Fig. 8

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Subsidence curves from different models in Figure 7 (wells W1-M1 to W1-M4) associated with Figure 1 bibliographic data. The subsidence of W1-M1, W1-M3 and W1-M3’ is constant after 250 Myr (i.e. still have a potential of subsidence), in contrast with the subsidence of W1-A1 and W1-A2 where it stops after 150 Myrs. The wells W1-M2 and W1-M4 show linear decay subsidence with deviations of different amplitude. See Figure 4B for the boundary conditions.
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