Fig. 3

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Seismic line-drawing illustrating, from the shelf to the deep basin, the Messinian and Pliocene-Pleistocene markers used in this study. The pre-salt unit is considered as the mega-sequence below the salt (in the deep basin) or below the Messinian Erosional Surface (in the upper slope and shelf) (modified after Leroux et al., 2019). Salt morphology domains from Bellucci et al., 2021a. LDSD refers to Large Diapirs Salt Domain.

Ligne sismique illustrant, depuis le plateau continental jusqu’au bassin profond, les marqueurs messiniens et pliocènes-pléistocènes utilisés dans cette étude.

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