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Sedimentary rocks of the Palaeozoic Cape Supergroup, Natal Group and Msikaba Formation were deposited on a passive continental margin in a variety of terrestrial and shallow marine-shelf depositional environments, from the early Ordovician until the mid-Carboniferous. Tectonism, which took place between 278Ma and 230Ma, affected only the Cape Supergroup rocks and resulted in the Cape Fold Belt. Rocks...
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