Fernández Lozano, Javier and Sokoutis, Dimitrios and Willingshofer, Ernst and Muñoz Martín, Alfonso and De Vicente Muñoz, Gerardo and Cloetingh, Sierd (2010) Sobre el origen de la asimetría en el patrón general del relieve en el interior de la Península Ibérica: nuevos resultados obtenidos mediante modelación análoga. Geogaceta, 49 . pp. 67-70. ISSN 0213-683X
Official URL: http://uhu.es/publicaciones/revistas/geogaceta/
Analogue modelling contributes to the interpretation of lithosphere scale folds in Iberia as a result of largescale convergence during Oligocene-Miocene times between the Iberian and European Plates. Different tectonothermal events affected the microplate since late Paleozoic and resulted in lateral strength variations of the Iberian lithosphere. An old and cold lithosphere, Variscan in age, can be found in the westernmost part of Iberia whereas a relative weak and hot Mesozoic lithosphere affected by episodes of rifting and basin inversion during Mesozoic- Tertiary times covers the area of the Iberian Chain. Our study aims at deciphering whether deformation and topography evolution in Iberia are related to lateral strength variations and/or the inherited structural grain stemming from Variscan deformation. We also have studied the strength of the lithosphere to gain insights into the effects of rheological variations related to local thrusting or primary strength variations along the Iberian lithosphere.
|Uncontrolled Keywords:||Lithosphere folds, Iberia, Cenozoic, Lithosphere strength|
|Subjects:||Sciences > Physics > Geophysics|
Sciences > Geology > Geodynamics
|Deposited On:||14 Sep 2011 13:13|
|Last Modified:||14 Sep 2011 13:13|