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In page Agulhas Bank:
"The Diaz Marginal Ridge (DMR) separates these basins from the AFFZ. The DMR is buried under 200–250 m (660–820 ft) of sediments and sedimentary rocks and 150–200 m (490–660 ft) of this sedimentary material is undisturbed Cretaceous sediments younger than the oldest Cretaceous sedimentary rocks in the Southern Outeniqua Basin. The DMR must therefore have formed after the initial West Gondwana breakup 130-90 Mya. The DMR probably formed when new, hot oceanic crust slid past old, cold continental crust and the contrast in temperatures induced a thermal uplift.[7]
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