Abstract
The term Karoo, as applied to igneous rocks, is usually taken to refer to a widespread series of volcanic and intrusive rocks found in southern Africa south of latitude 14°S and dominantly of Lower Jurassic age. Almost everywhere the volcanic members rest on sedimentary rocks of the Karoo Supergroup, an intercratonic basinal sequence of Late Carboniferous to Triassic age (e.g. see Tankard et al., 1982). This review will cover those igneous rocks conventionally referred to as Karoo but will also consider some aspects of a second great pulse of igneous activity which took place in the Lower Cretaceous, particularly in Namibia where substantial recent research has been concentrated on the Etendeka Plateau area. Here a series of lavas can be correlated with those of the Paraná province of Brazil (Erlank, 1984). Other Lower Cretaceous igneous rocks are found overlying the Karoo in the Zambesi valley (the Lupata series, Flores, 1964) and as the plutonic Chilwa Series of southern Malawi (Woolley and Garson, 1970). These, however, will not be described in the present work.
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Cox, K.G. (1988). The Karoo Province. In: Macdougall, J.D. (eds) Continental Flood Basalts. Petrology and Structural Geology, vol 3. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-7805-9_7
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