Abstract The Gulf of Cadiz and the Alboran Sea are characterized by tectonic activity due to
oblique convergence at the boundary between the Eurasian and Nubian plates. This activity …

Early marine diagenetic dolomite is a rather thermodynamically‐stable carbonate phase and
has potential to act as an archive of marine porewater properties. However, the variety of …

The distribution of active faults in the Iberian Peninsula is not homogeneous, being mainly
present, but not only, in areas affected by the Alpine Orogeny. They are located in several …

The low frequency of large destructive earthquakes in the Eastern Betics (SE Iberian
Peninsula), not recorded in the instrumental seismic catalog, complicate the estimation of …

We present an improved neotectonic numerical model of the complex NW Africa‐SW
Eurasia plate boundary segment that runs from west to east along the Gloria Fault up to the …

The aim of this work is to make a synthesis at regional scale focused on the geophysical
characterization of submarine faults around the Iberian margin to identify active structures …

We present the first GPS‐derived geodetic observations from the NE end of the Eastern
Betic Shear Zone obtained from the Bajo Segura GPS network (SE Spain). The network has …

Fault slip rate variability over time is a crucial aspect for understanding how single faults
interact among each other in fault systems. Several studies worldwide evidence the …

To define the seismic potential of the left-lateral strike-slip Alhama de Murcia fault (SE
Iberian Peninsula), we calculated its slip rate by measuring offset linear features of known …

The Miocene is an essential period in the configuration of the present-day relief of the Betic
Cordillera and the South Iberian continental margin, which determined the structure and …