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dc.contributor.authorPagés Valcarlos, J. L.
dc.contributor.authorVidal Romaní, Juan Ramón
dc.date.accessioned2010-01-22T13:26:31Z
dc.date.available2010-01-22T13:26:31Z
dc.date.issued1997
dc.identifier.citationCadernos do Laboratorio Xeolóxico de Laxe, 1997, 22: 121-132 ISSN: 0213-4497es_ES
dc.identifier.issn0213-4497
dc.identifier.urihttp://hdl.handle.net/2183/6284
dc.description.abstract[Abstract] The present paper srudy the evolution of the lower part of the Tambre Basin duting the Neogene. The basin, the fluvial network and a group of features are analyzed, such as the asymmetry of the net, the entrenchement, steps, etc, that are present in the Tambre and also frequent in other fluvial systems of Galicia. Ir is settled down that the current configuration of the fluvial network has been reached after a complex system of captures, with inversion of the drainage directions. Such evolution is not presented like an anecdotic circunstance in the layout ofthe river but rather it is considered a remarkable example ofthe fluvial processes that have contributed to the modeling ofthe present relief of Western Galicia.
dc.language.isospaes_ES
dc.publisherUniversidade da Coruñaes_ES
dc.subjectAsymmetrical fluvial nerworkes_ES
dc.subjectEntrenchmentes_ES
dc.subjectCaptureses_ES
dc.subjectTambrees_ES
dc.subjectWestern Galiciaes_ES
dc.titleEvolución neógena de la cuenca baja del Tambrees_ES
dc.title.alternativeNeogene evolution of the lower reach of the Tambre river
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccess


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