Figure 4. Portion of the stacked seismic line Lusigal 4 located in Figure 2 and showing the normal fault (F) bounding the PR to the east as suggested by Beslier et al. (1993). This normal fault has been reactivated as a reverse fault during lower Miocene. SR = synrift sediments; BU = breakup unconformity.

Figure 4. Portion of the stacked seismic line Lusigal 4 located in Figure 2 and showing the normal fault (F) bounding the PR to the east as suggested by Beslier et al. (1993). This normal fault has been reactivated as a reverse fault during lower Miocene. SR = synrift sediments; BU = breakup unconformity.