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The Namibian margin evolution started 130Myr ago after the breakup between South America and southern Africa. Today, it shows specific features: (i) an elevation and a bathymetry about 1000m higher than the surrounding areas, (ii) a significant sediment supply during the Late Cretaceous following the first sedimentary peak that occurred during rifting and just afterwards, and (iii) a long-term progradation...
The thermal and flexural evolution of passive margins is impacted by the (un)loading effects of erosion/sedimentation processes, which, in turn, affect their relief and sediment accumulation. These complex couplings are recorded by the stratigraphic trend of the associated sedimentary basins, which is controlled by the balance between sediment accumulation, subsidence and eustasy.Our objective is...
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