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- W2091325504 abstract "Offshore seismic reflection and well data have been used to establish the structural style of the offshore of Agadir and to extend the Atlas fabric into the deep-water domain. The obtained structural subsurface map exhibits a complex architecture resulting from the coexistence of normal, inverse, wrench faults and folds cored by Triassic salt. The seismic data indicate a structural style characterised by narrow, detached folding above Triassic salt layers. The strong similarities in the style of deformation between the Agadir offshore and the Cap-Tafelney fold belt, suggest that both of them form one continuous belt, which corresponds to the western termination of the Atlas alpine system. L’analyse des profils sismiques et des données de puits pétrolier a permis de définir le style structural de l’offshore d’Agadir et d’étendre les unités structurales du Haut Atlas vers le domaine marin. La carte obtenue fait apparaître une architecture complexe, due aux jeux successifs de failles normales, inverses et décrochantes. Les coupes sismiques présentées illustrent un style de déformation marqué par des anticlinaux étroits à cœur salifère et associés à une surface de détachement triasique. La grande similitude entre ce style et celui de la chaîne de Cap-Tafelney permet de déduire que ces deux entités forment une chaîne sous-marine continue, marquant à ce niveau la terminaison occidentale du système alpin." @default.
- W2091325504 created "2016-06-24" @default.
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- W2091325504 date "2000-09-01" @default.
- W2091325504 modified "2023-09-27" @default.
- W2091325504 title "Structure sismique de la plate-forme Atlantique au large d'Agadir (Maroc sud-occidental)" @default.
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- W2091325504 doi "https://doi.org/10.1016/s1251-8050(00)01422-1" @default.
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