Initial SE-dipping slow subduction of the Ligurian–Tethys lithosphere beneath Africa from
Late Cretaceous to middle Oligocene twisting to a later faster E-dipping subduction of the …

The present review paper is an attempt to summarize quantitative evidence of Late
Cenozoic changes in topographic relief. Different meanings of the word “relief”, as it is …

We map the lithospheric structure under the westernmost Mediterranean convergent setting
interpreting P-receiver functions obtained from a dense seismic network. No orogenic root …

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 have performed a geomorphic analysis of the Sierra Nevada, the highest range of the
Betic Cordillera (SE Spain), with the aim to elucidate its late Miocene to present-day …

We present the first comprehensive geodatabase of glacial cirques on the Iberian Peninsula,
excluding the Pyrenees. A total of 1519 cirques were mapped using Google Earth, guided …

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 …

We integrated optically stimulated luminescence dating and 10Be cosmogenic nuclide
measurements to quantify short‐to‐medium‐term (102–104 years) catchment dynamics and …

The landscape evolution in Neogene intramontane basins is a result of the interaction of
climatic, lithologic, and tectonic factors. When sedimentation ceases and a basin enters an …

The interplay between structural and metamorphic processes operating along the deep
plate interface in subduction zones remains elusive as much of the geologic record is …