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Figure 6. NW-SE trcnding seismic profile shows severa! stackcd large ramps (;
layered reflcctors are lower Miocene Flyschs. Post-Messinian faulting is shown at t
J:>.
N W0'1
Figure 7. NW-SE seismic line showing a wedge of mainly carbonate platform ro
overlain by lower Miocene-upper Miocene foreland basin deposits.
