Hostname: page-component-586b7cd67f-2plfb Total loading time: 0 Render date: 2024-11-23T12:22:32.810Z Has data issue: false hasContentIssue false
  • English
  • Français

Element Partition in a Kaolinitic Clay

Published online by Cambridge University Press:  14 March 2018

R. J. W. McLaughlin
R. J. W. McLaughlin*
Affiliation:
T. & R. Boote Ltd., Burslem, Staffs
Get access

Abstract

The major and minor elements for Pugu D, a rock containing a well-crystallised but disordered form of kaolinite are presented, The concentrations in the various fractions are discussed and reasons adduced for element behaviour. Relationships between element distribution and Sedimentation conditions are considered.

Type
Research Article
Information
Clay Minerals Bulletin , Volume 3 , Issue 18 , December 1957 , pp. 184 - 188
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1957

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

McLaughlin, R. J. W. 1955. Geochim. et cosmoch. Acta, 8, 109-30.CrossRefGoogle Scholar
McLaughlin, R. J. W. 1958. Geochim. et cosmoch. Acta, in press.Google Scholar
Robertson, R. H. S., Brindley, G. W. and Mackenzie, R. C. 1954. Amer. Mim, 39, 118-39.Google Scholar
Stockley, G. M. 1948. Bull. geol. Surv. Tanganyika, (20), 1–37.Google Scholar