Figure 11. Scheme of crustal and sedimentary compressive deformation focused by the presence of a serpentinized peridotite ridge. The prolongation of the major synsedimentary reverse fault occurs along the contact between the serpentinized PR and the sedi

Figure 11. Scheme of crustal and sedimentary compressive deformation focused by the presence of a serpentinized peridotite ridge. The prolongation of the major synsedimentary reverse fault occurs along the contact between the serpentinized PR and the sedimentary cover. Dotted areas correspond to sediments deformed during the Betic compressive phase.