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Geodynamic evolution of the central and western Mediterranean: Tectonics vs. igneous petrology constraints
We present a geodynamic reconstruction of the Central–Western Mediterranean and
neighboring areas during the last 50Myr, including magmatological and tectonic …
neighboring areas during the last 50Myr, including magmatological and tectonic …
Lateral slab deformation and the origin of the western Mediterranean arcs
The western Mediterranean subduction zone (WMSZ) extends from the northern Apennine
to southern Spain and turns around forming the narrow and tight Calabrian and Gibraltar …
to southern Spain and turns around forming the narrow and tight Calabrian and Gibraltar …
Active tectonics in the Sierra Nevada (Betic Cordillera, SE Spain): Insights from geomorphic indexes and drainage pattern analysis
The Sierra Nevada of the central Betic Cordillera is a 3000m-high mountain range
surrounded by Neogene–Quaternary sedimentary basins, having been uplifted since Late …
surrounded by Neogene–Quaternary sedimentary basins, having been uplifted since Late …
Evidence for active subduction beneath Gibraltar
We report on a marine seismic survey that images an active accretionary wedge west of
Gibraltar. Ramp thrusts offset the seafloor and sole out to an east-dip** décollement …
Gibraltar. Ramp thrusts offset the seafloor and sole out to an east-dip** décollement …
Arabia-Eurasia continental collision: Insights from late Tertiary foreland-basin evolution in the Alborz Mountains, northern Iran
A poorly understood lag time of 15–20 my exists between the initial Arabia-Eurasia
continental collision in late Eocene to early Oligocene time and the acceleration of tectonic …
continental collision in late Eocene to early Oligocene time and the acceleration of tectonic …
Kinematics of the Iberia–Maghreb plate contact from seismic moment tensors and GPS observations
The Iberian Peninsula and the Maghreb experience moderate earthquake activity and
oblique,∼ NW–SE convergence between Africa and Eurasia at a rate of∼ 5 mm/yr. Coeval …
oblique,∼ NW–SE convergence between Africa and Eurasia at a rate of∼ 5 mm/yr. Coeval …
Seismic sources on the Iberia-African plate boundary and their tectonic implications
The plate boundary between Iberia and Africa has been studied using data on seismicity
and focal mechanisms. The region has been divided into three areas: A; the Gulf of Cadiz; B …
and focal mechanisms. The region has been divided into three areas: A; the Gulf of Cadiz; B …
Geodynamic evolution of the lithosphere and upper mantle beneath the Alboran region of the western Mediterranean: Constraints from travel time tomography
A number of different geodynamic models have been proposed to explain the extension that
occurred during the Miocene in the Alboran Sea region of the western Mediterranean …
occurred during the Miocene in the Alboran Sea region of the western Mediterranean …
How does the Alpine belt end between Spain and Morocco?
A Michard, A Chalouan, H Feinberg… - Bulletin de la …, 2002 - pubs.geoscienceworld.org
Abstract The Betic-Rif arcuate mountain belt (southern Spain, northern Morocco) has been
interpreted as a symmetrical collisional orogen, partly collapsed through convective removal …
interpreted as a symmetrical collisional orogen, partly collapsed through convective removal …
Moment tensor solutions for small and moderate earthquakes in the Ibero‐Maghreb region
We applied time domain moment tensor inversion of local and regional waveforms to small
and moderate (Mw= 3.5–5.7) shallow earthquakes from the Iberian Peninsula, northern …
and moderate (Mw= 3.5–5.7) shallow earthquakes from the Iberian Peninsula, northern …