Distribution and origin of submarine landslides in the active margin of the southern Alboran Sea (Western Mediterranean Sea)
- 1Sorbonne Université, CNRS-INSU, Institut des Sciences de la Terre Paris, ISTeP, F-75005 Paris, France
- 2Instituto de Ciencias del Mar, CSIC, 08003 Barcelona, Spain
- 3Instituto Español de Oceanografía (IEO), C.O. Málaga, 29640 Fuengirola, Málaga, Spain
- 4Flanders Marine Institute (VLIZ), Wandelaarkaai 7, 8400, Oostende, Belgium
- 5Department of Geology, Ghent University, Krijgslaan 281 S8, 9000, Gent, Belgium
- 6Instituto Español de Oceanografía (IEO), C.O. Cádiz, 11006 Cádiz, Spain
- 7Géoazur, Université de Nice-Sophia Antipolis-CNRS-OCA, France
- 8National Institute of Oceanography and Applied Geophysics - OGS, 34010, Sgonico, TS, Italy
- 9Laboratoire de Géologie, Ecole normale supérieure, PSL research university, CNRS UMR 8538, 24 rue Lhomond, 75005 Paris, France
- 10Université Abdelmalek Essaadi, Morocco
- 11Université Mohammed V-Agdal, Rabat, Morocco
In the South Alboran Sea, the moderate seismicity (Mw=6.4) of the strike-slip Al Idrissi Fault Zone does not appear to control directly the landslides distribution. To provide a preliminary geohazard assessment, we characterized the spatial distribution, the volume and the ages of the submarine landslides from multibeam and seismic reflection data in the southern part of the Alboran Sea. Since the Quaternary numerous submarine landslide processes affect the marine sedimentary cover with volumes of the mass transport deposits (MTD) estimated between 0.01 to 15 km3.
West of the Al Idrissi Fault Zone, along the South Alboran Ridge’s northern flank, the distribution of the MTD follows the SW-NE bank and ridge trend that correlates with blind thrusts and folds covered by a plastered contourite drift. A pockmark field, related to fluid escape, is visible near landslide scars where the contourite drift is relatively thicker. In this area, landslide scars occur on variable slopes (2-24°) and their associated MTD have variable decompacted volumes (0.01-10km3). East of the Al Idrissi Fault Zone, between the Alboran Ridge and the Pytheas Bank, the mapped MTDs have uneven volumes. The smaller ones (<1 km3) have their slide scars on steep slopes (>10°), whereas those of the largest ones (3-15 km3) occur on gentler slopes (<5°).
These observations and a slope stability analysis suggest that the combination of seismic shaking, blind thrusts activity, relatively high sedimentation of contourite deposits, and fluid escape dynamics are likely the main controlling mechanisms rather than seismic shaking only. These causal factors would explain the concentration of landslide head scarps at the edge of the thickest parts of the contourite drifts (i.e. crests) may have been controlled locally by fluid overpressures in line with blind thrusts. Additionally, low to moderate seismicity potentially triggered by nearby faults might regionally have played a role in destabilising the seafloor sediments since 1.12 Ma, which coincides with the propagation of the Al Idrissi Fault Zone in the southern Alboran Sea.
How to cite: d'Acremont, E., Lafuerza, S., Rabaute, A., Lafosse, M., Jollivet Castelot, M., Gorini, C., Alonso, B., Ercilla, G., Vazquez, J. T., Vandorpe, T., Juan, C., Migeon, S., Ceramicola, S., Lopez-Gonzalez, N., Rodriguez, M., El Moumni, B., Benmarha, O., and Ammar, A.: Distribution and origin of submarine landslides in the active margin of the southern Alboran Sea (Western Mediterranean Sea), EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-5341, https://doi.org/10.5194/egusphere-egu22-5341, 2022.
