RT Journal Article
T1 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
A1 Fernández Lozano, Javier
A1 Sokoutis, Dimitrios
A1 Willingshofer, Ernst
A1 Muñoz Martín, Alfonso
A1 De Vicente Muñoz, Gerardo
A1 Cloetingh, Sierd
AB Analogue modelling contributes to the interpretation of lithosphere scale folds in Iberia as a result of largescaleconvergence during Oligocene-Miocene times between the Iberian and European Plates. Different tectonothermalevents affected the microplate since late Paleozoic and resulted in lateral strength variations of the Iberianlithosphere. An old and cold lithosphere, Variscan in age, can be found in the westernmost part of Iberia whereasa 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 andtopography 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.
PB Sociedad Geológica de España
SN 0213-683X
YR 2010
FD 2010
LK https://hdl.handle.net/20.500.14352/41967
UL https://hdl.handle.net/20.500.14352/41967
LA spa
DS Docta Complutense
RD 11 jul 2024