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

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dc.contributor.authorFernández Lozano, Javier
dc.contributor.authorSokoutis, Dimitrios
dc.contributor.authorWillingshofer, Ernst
dc.contributor.authorMuñoz Martín, Alfonso
dc.contributor.authorDe Vicente Muñoz, Gerardo
dc.contributor.authorCloetingh, Sierd
dc.date.accessioned2023-06-20T00:06:09Z
dc.date.available2023-06-20T00:06:09Z
dc.date.issued2010
dc.description.abstractAnalogue 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.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/13267
dc.identifier.issn0213-683X
dc.identifier.officialurlhttp://uhu.es/publicaciones/revistas/geogaceta/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/41967
dc.journal.titleGeogaceta
dc.language.isospa
dc.page.final70
dc.page.initial67
dc.publisherSociedad Geológica de España
dc.rights.accessRightsopen access
dc.subject.cdu551.4
dc.subject.keywordLithosphere folds
dc.subject.keywordIberia
dc.subject.keywordCenozoic
dc.subject.keywordLithosphere strength
dc.subject.ucmGeofísica
dc.subject.ucmGeodinámica
dc.subject.unesco2507 Geofísica
dc.subject.unesco2507 Geofísica
dc.titleSobre el origen de la asimetría en el patrón general del relieve en el interior de la Península Ibérica: nuevos resultados obtenidos mediante modelación análoga
dc.typejournal article
dc.volume.number49
dspace.entity.typePublication
relation.isAuthorOfPublication70f369a3-b3cd-43cb-874e-a7888da25de1
relation.isAuthorOfPublication.latestForDiscovery70f369a3-b3cd-43cb-874e-a7888da25de1
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