New geophysical and geological evidence for the present day southernmost active deformational front of the Rif thrust-and-fold belt and the oceanic accretionary prism of Cadiz: the Dhar Doum–Lalla Zahra fault, Northwestern Atlantic Coastal Morocco

• Published in: Environmental earth sciences 2012-12, Vol.67 (8), p.2411-2422
• Main Authors: Toto, E. A, El Miloudi, A, El Basri, M, Hafid, M, Zouhri, L, El Mouraouah, S, Benammi, M, El Mouraouah, A, Iben Brahim, A, Birouk, A, Kasmi, M
• Format: Article
• Language: English
• Subjects: Biogeosciences; Earth and Environmental Science; Earth Sciences; Environmental Science and Engineering; Geochemistry; Geology; geophysics; hazard characterization; Hydrology/Water Resources; Original Article; Terrestrial Pollution; tomography
• ISSN: 1866-6280; 1866-6299
• DOI: 10.1007/s12665-012-1692-1

Combining the results from field observations, high resolution 2D-electric resistivity and high resolution seismic refraction tomography, we have found new evidence for active faulting in the Dhar Doum area, northwestern Atlantic coast of Morocco. Qualitative interpretation of the inverted resistivity and seismic refraction data reveals the presence of two thrust faults that cut the topographic surface and displace the most recent sedimentary deposits. Furthermore, one of these seismically imaged faults strongly correlates with the Dhar Doum–Lalla Zahra fault. The steepening at the surface and the flattening with depth of this fault are likely to indicate an important strike-slip component associated with a major reverse component. If extended offshore to the west, the Dhar Doum fault could be a continuation of the southernmost deformational front of the Cadiz oceanic accretionary prism. Therefore, this structure is very likely to represent the actual active southern deformational front of the oceanic accretionary prism, as well as that of the Rif fold-and-thrust belt. The southward thickening of the growth strata composing the uppermost dune system and the occurrence of Plio-Quaternary conglomerates north of the Dhar Doum–Lalla Zahra fault suggest that the neotectonic activity may have started by the end of the Pliocene and have continued to the present as indicated by the folding-and-faulting of the most recent sedimentary deposits and the presence of high scarps. The identification of active faulting in the study area that may have a profound influence on seismic hazard analysis of the whole Rif foredeep basin.