Pre-Cambrian structure and the origin of granitoid rocks in south-west Uganda
This thesis gives an account and interpretation of the geology of over four-thousand square miles of south-West Uganda. The Qominant sedimentary rocks are part of the Karagwe-Ankolean System and have been involved in granitisation and orogeny. The area dealt with is part of a curvet orogency belt st...
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University of London
1956
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.526746 |