(A) Model M with far field tectonics, remote sediment supply and thermal anomaly shows a complexification of the basin and arch architecture within Figure 9 with the set-up of inter-basins boundary secondary arches and intra-basin secondary arches. The strain is concentrated in the central basin with creation of grabens above shear zones (i.e. limits of terranes). (B) Stratigraphy and hiatus repartition between the wells W1-M6 to W5-M6. (C) Subsidence curves of wells W1-M6 to W6-M6 display an exponential decay with deviations of different amplitude depending on their localization (i.e. near maximum strain zones or not). Oscillations related to tectonic loading might be in phase, in antiphase or out of phase between arches and basins or between neighbouring basins but also depending on tectonic context. Comparison with Figure 1 subsidence bibliographic data (dashed lines). See Figure 4B for the boundary conditions.