Fig. 10.17. (Left) Reconstruction of the plate tectonic setting of the basins associated with subduction of the Gondwana
orogen. (Above) Cartoons to show the evolution of the Cape Fold belt of the Gondwana orogen in South Africa. [Reprinted from Johnson, M. R., van Vuuren, C. J., Visser, J. N. J., Cole, D. I., Wickens, H. de V., Christie, A. D. M., and
Roberts, D. L. 1997. The Foreland Karoo basin, South Africa. In "African Basins" (R. C. Selley, ed.), pp. 269-317, with
permission from Elsevier Science.]
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