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 Basin, in the Betic Cordillera, is a region affected by shallow brittle deformation, as it was the scenario for the recent Granada 2021 seismic sequence. This seismicity presented a swarm behavior at the beginning of the sequence, followed by mainshock-aftershock features. Geological and gravity data presented here reveal that the basement is affected by two sets of NW-SE and NE-SW normal faults and intensely deformed by vertical NW-SE joints. Improved relocation of the Granada 2021 seismicity reveals a confined chim...
The northwestern area of the Iberian Peninsula traditionally is considered a seismically stable area...
The northwest of Iberia experiences important tectonic activity that has led to several episodes of ...
The coexistence of shortening and extensional tectonic regimes is a common feature in orogenic belts...
Understanding active tectonics and seismicity in extensional settings requires the analysis of high-...
A fault database has been created for the Granada basin (S Spain) concerning seismic potential in th...
The Betic Cordilleras in southern Spain have experienced a number of moderate to strong seismic even...
The Granada and Guadix-Baza Basins, the largest Neogene-Quaternary intramontane basins of the Betic ...
This study was supported by FEDER/MINECO projects CGL2015-67130-C2-2-R and PID2019-109608GB-I00, FED...
The geometry and kinematics of active faults have a significant impact on their seismic potential. I...
Perea, Héctor ... et al.-- 11 pages, 8 figures, 2 tables, supplementary data https://doi.org/10.1016...
The injection of fluids into the crust can modify the governing stress state and therefore generate ...
Several major N80ºE faults occur in the Bullas-Mula area (SE Spain). These faults and the numerous t...
Several major N80ºE faults occur in the Bullas-Mula area (SE Spain). These faults and the numerous t...
X Congreso Geológico de España, 5-7 Julio 2021, Vitoria - GasteizLa región Cantábrica, al tratarse d...
The Malaga Basin is located in the westernmost part of the Betic Cordillera. This alpine cordillera ...
The northwestern area of the Iberian Peninsula traditionally is considered a seismically stable area...
The northwest of Iberia experiences important tectonic activity that has led to several episodes of ...
The coexistence of shortening and extensional tectonic regimes is a common feature in orogenic belts...
Understanding active tectonics and seismicity in extensional settings requires the analysis of high-...
A fault database has been created for the Granada basin (S Spain) concerning seismic potential in th...
The Betic Cordilleras in southern Spain have experienced a number of moderate to strong seismic even...
The Granada and Guadix-Baza Basins, the largest Neogene-Quaternary intramontane basins of the Betic ...
This study was supported by FEDER/MINECO projects CGL2015-67130-C2-2-R and PID2019-109608GB-I00, FED...
The geometry and kinematics of active faults have a significant impact on their seismic potential. I...
Perea, Héctor ... et al.-- 11 pages, 8 figures, 2 tables, supplementary data https://doi.org/10.1016...
The injection of fluids into the crust can modify the governing stress state and therefore generate ...
Several major N80ºE faults occur in the Bullas-Mula area (SE Spain). These faults and the numerous t...
Several major N80ºE faults occur in the Bullas-Mula area (SE Spain). These faults and the numerous t...
X Congreso Geológico de España, 5-7 Julio 2021, Vitoria - GasteizLa región Cantábrica, al tratarse d...
The Malaga Basin is located in the westernmost part of the Betic Cordillera. This alpine cordillera ...
The northwestern area of the Iberian Peninsula traditionally is considered a seismically stable area...
The northwest of Iberia experiences important tectonic activity that has led to several episodes of ...
The coexistence of shortening and extensional tectonic regimes is a common feature in orogenic belts...