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Model for the topographic evolution in NW Iberia during the lithospheric delamination at the end of the Variscan Orogeny

dc.contributor.authorMuñoz Quijano, I. N.
dc.contributor.authorGutiérrez Alonso, Gabriel
dc.date.accessioned2014-06-26T09:48:51Z
dc.date.available2014-06-26T09:48:51Z
dc.date.issued2007
dc.identifier.urihttp://hdl.handle.net/10272/8368
dc.description.abstractThrough a simple isostatic balance modelization we attempt an approach to one of the possible lithospheric and topographical scenarios that took place in the aftermath of the Variscan Orogeny. From this point of view, the results obtained, together with their comparison with the geologic, sedimentary and igneous record, during the Upper Carboniferous and the Early Permian, allow to explain most of the geological processes that took place in the studied region due to a process of lithospheric thickening under the Cantabrian Zone and the subsequent lithospheric delamination of the formerly generated root. This process caused a topographical inversion of the relief, from initially higher mountains in the western part of the Variscan Orogen (In present day coordinates) to subsequent dominant elevations in the east (Cantabrian Zone), contemporary with the lithospheric delaminationen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherTopographyen_US
dc.subject.otherLithospheric delaminationen_US
dc.subject.otherIsostasyen_US
dc.subject.otherCantabrian zoneen_US
dc.subject.otherVariscan orogenen_US
dc.titleModelo de evolución topográfica en el NO de la Península Ibérica durante la delaminación litosférica al final de la Orogenia Variscaen_US
dc.titleModel for the topographic evolution in NW Iberia during the lithospheric delamination at the end of the Variscan Orogenyeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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