(A) Tectono-stratigraphic basin architecture and heat production of Model M5 without thermal anomaly shows stratigraphic features (i.e. onlaps, truncations and thickness variations) when approaching the arches. (B) Stratigraphy and hiatus repartition between the wells W1-M5 to W3-M5. (C) Subsidence curves of well W1-M5 to W3-M5 are characterized by exponential decay shape. Comparison with Figure 1 subsidence bibliographic data (dashed lines).