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An X-ray examination of an exceptionally well crystallized kaolinite

Published online by Cambridge University Press:  14 March 2018

J. Goodyear  and
W. J. Duffin
J. Goodyear
Affiliation:
Physics Department, University of Hull
W. J. Duffin
Affiliation:
Physics Department, University of Hull
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Summary

Specimens of kaolinite have been found in inclusions in the ferruginous deposits on the Yorkshire Coast, just north of Scalby. The excellent quality of the X-ray powder pattern suggests that this kaolinite is better crystalline than kaolinites from other localities. Although the lattice constants of the Scalby material are considered to be identical with those previously published for kaolinite, minor differences in the intensities of the X-ray reflections do occur and may be due to a less distorted structural layer in the Sealby kaolinite.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 32 , Issue 254 , September 1961 , pp. 902 - 907
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1961

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References

Brindley, (G. W.) and Robinson, (K.), 1946. Min. Mag., vol. 27, p. 242.Google Scholar
Brindley, (G. W.) and Nakahira, (M.), 1958. Min. Mag., vol. 31, p. 781.Google Scholar
Newnham, (R. E.), 1950. Ph.D. Thesis, Pennsylvania State University.Google Scholar
Newnham, (R. E.) and Brindley, (G. W.), 1956. Acta Cryst., vol. 9, p. 759.Google Scholar