Ternary classification of low rate intracratonic basins. The diagram relates typical tectono-stratigraphic basin architecture (flat syncline-shaped, syncline-shaped or complex-shaped basin) to internal and external forcing parameters. Example of plotted basins according to their architecture, geometry and subsidence history (see Fig. 12): 1: Ahnet Basin, North Africa (Perron et al., 2018); 2: Mouydir Basin, North Africa (Perron et al., 2018); 3: Tim Mersoï Basin, North Africa (Perron, 2019); 4: Tamesna Basin, North Africa (Lessard, 1961; Perron, 2019). Notice that here the “hot” geotherm (Fig. 4C) is by default if it is not specified. Basic local erosion/deposition processes are active in each model.