Aproximación al paleorelieve Tortoniense del margen ibérico meridional (depresión occidental del Guadalquivir)

The Tortonian palaeorelief features of the sruthern edge of the Iberian Massif (W. Guadalquivir basin)

dc.contributor.author	Rodríguez Vidal, Joaquín
dc.date.accessioned	2020-05-14T10:11:26Z
dc.date.available	2020-05-14T10:11:26Z
dc.date.issued	1991
dc.identifier.uri	http://hdl.handle.net/10272/17948
dc.description.abstract	During the Middle•Upper Tortonian, the southern edge of the Iberian Massif was affected by a marine transgression. So the planated topography (pre-Tertiary erosion surface). tilted to the south (1% - 3%), was cutting by N-S fluvial pattern. The uneven relief conditioned the local sedimentation with little deltas, beaches and others related environments, as well as cliffs and marine benches	es_ES
dc.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Geomorphology	es_ES
dc.subject.other	Tortonian	es_ES
dc.subject.other	Iberian Massif	es_ES
dc.subject.other	Guadalquivir basin	es_ES
dc.title	Aproximación al paleorelieve Tortoniense del margen ibérico meridional (depresión occidental del Guadalquivir)	es_ES
dc.title	The Tortonian palaeorelief features of the sruthern edge of the Iberian Massif (W. Guadalquivir basin)	eng
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

The Tortonian palaeorelief features of the sruthern edge of the Iberian Massif (W. Guadalquivir basin)

dc.contributor.author	Rodríguez Vidal, Joaquín
dc.date.accessioned	2020-05-14T10:11:26Z
dc.date.available	2020-05-14T10:11:26Z
dc.date.issued	1991
dc.identifier.uri	http://hdl.handle.net/10272/17948
dc.description.abstract	During the Middle•Upper Tortonian, the southern edge of the Iberian Massif was affected by a marine transgression. So the planated topography (pre-Tertiary erosion surface). tilted to the south (1% - 3%), was cutting by N-S fluvial pattern. The uneven relief conditioned the local sedimentation with little deltas, beaches and others related environments, as well as cliffs and marine benches	es_ES
dc.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Geomorphology	es_ES
dc.subject.other	Tortonian	es_ES
dc.subject.other	Iberian Massif	es_ES
dc.subject.other	Guadalquivir basin	es_ES
dc.title	Aproximación al paleorelieve Tortoniense del margen ibérico meridional (depresión occidental del Guadalquivir)	es_ES
dc.title	The Tortonian palaeorelief features of the sruthern edge of the Iberian Massif (W. Guadalquivir basin)	eng
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

Files in this item

This item appears in the following Collection(s)