Fig. 3: Deep structure of the Yusuf Fault System (YFS).
From: Evidence for a developing plate boundary in the western Mediterranean
a Pre-stack depth migrated section across the YFS (see Figs. 1 and 2 for location) showing the tectonic structure. The Yusuf pull-apart Basin (CMPs 7500–8500) has 2.7 km of maximum sediment thickness. b Time-migration of the same section. The Moho is located at ~11–12 s TWTT southern of the YFS, while it is located at ~8–9 s TWTT northern of the YFS. B: Basement, M: Messinian unconformity, MB: Metamorphic basement, S: Sediments, YFS: Yusuf Fault System.
