Descenso eustático messiniense en una cuenca atlántica. El cañón submarino del Río Guadalquivir. (SO de España)

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dc.contributor.authorMartínez del Olmo, W.
dc.contributor.authorRiaza Molina, C.
dc.contributor.authorTorrescusa Villaverde, S.
dc.date.accessioned2020-05-28T12:25:58Z
dc.date.available2020-05-28T12:25:58Z
dc.date.issued1996
dc.description.abstractNumerous seismic lines allow {he identification of a deep and long erosive canyon incised during the Messinian on shelfal and basinal deposits of Upper Tortonian and Messinian s.s. age. Reconstructions of the pre-erosional sedimentary architecture and other regional data support the interpretation of the erosion being of submarine origin and probably related with a Guadalquivir paleo-riveres_ES
dc.identifier.urihttp://hdl.handle.net/10272/18111
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMessinian unconformityes_ES
dc.subject.otherEustatic changeses_ES
dc.subject.otherSystem Tractses_ES
dc.subject.otherIncised valley filles_ES
dc.titleDescenso eustático messiniense en una cuenca atlántica. El cañón submarino del Río Guadalquivir. (SO de España)es_ES
dc.titleThe messinian submarine canyon of the Guadalquivir river (Atlantic coast southwestern Spain)eng
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 20-1, (1996)