Hostname: page-component-586b7cd67f-t7czq Total loading time: 0 Render date: 2024-11-23T21:53:34.282Z Has data issue: false hasContentIssue false
  • English
  • Français

X-ray Examination of some Clays from the London Platform

Published online by Cambridge University Press:  01 May 2009

R. W. Tank
R. W. Tank
Affiliation:
Lawrence University, Appleton, Wisconsin.
Get access Rights & Permissions [Opens in a new window]

Abstract

X-ray analyses of Kimmeridgian clays recovered from the Warlingham Number 1 Borehole indicate that illite and kaolinite are the dominant clay minerals present. Illite, chlorite, and kaolinite, are present in the Devonian clays recovered from the Willesden Number 1 Borehole. The relationships between the clay minerals of the Kimmeridgian and Devonian clays and the clay mineral assemblage of the English Wealden is discussed.

Type
Articles
Information
Geological Magazine , Volume 101 , Issue 6 , 30 December 1964 , pp. 535 - 540
Copyright
Copyright © Cambridge University Press 1964

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

REFERENCES

Allen, P., 1954. Geology and geography of the London-North Sea Uplands in Wealden times. Geol. Mag., 91, 498–508.CrossRefGoogle Scholar
Butterworth, B., and Honeyborne, D. B., 1952. Bricks and clays of the Hastings Beds. Trans. Brit. Ceramic Soc., 51, 211–259.Google Scholar
Droste, J. B., 1956. Alteration of clay minerals by weathering in Wisconsin tills. Bull. geol. Soc. Amer., 67, 911–18.CrossRefGoogle Scholar
Tank, R. W., 1962. Clay mineralogy of selected clays from the English Wealden. Geol. Mag., 99, 128–136.CrossRefGoogle Scholar