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 …

Abstract The Granada Basin is a slowly deforming intramountain basin in the Betic
Cordillera (S-Spain). Despite historical and paleoseismological evidence for M6 …

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 …

Abstract The 2020–2021 Santa Fe seismic sequence is the first well‐instrumented and
widely felt seismic series occurred in the Granada basin during the Spanish instrumental …

Distributed acoustic sensing (DAS) is an innovative technology with great potential for
acquiring seismic data sets in urban areas. In this work, we check the suitability of a DAS …

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 …

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 …

Back-arc basins in subduction systems usually form following discrete subduction-related
extension stages. However, in the westernmost Mediterranean, the initiation of Cenozoic …

The Betic Cordillera was formed by the collision between the Alboran Domain and the South
Iberian paleomargin in the frame of the NW–SE convergent Eurasia–Nubia plate boundary …

Seismic surveys are crucial for investigating subsurface geological formations and require
significant logistical and economic resources. This study reuses legacy seismic surveys from …