Fig. 4: The Yusuf pull-apart Basin.
From: Evidence for a developing plate boundary in the western Mediterranean
a Time-migrated section crossing along the Yusuf pull-apart basin depocentre parallel to the YFS strike (Figs. 1 and 2; Vertical Exaggeration ~2.5). Pre-kinematic unit S6 is disrupted ~11 km below the basin depocentre (CMPs 9000–5000). b Time-migrated YFS-strike perpendicular section (Figs. 1 and 2; Vertical Exaggeration ~2.5). c Ages and seismostratigraphic units identified at the Yusuf pull-apart Basin (YB) and the East and South Alboran Basins (EAB and SAB, respectively).
