Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-26T19:35:55.408Z Has data issue: false hasContentIssue false
  • English
  • Français

Some Comments on the Tillite from the Buem Formation of Upper Precambrian Age, from the Volta Region of Ghana, West Africa

CORRESPONDENCE

Published online by Cambridge University Press:  01 May 2009

S. V. Bell
S. V. Bell
Affiliation:
Department of Geology, University of Khartoum, Khartoum, Republic of the Sudan.
Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Correspondence
Information
Geological Magazine , Volume 101 , Issue 6 , 30 December 1964 , pp. 564 - 565
Copyright
Copyright © Cambridge University Press 1964

References

REFERENCES

Bates, D. A., 1954. Report of the Director of the Geological Survey for the year 1952–1953. Accra, Gold Coast.Google Scholar
Bell, S. V., 1962. Unpublished report on the Geology of Field Sheet 182. Ghana Geological Survey, Accra, Ghana.Google Scholar
Haughton, S. H., 1963. Stratigraphic History of Africa South of the Sahara. Oliver and Boyd, Edinburgh and London.Google Scholar
Junner, N. R., 1936. Report on the Geological Survey Department for the Financial Year 1933–36. Accra, Gold Coast.Google Scholar
Koert, W., 1906. Uber Gold Vorkommen bei Kpandu in Togo. Dtsch. Kolon Blatt, 17, 279.Google Scholar
Schermerhorn, L. J. G., and Stanton, W. I., 1963. Tilloids in the West Congo geosyncline. Quart. J. geol. Soc. Lond., 119 (2), 201–241.CrossRefGoogle Scholar