The coexistence of shortening and extensional tectonic regimes is a common feature in orogenic belts. The westernmost end of the Western Mediterranean is an area undergoing shortening related to the 5 mm/yr NNW‒SSE convergence of the Nubia and Eurasia Plates. In this region, the Central Betic Cordillera shows a regional ENE‒WSW extension. Here, we present GNSS-derived geodetic data along a 170 km-long transect orthogonal to the main active normal faults of the Central Betic Cordillera. Our data indicate that the total extension rate along the Central Betic Cordillera is 2.0 ± 0.3 mm/yr. Extension is accommodated in the eastern (0.8 ± 0.3 mm/yr in the Guadix-Baza Basin) and western (1.3 ± 0.3 mm/yr in the Granada Basin) parts of the Central ...
The Gibraltar arc and surrounding areas are a complex tectonic region and its tectonic evolution.sin...
The Malaga Basin is located in the westernmost part of the Betic Cordillera. This alpine cordillera ...
The Betic Cordillera of southern Spain forms a clear example of a collisional orogen that has underg...
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...
The eastern Betic Cordillera, south-eastern Spain, is one of the most seismically active area within...
The Gibraltar Arc includes the Betic and Rif Cordilleras surrounding the Alboran Sea; it is formed a...
Based on new seismological and recent faulting data, we analyze five main sectors in the western par...
The late Paleozoic collision between Gondwana and Laurussia resulted in the polyphase deformation an...
Some of the contacts between the superimposed tectonic units in the region of Aguilas-Mazarrón, in t...
The Betic (Southern Spain) and the Rif (Morocco) mountain chains, connected through the Gibraltar St...
Memoria de tesis doctoral presentada por Víctor Tendero Salmerón para obtener el título de Doctor en...
We present the first GPS‐derived geodetic observations from the NE end of the Eastern Betic Shear Zo...
The Betic Cordilleras in southern Spain have experienced a number of moderate to strong seismic even...
Les cordillères Bético-Rifaines sont situées en Méditerranée occidentale, où elles forment un arc ét...
The Gibraltar arc and surrounding areas are a complex tectonic region and its tectonic evolution.sin...
The Malaga Basin is located in the westernmost part of the Betic Cordillera. This alpine cordillera ...
The Betic Cordillera of southern Spain forms a clear example of a collisional orogen that has underg...
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...
The eastern Betic Cordillera, south-eastern Spain, is one of the most seismically active area within...
The Gibraltar Arc includes the Betic and Rif Cordilleras surrounding the Alboran Sea; it is formed a...
Based on new seismological and recent faulting data, we analyze five main sectors in the western par...
The late Paleozoic collision between Gondwana and Laurussia resulted in the polyphase deformation an...
Some of the contacts between the superimposed tectonic units in the region of Aguilas-Mazarrón, in t...
The Betic (Southern Spain) and the Rif (Morocco) mountain chains, connected through the Gibraltar St...
Memoria de tesis doctoral presentada por Víctor Tendero Salmerón para obtener el título de Doctor en...
We present the first GPS‐derived geodetic observations from the NE end of the Eastern Betic Shear Zo...
The Betic Cordilleras in southern Spain have experienced a number of moderate to strong seismic even...
Les cordillères Bético-Rifaines sont situées en Méditerranée occidentale, où elles forment un arc ét...
The Gibraltar arc and surrounding areas are a complex tectonic region and its tectonic evolution.sin...
The Malaga Basin is located in the westernmost part of the Betic Cordillera. This alpine cordillera ...
The Betic Cordillera of southern Spain forms a clear example of a collisional orogen that has underg...