EGU2020-3125
https://doi.org/10.5194/egusphere-egu2020-3125
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Earthquake crisis unveils the growth of an incipient continental fault system

Eulàlia Gràcia1, Ingo Grevemeyer2, Rafael Bartolomé1, Héctor Perea3, Sara Martínez-Loriente1, Laura Gómez de la Peña2, Antonio Villaseñor1, Yann Klinger4, Claudio Lo Iacono1, Susana Diez5, Alcinoe Calahorrano1, Miquel Camafort1, Sergio Costa1, Elia d'Acremont6, Alain Rabaute6, and César R. Ranero1
Eulàlia Gràcia et al.
  • 1Institut de Ciències del Mar - CSIC, Barcelona, Spain (egracia@icm.csic.es, rafael@icm.csic.es, smartinez@icm.csic.es, antonio.villasenor@csic.es, loiacono@icm.csic.es, acalahor@icm.csic.es, camafort@icm.csic.es, pitiuso@gmail.com, cranero@icm.csic.es)
  • 2GEOMAR, Helmholtz Centre for Ocean Research, 24148 Kiel, Germany (igrevemeyer@geomar.de)
  • 3Universidad Complutense de Madrid, Facultad de Ciencias Geológicas, 28040 Madrid, Spain (hperea01@ucm.es)
  • 4Institut de Physique du Globe de Paris, Sorbonne Paris Cité CNRS, 75005 Paris, France (klinger@ipgp.fr)
  • 5Unitat de Tecnologia Marina, UTM-CSIC, 08003 Barcelona, Spain (sdiez@utm.csic.es)
  • 6Sorbonne Universités, UPMC, Univ. Paris 6, CNRS-ISTEP, 75252 Paris, France (elia.dacremont@sorbonne-universite.fr; alain.rabaute@upmc.fr)

Large continental faults extend for thousands of kilometres and often form the tectonic boundaries between plates that are associated with prominent topographic features. In these active areas, well-defined faults produce large earthquakes, and thus imply a high seismic hazard. These paradigms are called into question in the Alboran Sea, which hosts an allegedly complex diffuse boundary between the Eurasia and Nubia plates, and we discovered one of the few examples worldwide of the initial stages of these key tectonic structures. On the 25th January 2016, a magnitude Mw6.4 submarine earthquake struck the north of the Moroccan coast, the largest event ever recorded in the Alboran Sea. The quake was preceded by an earthquake of magnitude Mw5.1 and was followed by numerous aftershocks whose locations mainly migrated to the south. The mainshock nucleated at a releasing bend of the poorly known Al-Idrissi Fault System (AIFS). According to slip inversion and aftershock distribution, we assume a rupture length of 18 km. Here we combine newly acquired multi-scale bathymetric and marine seismic reflection data with a resolution comparable to the studies on land, together with seismological data of the 2016 Mw 6.4 earthquake offshore Morocco – the largest event recorded in the area – to unveil the 3D geometry of the AIFS. We found that, despite its subdued relief, the AIFS is a crustal-scale boundary. We report evidence of left-lateral strike-slip displacement, characterize their fault segments and demonstrate that the AIFS is the source of the 2016 events. The occurrence of the Mw 6.4 earthquake and previous events of 1994 and 2004 supports that the AIFS is currently growing through propagation and linkage of its segments, which eventually might generate a greater rupture (up to Mw 7.6), increasing the potential hazard of the structure. The AIFS provides a unique model of the inception and growth of a young plate boundary system in the Alboran Sea (Western Mediterranean).

This work has been recently published in Nature Communications (IF:12.35), 10, 3482 (2019) doi:10.1038/s41467-019-11064-5. I would like to present our article recently published in NCOMM, so, please consider our work for an ORAL INVITED presentation. Many thanks!

How to cite: Gràcia, E., Grevemeyer, I., Bartolomé, R., Perea, H., Martínez-Loriente, S., Gómez de la Peña, L., Villaseñor, A., Klinger, Y., Lo Iacono, C., Diez, S., Calahorrano, A., Camafort, M., Costa, S., d'Acremont, E., Rabaute, A., and Ranero, C. R.: Earthquake crisis unveils the growth of an incipient continental fault system, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3125, https://doi.org/10.5194/egusphere-egu2020-3125, 2020

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