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The Late Palaeozoic Glaciation of Gondwanaland in Relation to West Africa and to Northern South America During Carboniferous Time

Published online by Cambridge University Press:  01 May 2009

M. M. Anderson
Affiliation:
Geology Department, University of Mandalay, Burma.

Abstract

Lower Carboniferous strata are shown to be absent from the Amazon basin and Ghana, the Bermejo series of Bolivia is Permo-Triassic, the Sekondi series of Ghana does not include glacial deposits and may prove to be Devonian, early Carboniferous glaciation is unknown in Africa and restricted to Argentina in South America. In the light of these interpretations the extent to which late Carboniferous glaciation affected northern South America and Africa is briefly reviewed and shown to conflict with the reconstructions by L. C. King (1958). The non-glaciation of Africa and South America north of at least latitude 25 degrees South during early Carboniferous times is regarded as proving that these areas did not pass through the south polar region at that time. The known distribution of early and late Carboniferous glacial deposits is considered in relation to continental drift and movement can only have been westwards during the Carboniferous period.

Type
Articles
Copyright
Copyright © Cambridge University Press 1961

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References

REFERENCES

Ahlfeld, F., 1956. “ Bolivia ” in Handbook of South American Geology. Geol. Soc. Amer. Mem., 65, 169179.Google Scholar
Anderson, M. M., 1961. The Geological Structure and Age of the Sekondi Series, Ghana. Journ. W.Afr. Sci. Assoc., 7.Google Scholar
Barbosa, O., 1952. Comparison between the Gondwana of Brazil, Bolivia, and Argentina. XIX Intern. Geol. Congr. Algeria, Symposium Gondwana, 313324.Google Scholar
Bates, D. A., 1956. Gold Coast and Togoland. Lexique Stratigraphique International, IV, Fasc. 3b, 25–6.Google Scholar
Beurlen, K., 1953. Einige vorlaufige Mitteilungen über die Stratigraphie des Gondwana-Systems in Südbrasilien. Neues Jahb. Geol. u. Palaont., Abh. Bd. 97, 241256.Google Scholar
Cox, L. R., 1946. The Fossils and Age of the Sekondi Series (Upper Palaeozoic) of the Gold Coast. Ann. Mag. Nat. Hist., Ser. 11, xiii, 602624.Google Scholar
Crow, A. T., 1952. The Rocks of the Sekondi Series of the Gold Coast. Gold Coast Geol. Surv. Bull., 18.Google Scholar
Davies, A. M., 1925. Fossils from Accra. C. R. Congr. Geol. Internat., XIII Sess., fasc. 2, 947.Google Scholar
Junner, N. R., 1939. Sekondian System. Rept. Gold Coast Geol. Surv., 1938–39, 1315.Google Scholar
Junner, N. R. 1940. Geology of the Gold Coast and Western Togoland. Gold Coast Geol. Surv. Bull., 11.Google Scholar
King, L. C., 1958. Basic Palaeogeography of Gondwanaland during the Late Palaeozoic and Mespzoic Eras. Quart. Journ. Geol. Soc., cxiv, 4770.CrossRefGoogle Scholar
SirKitson, A., 1928. Provisional Geological Map of the Gold Coast and Western Togoland with Brief Descriptive Notes thereon. Gold Coast Geol. Surv. Bull., 2, 1011.Google Scholar
Mather, K. F., 1922. Front Ranges of the Andes between Santa Cruz and Embarcacion. Bull. Geol. Soc. Amer., 23, 703764.CrossRefGoogle Scholar
McCallien, W. J., and Anderson, M. M., 1960. Two Notes on Slumping near Takoradi, Ghana. Journ. W.Afr. Sci. Assoc., 6.Google Scholar
De Oliveira, A. I., 1956. “ Brazil ”in Handbook of South American Geology. Geol. Soc. Amer. Mem., 65, 1638.Google Scholar