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 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 …

Including faults as seismogenic sources in probabilistic seismic hazard assessments
(PSHA) has turned into a common practice as knowledge of active faults is improving …

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 …

Constraining the date of the last major event occurred in a fault is of paramount importance
in probabilistic seismic hazard assessment when time-dependent models are considered …

In regions with slow‐moving faults, the incompleteness of earthquake and fault data
complicates the study of seismic hazard. The instrumental and historical seismic catalogs …

In this work, we prove the usefulness of morphometric analyses, typically applied to basin-
border faults, to define the tectonic geomorphology of a slow-moving, intrabasinal structure …

Fault slip rate is one of the most crucial parameters to characterize earthquake occurrence in
fault‐based seismic hazard assessments (SHA). Accordingly, paleoseismic studies have …