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Recent geological and geophysical studies of the Karoo and pre-Karoo rifts and basins of Zimbabwe, Zambia, and Botswana have focussed on the thick sedimentary sequences overlying the crystaline basement. This review of the work of a West German team in cooperation with local geological surveys confirms the presence of potential hydrocarbon source rocks in al the areas reported here. Most have passed through the "oil window" and are now in the stage of wet gas generation; favourable traps also exist. The author evaluates each basin and trough for its hydrocarbon potential. (Ed.) were widely distributed lavas, some with sedimentary intercalations. In the Cenozoic, the predominant sediments were aeolian and fluviatile. These cover large areas of southern Africa, burying most of its Palaeozoic and Mescrzoic rocks. In general, all the basins and troughs described here pased through a similar history from the late Palaeozoic to the Recent. This applies both to the tectonic events and to the depositional history of Karoo and post-Karoo sediments.

Prospects for Oil and Gas in Zimbabwe, Zambia and Botswana