Figure 1
From: Coevolution of diagenetic fronts and fluid-fracture pathways

(A) Geological map of the Western High Atlas showing the Essaouira-Agadir basin (EAB) onshore and its extension offshore14,20. The study location is highlighted with a red star (Amsittene Anticline). The lower image depicts the cross section from A-B which shows the overall basin structure and influence of salt diapir as well as deep transfer fault to the formation of Amsittene anticlinal structure (Hafid, 2000). (B) Generalized stratigraphy of the Essaouira-Agadir basin (EAB) and the corresponding tectonic events11,20. The numbered black rectangles represent: 1. Arich Ouzla Formation, 2. Amsittene Formation, and 3. Im-n-Tanout Formation.