2026-06-08T01:02:16Zhttps://docta.ucm.es/rest/oai/requestoai:docta.ucm.es:20.500.14352/886312025-08-28T17:34:59Zcom_20.500.14352_14col_20.500.14352_15
Docta Complutense
author
Vicente Muñoz, Gerardo De
author
Cloetingh, S.
author
Van Wees, J.D.
author
Cunha, P.P.
2023-11-07T18:46:45Z
2023-11-07T18:46:45Z
2011
De Vicente, G., et al. «Tectonic Classification of Cenozoic Iberian Foreland Basins». Tectonophysics, vol. 502, n.o 1-2, abril de 2011, pp. 38-61. DOI.org (Crossref), https://doi.org/10.1016/j.tecto.2011.02.007.
10.1016/j.tecto.2011.02.007
https://hdl.handle.net/20.500.14352/88631
https://doi.org/10.1016/j.tecto.2011.02.007
http://www.journals.elsevier.com/tectonophysics/
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 contacts between topographic highs and basins are thrust or strike-slip faults. All these basins seem to have undergone a common sedimentary evolution, comprising four stages: initiation of sedimentation, intense syn-tectonic infilling, change from endorheic to exorheic drainage, and accelerated erosion related to fluvial incision. This simple evolutionary model shows a migration from East to West, in which basins are still tectonically active at the Atlantic margin of Iberia. This common evolution is also found in a series of geometrical characteristics, such as the ratio r of length of strike-slip fault and length of thrust fault, that are very similar in both types of basin border settings. Thrust-related basins are mainly associated with segmented pop-downs, whereas the main basins have the characteristics of open-ramp basins. Strike-slip related basins are mostly transpressive structures, although small pull-apart basins are usual along the Vilariça and Messejana faults. For basin areas larger than 100– 1000 km2, a constant r value of 0.6 is found (including the Ebro, Duero, Madrid, Lower Tagus and Badajoz basins). Within the Iberian microcontinent, the total amount of Cenozoic contractional deformation was distributed between strike-slip and thrust faults with an r ratio close to 0.6. However, for small basins this parameter seems to depend on the type of fault, range or deformation belt (pure strike-slip, transtension, transpression, and pop-up) independently of its local tectonic development.
eng
Tectonic classification of Cenozoic Iberian foreland basins
journal article
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2011DeVicente_etal.pdf.txt