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Figure 3.

(A) Erosion/deposition maps of the source, transfer, and sink domains at 5, 10, 15, 20, and 25 m.y. Stage 1 (0–15 m.y.), active salt deformation controls basin accommodation and sediments infill the proximal minibasins. Stage 2 (15–25 m.y.) sedimentary pathways (M and N) bypass sediments around salt-cored highs A and B. Parts of minibasin X remain sediment starved. (B) Cross section along northern end of minibasin X showcasing modified stratigraphic patterns (see Fig. 4).

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