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 …

Holocene earthquake record offshore Portugal (SW Iberia): testing turbidite paleoseismology in a slow-convergence margin

E Gracia, A Vizcaino, C Escutia, A Asioli… - Quaternary Science …, 2010 - Elsevier
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 …

Kinematics of the Iberia–Maghreb plate contact from seismic moment tensors and GPS observations

D Stich, E Serpelloni, F de Lis Mancilla, J Morales - Tectonophysics, 2006 - Elsevier
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 …

New GPS constraints on active deformation along the Africa–Iberia plate boundary

A Koulali, D Ouazar, A Tahayt, RW King… - Earth and Planetary …, 2011 - Elsevier
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 …

Testing the sensitivity of geomorphic indices in areas of low-rate active folding (eastern Betic Cordillera, Spain)

A Pedrera, JV Pérez-Peña, J Galindo-Zaldívar… - Geomorphology, 2009 - Elsevier
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 …

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 …

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

D Lange, J Cembrano, A Rietbrock, C Haberland… - Tectonophysics, 2008 - Elsevier
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 …

Inversion of moment tensor focal mechanisms for active stresses around the microcontinent Iberia: Tectonic implications

G De Vicente, S Cloetingh, A Muñoz‐Martín, A Olaiz… - …, 2008 - Wiley Online Library
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 …

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 …

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 …