Fig. 6
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Subsidence curves from different models in Figure 5 (wells W1-A1 to W1-A2 and W1-P1 to W1-P2) associated with Figure 1 bibliographic data (dashed lines). The thermal subsidence of W1-A1 and W1-A2 is achieved after 150 Myr. The wells P1 and P2 show linear decay subsidence with deviations of different amplitudes. See Figure 4B for the boundary conditions.
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