• High- and Low-Angle Normal Fault Activity in a Collisional Orogen: The Northeastern Granada Basin (Betic Cordillera) 

      Madarieta-Txurruka, Asier; Galindo‐Zaldivar, Jesus; González-Castillo, Lourdes; Peláez, José A; Ruiz-Armenteros, Antonio M.; Henares, Jesús ; Garrido-Carretero, María Selmira; Avilés, Manuel; Gil, Antonio J. (John Wiley and Sons Inc, 2021)
      Understanding active tectonics and seismicity in extensional settings requires the analysis of high-angle normal faults (HANFs) and the transfer of deformation at depth. The debate surrounds the role of low-angle normal ...
    • Seismicity in Strike‐Slip Foreland Faults (Central Betic Cordillera Front): Evidence of Indentation Tectonics 

      Tendero‐Salmerón, Víctor; Galindo‐Zaldivar, Jesus; Peláez, José A; Martínez‐Martos, Manuel; Henares, Jesús ; Marín‐Lechado, Carlos; Gil, Antonio J.; López‐Garrido, Ángel Carlos (Tectonics, 27/05/2020)
      Unexpected seismicity has been detected in the past few years along the northern Guadiana Menor River (Guadalquivir foreland basin) at the northern boundary of the Betic Cordillera. Earthquake focal mechanisms evidence the ...
    • Stochastic Modeling of the Al Hoceima (Morocco) Aftershock Sequences of 1994, 2004 and 2016 

      Hamdache, M.; Peláez, José A; Gospodinov, Dragomir; Henares, Jesús; Galindo‐Zaldivar, Jesus; Sanz de Galdeano, Carlos; Ranguelov, Boyko (Applied Sciences, 2022)
      The three aftershock sequences that occurred in Al Hoceima, Morocco, in May 1994 (Mw 6.0), February 2004 (Mw 6.4) and January 2016 (Mw 6.3) were stochastically modeled to investigate their temporal and energetic behavior. ...
    • The Role of Faults as Barriers in Confined Seismic Sequences: 2021 Seismicity in the Granada Basin (Betic Cordillera) 

      Madarieta-Txurruka, Asier; González-Castillo, Lourdes; Peláez, José A; Catalán, Manuel; Henares, Jesús; Gil, Antonio J.; Lamas-Fernández, Francisco; Galindo‐Zaldivar, Jesus (Tectonics, 2022)
      Fault barriers are key structures for studying seismic hazard in regions of intense brittle deformation. The interaction between fault sets affects their seismogenic behavior, if some of them act as barriers. The Granada ...