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 …
Lithospheric folding and sedimentary basin evolution: a review and analysis of formation mechanisms
S Cloetingh, E Burov - Basin Research, 2011 - earthdoc.org
Lithospheric folding is an important mode of basin formation in compressional intraplate
settings. Basins formed by lithospheric folding are characterized by distinct features in …
settings. Basins formed by lithospheric folding are characterized by distinct features in …
3D GNSS velocity field sheds light on the deformation mechanisms in Europe: Effects of the vertical crustal motion on the distribution of seismicity
Crustal deformation and seismicity in Europe are still poorly understood. Seismic activity is
classically ascribed to crustal strain rates generated by edge‐driven tectonic forces …
classically ascribed to crustal strain rates generated by edge‐driven tectonic forces …
[图书][B] The Paleogene and Neogene of western Iberia (Portugal): a Cenozoic record in the European Atlantic domain
The Portuguese mainland, located in western Iberia, represents a key area for
understanding the evolution of the European Atlantic margin during the Cenozoic and the …
understanding the evolution of the European Atlantic margin during the Cenozoic and the …
Tectonic classification of Cenozoic Iberian foreland basins
The Iberian microcontinent stands out because of its intense Alpine intraplate deformation.
This is reflected in a large number of Cenozoic basins of very different sizes. Most of the …
This is reflected in a large number of Cenozoic basins of very different sizes. Most of the …
The influence of surface and tectonic processes on landscape evolution of the Iberian Chain (Spain): Quantitative geomorphological analysis and geochronology
In tectonically active areas, the landscape response to tectonic forcing is described and
possibly quantified by regional topographic and hydrographic features as well as by spatial …
possibly quantified by regional topographic and hydrographic features as well as by spatial …
Using river long profiles and geomorphic indices to evaluate the geomorphological signature of continental scale drainage capture, Duero basin (NW Iberia)
Well-constrained case studies of transient landscape responses are needed to improve our
understanding of erosion processes associated with drainage captures. The Duero basin is …
understanding of erosion processes associated with drainage captures. The Duero basin is …
The Spanish‐Portuguese Central System: An example of intense intraplate deformation and strain partitioning
The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and
deformation belts with a wide variety of structural trends. The Spanish‐Portuguese Central …
deformation belts with a wide variety of structural trends. The Spanish‐Portuguese Central …
Displacement transfer from borders to interior of a plate: A crustal transect of Iberia
A NS crustal transect of the whole Iberian Plate is presented. The displacement transfer
during the Alpine deformation from the border ranges (Cantabrian and Betic chains) toward …
during the Alpine deformation from the border ranges (Cantabrian and Betic chains) toward …
Reconstructing the interacting effects of base level, climate, and tectonic uplift in the lower Miño River terrace record: a gradient modelling evaluation
The origin of the lower Miño River terraces in the NW Iberian Peninsula has been a topic of
debate since the 1940s. Various hypotheses about their main controlling factors have been …
debate since the 1940s. Various hypotheses about their main controlling factors have been …