Control of inherited accreted lithospheric heterogeneity on the architecture and the low, long-term subsidence rate of intracratonic basins

Open Access

Fig. 12

Comparison of total subsidence curves between numerical models and geological data extracted from the Mouydir Basin, Algeria (9: Well W21; Perron et al., 2018) and the Ahnet Basin, Algeria (5: well W1, Kracha, 2011). The Algerian wells are localized in Figure 2A. The curves are presented in Figure 1.

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