Please use this identifier to cite or link to this item:
logo share SHARE logo core CORE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE

Invite to open peer review

A first appraisal of the seismogenic and tsunamigenic potential of the largest fault systems in the westernmost Mediterranean

AuthorsGómez de la Peña, L. CSIC ORCID; Gràcia, Eulàlia CSIC ORCID ; Maesano, Francesco; Basili, Roberto; Kopp, Heidrun; Sànchez-Serra, Cristina CSIC ORCID ; Scala, Antonio; Romano, Fabrizio; Volpe, Manuela; Piatanesi, Alessio; Ranero, César R. CSIC ORCID
KeywordsWestern Mediterranean
Seismogenic potential
Tsunamigenic potential
Numerical modelling
Active faults
Active seismic data
Issue DateMar-2022
CitationMarine Geology 445: 106749 (2022)
AbstractThe westernmost Mediterranean hosts part of the plate boundary between the European and African tectonic plates. Based on the scattered instrumental seismicity, this boundary has been traditionally interpreted as a wide zone of diffuse deformation. However, recent seismic images and seafloor mapping studies support that most of the plate convergence may be accommodated in a few tectonic structures, rather than in a broad region. Historical earthquakes with magnitudes Mw > 6 and historical tsunamis support that the low-to-moderate instrumental seismicity might also have led to underestimation of the seismogenic and tsunamigenic potential of the area. We evaluate the largest active faults of the westernmost Mediterranean: the reverse Alboran Ridge, and the strike-slip Carboneras, Yusuf and Al-Idrissi fault systems. For the first time, we use a dense grid of modern seismic data to characterize the entire dimensions of the main fault systems, accurately describe the geometry of these structures and estimate their seismic source parameters. Tsunami scenarios have been tested based on 3D-surfaces and seismic source parameters, using both uniform and heterogeneous slip distributions. The comparison of our results with previous studies, based on limited information on the fault geometry and kinematics, indicates that accurate fault geometries and heterogeneous slip distributions are needed to properly assess the seismic and tsunamigenic potential in this area. Based on fault scaling relations, the four fault systems have a large seismogenic potential, being able to generate earthquakes with Mw > 7. The reverse Alboran Ridge Fault System has the largest tsunamigenic potential, being able to generate a tsunami wave amplitude greater than 3 m in front of the coasts of Southern Spain and Northern Africa
Description15 pages, 10 figures, 3 tables, supplementary material Data availability: The data (3D complex mesh of the ARFS and rake values, and the resulting grid files of the tsunami simulations containing the maximum wave amplitude) are archived at PANGAEA repository ( The EMODnet bathymetry is available at The stochastic slip distributions have been produced by the code ANTI-FASc ( a platform partially based on the code k223d (Herrero and Murphy, 2018 available at, in turn based on the slipk2 (available at and the trilateration codes (available at
Publisher version (URL)
Appears in Collections:(ICM) Artículos

Files in This Item:
Show full item record

CORE Recommender


checked on Apr 10, 2024

Page view(s)

checked on Apr 16, 2024


checked on Apr 16, 2024

Google ScholarTM




WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.