Hostname: page-component-848d4c4894-ndmmz Total loading time: 0 Render date: 2024-06-02T11:35:12.587Z Has data issue: false hasContentIssue false

Replacement Veins in the Dahomeyan of Ghana

Published online by Cambridge University Press:  01 May 2009

Abstract

A basic gneiss in Ghana is traversed by light veins which are considered to have originated by replacement because gneissic mineral banding persists through them. Veins make up to 10 per cent of the rock over hundreds of square miles. It appears that a very large amount of material has been transported through the basic rocks without destroying their gneissic structure.

Type
Articles
Copyright
Copyright © Cambridge University Press 1959

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

Aicard, P., and R., Pougnet, 1954. Le dahomeyau du Dahomey et du Togo Francais. C.R. 19th. Int. Geol. Cong. Fasc., xx, 107113.Google Scholar
Bates, D. A., 1954. Report of the Director, Gold Coast Geol. Surv., 19521953.Google Scholar
Goodspeed, G. E., 1940. Dilation and replacement dikes. Journ. Geol., xlviii, 175195.CrossRefGoogle Scholar
Junner, N. R., and Bates, D. A., 1945. Reports on the Geology and Hydrology of the Coastal Area East of the Akwapim Range. Gold Coast Geol. Surv. Mem., vii.Google Scholar
Roques, M., 1949. Le precambrien de l'afrique Occidenta le francaise. Bull. Soc. Geol. France ser. V, xviii, 589628.Google Scholar
Roques, M., 1951. Presentation d'un memoire sur le precambrien de l'a.O.F. Rept. 18th Int. Geol. Cong., xiv, 184.Google Scholar
Schmidt, W., 1932. Tektonik und Verformungslehre. Borntraeger, Berlin.CrossRefGoogle Scholar
Turner, F. J., and Verhoogen, J., 1951. Igneous and Metamorphic Petrology. McGraw Hill, New York.Google Scholar
von Knorring, O., and Kennedy, W. Q., 1958. The mineral paragenesis and metamorphic status of garnet-hornblende-pyroxene-scapolite gnesis from Ghana. Miner. Mag., xxxi, 846859.Google Scholar
Wells, A. K., and Bishop, A. C., 1954. The Origin of Aplites. Proc. Geol. Assoc., lxv, 95115.CrossRefGoogle Scholar