Tethys–Atlantic interaction along the Iberia–Africa plate boundary: The Betic–Rif orogenic system
J Vergés, M Fernàndez - Tectonophysics, 2012 - Elsevier
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 …
Late Cretaceous to middle Oligocene twisting to a later faster E-dipping subduction of the …
Holocene earthquake record offshore Portugal (SW Iberia): testing turbidite paleoseismology in a slow-convergence margin
The SW margin of the Iberian Peninsula hosts the present-day boundary between the
Eurasian and African Plates. Convergence (4–5mm/yr) is accommodated through a wide …
Eurasian and African Plates. Convergence (4–5mm/yr) is accommodated through a wide …
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 …
New GPS constraints on active deformation along the Africa–Iberia plate boundary
We use velocities from 65 continuous stations and 31 survey-mode GPS sites as well as
kinematic modeling to investigate present day deformation along the Africa–Iberia plate …
kinematic modeling to investigate present day deformation along the Africa–Iberia plate …
Crustal types and Tertiary tectonic evolution of the Alborán sea, western Mediterranean
G Booth‐Rea, CR Ranero… - Geochemistry …, 2007 - Wiley Online Library
Multichannel seismic reflection images across the transition between the east Alborán and
the Algero‐Balearic basins show how crustal thickness decreases from about 5 s two‐way …
the Algero‐Balearic basins show how crustal thickness decreases from about 5 s two‐way …
Testing the sensitivity of geomorphic indices in areas of low-rate active folding (eastern Betic Cordillera, Spain)
Active deformation structures have an incidence in topography that can be quantified by
using geomorphic indices. Most of these indices have been checked in faulted regions with …
using geomorphic indices. Most of these indices have been checked in faulted regions with …
Inversion of moment tensor focal mechanisms for active stresses around the microcontinent Iberia: Tectonic implications
The Iberian microcontinent and its connected oceanic crust are affected by deformations
related to the Eurasian‐African plate boundary. Active stress inversions from populations of …
related to the Eurasian‐African plate boundary. Active stress inversions from populations of …
First seismic record for intra-arc strike-slip tectonics along the Liquiñe-Ofqui fault zone at the obliquely convergent plate margin of the southern Andes
A temporal seismic network recorded local seismicity along a 130 km long segment of the
transpressional dextral strike-slip Liquiñe-Ofqui fault zone (LOFZ) in southern Chile. Seventy …
transpressional dextral strike-slip Liquiñe-Ofqui fault zone (LOFZ) in southern Chile. Seventy …
Active thrust faulting offshore Boumerdes, Algeria, and its relations to the 2003 Mw 6.9 earthquake
J Déverchère, K Yelles, A Domzig… - Geophysical …, 2005 - Wiley Online Library
We investigate the active seismogenic fault system in the area of the 2003 Mw 6.9
Boumerdes earthquake, Algeria, from a high‐resolution swath bathymetry and seismic …
Boumerdes earthquake, Algeria, from a high‐resolution swath bathymetry and seismic …
Slab rupture and delamination under the Betics and Rif constrained from receiver functions
F de Lis Mancilla, G Booth-Rea, D Stich… - Tectonophysics, 2015 - Elsevier
We map the lithospheric structure under the westernmost Mediterranean convergent setting
interpreting P-receiver functions obtained from a dense seismic network. No orogenic root …
interpreting P-receiver functions obtained from a dense seismic network. No orogenic root …