Fig. 12
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Field view of the south flank of the Ikkou diapir showing complex halokinetic geometries in sequence S4.3. The layers mostly made of conglomeratic deposits (marker beds R1, R2 and R3) show synsedimentary folding and internal erosions forming angular unconformities that can reach 90° (e.g., marker bed R2). See location in Figure 12a.
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