The structural and magmatic evolution of the Lebombo Monocline, Southern Africa, with particular reference to Swaziland
The Lebombo Monocline is a large flexure of Karroo age extending from Southern Rhodesia to Natal. It consists mainly of a thick sequence of Karr basalts and rhyolites overlying the Archaean crust. The Karroo strata dip eastwards beneath Cretaceous cover at angles of up to 50°. Four 1:50,000 detailed...
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University of Oxford
1977
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.451691 |