Figure 3

SW-NE-trending single-channel CHIRP seismic reflection profiles showing the three morphologic domains: outer SW, inner, and outer NE. The outer SW is deformed while the inner preserves two main units: a basal veneer unit and an upper transparent unit. The carbonate mound in (A) is emplaced along the strike of the west fault, as shown in. (B) Interpretation made with SonarWiz software, version 7.04 (CHESAPEAKE TECHNOLOGIES; https://chesapeaketech.com).