Articles | Volume 11, issue 2
https://doi.org/10.5194/se-11-741-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-11-741-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Plio-Quaternary tectonic evolution of the southern margin of the Alboran Basin (Western Mediterranean)
Manfred Lafosse
CORRESPONDING AUTHOR
Institut des Sciences de la Terre Paris, ISTeP UMR 7193, INSU-CNRS, Sorbonne Université, 75005 Paris, France
Tectonic and Structural Geology groups, Department of Earth Sciences, Utrecht University, P.O. Box 80.021, 3508 TA Utrecht, the Netherlands
Elia d'Acremont
Institut des Sciences de la Terre Paris, ISTeP UMR 7193, INSU-CNRS, Sorbonne Université, 75005 Paris, France
Alain Rabaute
Institut des Sciences de la Terre Paris, ISTeP UMR 7193, INSU-CNRS, Sorbonne Université, 75005 Paris, France
Ferran Estrada
Instituto de Ciencias del Mar, ICM-CSIC, Continental Margin Group,
08003 Barcelona, Spain
Martin Jollivet-Castelot
Labratoire d'Océanologie et de Géosciences (LOG), Univ. Lille, CNRS, Univ. Littoral Côte d'Opale, UMR 8187,
59000, Lille,
France
Juan Tomas Vazquez
Juan-Tomas Vazquez, Instituto Español de Oceanografía, Centro Oceanográfico de Málaga, 29640 Fuengirola, Spain
Jesus Galindo-Zaldivar
Dpto. de Geodinámica, Universidad de Granada, Granada, Spain
Instituto Andaluz de Ciencias de la Tierra (CSIC-UGR), Granada,
Spain
Gemma Ercilla
Instituto de Ciencias del Mar, ICM-CSIC, Continental Margin Group,
08003 Barcelona, Spain
Belen Alonso
Instituto de Ciencias del Mar, ICM-CSIC, Continental Margin Group,
08003 Barcelona, Spain
Jeroen Smit
Tectonic and Structural Geology groups, Department of Earth Sciences, Utrecht University, P.O. Box 80.021, 3508 TA Utrecht, the Netherlands
Abdellah Ammar
Département de Géologie, Faculté des Sciences, Université Mohammed V, Avenue Ibn-Batouta, B. P. 1014, Rabat, Morocco
Christian Gorini
Institut des Sciences de la Terre Paris, ISTeP UMR 7193, INSU-CNRS, Sorbonne Université, 75005 Paris, France
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15 citations as recorded by crossref.
- Detailed tectonic reconstructions of the Western Mediterranean region for the last 35 Ma, insights on driving mechanisms A. Romagny et al. 10.1051/bsgf/2020040
- Understanding the complex geomorphology of a deep sea area affected by continental tectonic indentation: The case of the Gulf of Vera (Western Mediterranean) G. Ercilla et al. 10.1016/j.geomorph.2022.108126
- The Neotectonic Deformation of the Eastern Rif Foreland (Morocco): New Insights from Morphostructural Analysis M. Makkaoui et al. 10.3390/app14104134
- Transfer zones in Mediterranean back-arc regions and tear faults L. Jolivet et al. 10.1051/bsgf/2021006
- Lateral variations of pressure-temperature evolution in non-cylindrical orogens and 3-D subduction dynamics: the Betic-Rif Cordillera example E. Bessière et al. 10.1051/bsgf/2021007
- New insights on the Alboran Sea basin extension and continental collision from magnetic anomalies related to magmatism (western Mediterranean) V. Tendero-Salmerón et al. 10.1016/j.margeo.2021.106696
- Slip Partitioning in the 2016 Alboran Sea Earthquake Sequence (Western Mediterranean) D. Stich et al. 10.3389/feart.2020.587356
- Submarine Active Faults and Morpho-Tectonics Around the Iberian Margins: Seismic and Tsunamis Hazards L. Somoza et al. 10.3389/feart.2021.653639
- Evolution of the North Anatolian Fault from a diffuse to a localized shear zone in the North Aegean Sea during the Plio-Pleistocene M. Rodriguez et al. 10.1093/gji/ggad364
- Geomechanical attributes of the Cenozoic sediments of ODP leg 161, western Mediterranean Sea and its implications as geological proxy S. Sen & Ş. Merey 10.1007/s11001-021-09441-1
- Application of Automated Throw Backstripping Method to Characterize Recent Faulting Activity Migration in the Al Hoceima Bay (Northeast Morocco): Geodynamic Implications V. Tendero-Salmerón et al. 10.3389/feart.2021.645942
- Distribution and origin of submarine landslides in the active margin of the southern Alboran Sea (Western Mediterranean Sea) E. d'Acremont et al. 10.1016/j.margeo.2022.106739
- Geodynamic evolution of a wide plate boundary in the Western Mediterranean, near-fieldversusfar-field interactions L. Jolivet et al. 10.1051/bsgf/2021043
- Active negative flower structure at the western edge of the Tunisian Atlas: Morphotectonic evidence from the case study of Borj Edouane-El Gara Quaternary basin R. Azizi et al. 10.1016/j.quaint.2021.07.012
- The Beni Bousera marbles, record of a Triassic-Early Jurassic hyperextended margin in the Alpujarrides-Sebtides units (Rif belt, Morocco) A. Farah et al. 10.1051/bsgf/2021015
14 citations as recorded by crossref.
