Authors: Hector Perea, James Holmes and Neal Driscoll.

Meeting: Fault2SHA 2019 workshop in Barcelona (Spain).

We presented an interpretation of the high-resolution seismic 3D seismic dataset in the offshore Southern California between Los Angeles and San Diego. The results show the presence of a complex fault system developed in a shear zone along the Newport-Inglewood Rose Canyon fault.

Authors: Eulàlia Gràcia, Ingo Grevemeyer, Rafael Bartolomé, Hector Perea, Sara Martínez-Loriente, Laura Gómez de la Peña, Antonio Villaseñor, Yann Klinger, Claudio Lo Iacono, Susana Diez, Alcinoe Calahorrano, Miquel Camafort, Sergio Costa, Elia d’Acremont, Alain Rabaute and César R. Ranero.

Meeting: Fault2SHA 2019 workshop in Barcelona (Spain).

We report evidence of left-lateral strike-slip displacement along the Al-Idrissi fault, characterize their fault segments and demonstrate that the fault was the source of the 2016 events.

Authors: Hector Perea, James Holmes and Neal Driscoll.

Meeting: AGU 2018 Fall meeting in Washington DC (US).

We presented a preliminary interpretation of the high-resolution seismic 3D seismic dataser in the offshore along the Newport-Inglewood Rose Canyon fault, in the offshore Southern California between Los Angeles and San Diego.

Authors: Rodrigo León, Pierre Lacan, Hector Perea, María Ortuño and Ramón Zuñiga.

Meeting: RAUGM 2018 Annual Meeting in Puerto Vallarta (Mexico).

A study of the Coulomb stress transfer has been done to show the influence of the 1912 Acambay earthquake, produced in the Acambay fault in the Trans-Mexican Volcanic Belt, to understand the distribution of the regional seismicity after the earthquake and reveal the faults that accumulated stress due to this event and that could be close to rupture in a future event.

Authors: Yuval Levy, Tom Rockwell, John Shaw, Andreas Plesch, Neal Driscoll and Hector Perea.

Meeting: SCEC 2018 Annual Meeting in Palm Springs (US).

To test different interpretations for the evolution and structure of the WTR, we used Trishear forward modelling. The Trishear models are a good first-order match to published geologic maps and well data. The modelling of multiple cross-sections argues that all of the observed deformation can be explained by an evolving fold and thrust belt, which includes a regionally extensive decollement underlying the observed thrusts and folds.

Authors: Eulàlia Gràcia, Ingo Grevemeyer, Rafael Bartolomé, Hector Perea, Sara Martínez-Loriente, Laura Gómez De La Peña, Antonio Villaseñor, Miquel Camafort, Cristina Sanchez Serra and César R. Ranero.

Meeting: ESC 2018 General Assembly in Valletta (Malta).

We report evidence of left-lateral strike-slip displacement in the Al-Idrissi fault, characterize their fault segments and demonstrate that this is a basement fault and the source of the 2016 earthquake events. Located along a lithospheric boundary, the Al-Idrissi Fault System is a young structure.

Authors: Eulàlia Gràcia, Rafael Bartolomé, Hector Perea, Sara Martínez-Loriente, Laura Gómez De La Peña, Miquel Camafort, Claudio Lo Iacono, Cristina Sanchez Serra, William Meservy, Eulàlia Masana, Ingo Grevemeyer and César R. Ranero.

Meeting: Iberfault 2018 in Alicante (Spain).

We present an overview of the three largest continental strike-slip fault systems in the Alboran Basin: Carboneras, Yusuf and Al-Idrissi. Our dataset results from an integration of different types of acoustic and seismic data. This data is used to map and characterize better the active fault systems.

Authors: Yuval Levy, Tom Rockwell, John Shaw, Andreas Plesch, Neal Driscoll and Hector Perea.

Meeting: SSA 2018 Annual Meeting in Miami (US).

To test different interpretations for the evolution and structure of the WTR, we used Trishear forward modelling. The Trishear models are a good first-order match to published geologic maps and well data. The modelling of multiple cross-sections argues that all of the observed deformation can be explained by an evolving fold and thrust belt, which includes a regionally extensive decollement underlying the observed thrusts and folds.

Authors: Laura Gómez de la Peña, César Ranero, Eulàlia Gràcia, Hector Perea, Guillermo Booth-Rea and Jose Miguel Azañón.

Meeting: EGU General Assembly 2018 in Vienna (Austria).

In this study, we estimate the total slip accommodated by the most prominent tectonic structures in the Alboran sea since the earliest Pliocene. Results show that estimated total slip accommodated by the main fault system may be similar (with error bounds) to the estimated plate convergence value since the Messinian time.

Authors: Hector Perea, Gülsen Ucarkus, Neal Driscoll, Graham Kent, Yuval Levy and Thomas Rockwell.

Meeting: PATA 2017 Annual Meeting in Blenheim (New Zealand).

We presented the high-resolution seismic CHIRP profiles and the analysis of the Holocene deformation events (paleoearthquakes) in different folding and faulting systems in the offshore between Ventura and Santa Barbara cities.

Authors: Hector Perea, Gülsen Ucarkus, Neal Driscoll, Graham Kent, Yuval Levy and Thomas Rockwell.

Meeting: SCEC 2017 Annual Meeting in Palm Springs (US).

We presented the high-resolution seismic CHIRP profiles showing Holocene active tectonic deformation in the offshore between Ventura and Santa Barbara cities.

Authors: Hector Perea, Gülsen Ucarkus, Neal Driscoll, Graham Kent and Thomas Rockwell.

Meeting: SSA 2017 Annual Meeting in Denver (US).

We presented the preliminary results on the Quaternary active tectonic deformation in the offshore between Ventura and Santa Barbara cities using high-resolution CHIRP seismic data.

Authors: Hector Perea, Eulàlia Gràcia, Rafael Bartolomé, Sara Martínez-Loriente, Laura Gómez de la Peña, Ximena Moreno, Claudio Lo Iacono, Susana Diez, Olvido Tello, María Gómez-Ballesteros, Ben de Mol and Juanjo Dañobeitia.

Meeting: FLOWS 2016 meeting (https://www.flows-cost.eu/) (COST Action ES1301) in Barcelona (Spain).

We presented the Averroes faults and North Averroes faults in the Alboran Sea (western Mediterranean), their kinematics and evolution, and characterized their seismic hazard.