Figure 10. Basement depth contour map of the Málaga Graben (de la Linde et al., 1996). Contour lines every 100 ms (TWT), showing Andalucía-G1 (And-G1), Alborán-A1 (Alb-A1), DSDP 121, and Site 976 locations. Both flanks of the graben correspond to complex interference of former submarine or formerly emerged surfaces and low- and high-angle normal faults, normal-oblique transfer faults, and tops of rollover structures affecting the basement. Steep surfaces near the Spanish coast correspond to post-Messinian strike-slip or oblique faults that prolongate on land.

Figure 10. Basement depth contour map of the Málaga Graben (de la Linde et al., 1996). Contour lines every 100 ms (TWT), showing Andalucía-G1 (And-G1), Alborán-A1 (Alb-A1), DSDP 121, and Site 976 locations. Both flanks of the graben correspond to complex interference of former submarine or formerly emerged surfaces and low- and high-angle normal faults, normal-oblique transfer faults, and tops of rollover structures affecting the basement. Steep surfaces near the Spanish coast correspond to post-Messinian strike-slip or oblique faults that prolongate on land.