The structural and magmatic evolution of the Lebombo monocline, South Africa, with particular reference to Swaziland
<p>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 1:50,00...
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Other Authors: | |
Format: | Thesis |
Language: | English |
Published: |
1977
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