Information
Mineralogical Magazine , Volume 48 , Issue 346 , March 1984 , pp. 113 - 117
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1984

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Article purchase

Temporarily unavailable

References

Bailey, S. W. (1980) In Crystal Structures of Clay Minerals and their Identification (Brindley, G. W., and Brown, G., eds.). Mineralogical Society London, 1–123.Google Scholar
Brinkmann, R. (1977) Geoderma. 17, 111–44.CrossRefGoogle Scholar
Buckley, H. A., Bevan, J. C., Brown, K. M., and Johnson, L. R. (1978) Mineral. Mag. 42, 373–82.CrossRefGoogle Scholar
Carroll, D. (1970) Geol. Soc. Am. Spec. Pap. 126, 1–80.Google Scholar
Deer, W. A., Howie, R. A., and Zussman, J. (1962) Rock Forming Minerals, 3. Longmans, London.Google Scholar
Eastwood, T., Hollingworth, S. E., Rose, W. C. C., and Trotter, F. M. (1968) Geology of the Country around Cockermouth and Caldbeck, 152–3. HMSO, London.Google Scholar
Heddle, M. F. (1901) The Mineralogy of Scotland, 2, 145–6. David Douglas, Edinburgh.Google Scholar
Hendricks, S. B., and Ross, C. S. (1941) Am. Mineral. 26, 683–708.Google Scholar
Kautz, K. (1965) Beitr. Mineral. Petrogr. 11, 398–404.Google Scholar
Malkova, K. M. (1956) Lvov. Geol. Obslach Mineral. Sb. 10, 305–18.[MA 13-179].Google Scholar
Manghnani, M. H., and Hower, J. (1964) Am. Mineral. 49, 586–98.Google Scholar
Mehra, O. P., and Jackson, M. L. (1960) Clays Clay Minerals. 5, 317–27.Google Scholar
Pirani, R. (1963) Mineral Petrogr. Ada. 9, 31–78.Google Scholar
Reynolds, R. C. (1980) In Crystal Structures of Clay Minerals and their Identification (Brindley, G. W., and Brown, G., eds.). Mineralogical Society London, 249–303.Google Scholar
Smulikowski, K. (1936) Arch. Mineral. 12, 144–80.Google Scholar
Smulikowski, K. (1954) Ibid. 21, 119.Google Scholar
Walker, G. P. L. (1960) Mineral. Mag. 32, 503–27.Google Scholar
Weaver, C. E., and Pollard, L. D. (1973) The Chemistry of Clay Minerals. Elsevier, 5–53.Google Scholar
Wiewiora, A., Lafka, B., and Szczyrba, J. (1979) In Eighth Conference on Clay Mineralogy and Petrology, Teplice, Czechoslovakia, 47–58. Charles University Press, Prague.Google Scholar
Wise, W. S., and Eugster, H. P. (1964) Am. Mineral. 49, 1031–83.Google Scholar
Yoder, H. S., and Eugster, H. P. (1955) Geochim. Cosmochim. Acta. 8, 225–80.CrossRefGoogle Scholar