- Detailed tectonic reconstructions of the Western Mediterranean region for the last 35 Ma, insights on driving mechanisms A. Romagny et al. 10.1051/bsgf/2020040
- Understanding the complex geomorphology of a deep sea area affected by continental tectonic indentation: The case of the Gulf of Vera (Western Mediterranean) G. Ercilla et al. 10.1016/j.geomorph.2022.108126
- The Neotectonic Deformation of the Eastern Rif Foreland (Morocco): New Insights from Morphostructural Analysis M. Makkaoui et al. 10.3390/app14104134
- Transfer zones in Mediterranean back-arc regions and tear faults L. Jolivet et al. 10.1051/bsgf/2021006
- Lateral variations of pressure-temperature evolution in non-cylindrical orogens and 3-D subduction dynamics: the Betic-Rif Cordillera example E. Bessière et al. 10.1051/bsgf/2021007
- New insights on the Alboran Sea basin extension and continental collision from magnetic anomalies related to magmatism (western Mediterranean) V. Tendero-Salmerón et al. 10.1016/j.margeo.2021.106696
- Slip Partitioning in the 2016 Alboran Sea Earthquake Sequence (Western Mediterranean) D. Stich et al. 10.3389/feart.2020.587356
- Submarine Active Faults and Morpho-Tectonics Around the Iberian Margins: Seismic and Tsunamis Hazards L. Somoza et al. 10.3389/feart.2021.653639
- Evolution of the North Anatolian Fault from a diffuse to a localized shear zone in the North Aegean Sea during the Plio-Pleistocene M. Rodriguez et al. 10.1093/gji/ggad364
- Geomechanical attributes of the Cenozoic sediments of ODP leg 161, western Mediterranean Sea and its implications as geological proxy S. Sen & Ş. Merey 10.1007/s11001-021-09441-1
- Application of Automated Throw Backstripping Method to Characterize Recent Faulting Activity Migration in the Al Hoceima Bay (Northeast Morocco): Geodynamic Implications V. Tendero-Salmerón et al. 10.3389/feart.2021.645942
- Distribution and origin of submarine landslides in the active margin of the southern Alboran Sea (Western Mediterranean Sea) E. d'Acremont et al. 10.1016/j.margeo.2022.106739
- Geodynamic evolution of a wide plate boundary in the Western Mediterranean, near-fieldversusfar-field interactions L. Jolivet et al. 10.1051/bsgf/2021043
- Active negative flower structure at the western edge of the Tunisian Atlas: Morphotectonic evidence from the case study of Borj Edouane-El Gara Quaternary basin R. Azizi et al. 10.1016/j.quaint.2021.07.012
Latest update: 01 Nov 2024
Short summary
The Alboran Sea is one of the most active region of the Mediterranean Sea. There, the basin architecture records the effect of the Africa–Eurasia plates convergence. We evidence a Pliocene transpression and a more recent Pleistocene tectonic reorganization. We propose that main driving force of the deformation is the Africa–Eurasia convergence, rather than other geodynamical processes. It highlights the evolution and the geometry of the present-day Africa–Eurasia plate boundary.
The Alboran Sea is one of the most active region of the Mediterranean Sea. There, the basin...