Based on more than 4,500 km of new and re-processed multichannel seismic lines, high-
resolution seafloor bathymetry, available well data, and basement dredge samples, we have …

Landslide research has benefited greatly from advances in remote sensing techniques.
However, the recent increase in available data on land surface movement provided by …

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 …

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 …

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 …

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 …

The Gibraltar Arc includes the Betic and Rif Cordilleras surrounding the Alboran Sea; it is
formed at the northwest–southeast Eurasia–Nubia convergent plate boundary in the …

Abstract The Eurasian‐African NW‐SE oblique plate convergence produces shortening and
orthogonal extension in the Alboran Sea Basin (westernmost Mediterranean), located …

Abstract The Guadalquivir Accretionary Complex forms a largely oblique prism at the
northern edge of the Betic‐Rif orogen, where Miocene sediments plus allochthonous …

Abstract The central Betic Cordillera, southern Spain, is affected by an uplift related to the
NNW–SSE Eurasia‐Nubia convergence and shallow ENE–WSW orthogonal extension …