Hostname: page-component-586b7cd67f-l7hp2 Total loading time: 0 Render date: 2024-11-29T18:08:20.351Z Has data issue: false hasContentIssue false

An X-ray examination of an exceptionally well crystallized kaolinite

Published online by Cambridge University Press:  14 March 2018

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

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
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1961

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.)

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