El Neógeno superior marino en Vejer de la Frontera (Cádiz, SO España) y su evolución regresiva

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dc.contributor.authorRico García, Alberto
dc.date.accessioned2014-07-03T09:10:01Z
dc.date.available2014-07-03T09:10:01Z
dc.date.issued2007
dc.description.abstractThe upper Neogene deposits which outcrop in the area of Vejer de la Frontera (Cádiz, SW Spain) have been studied. The sedimentological, paleontological, and taphonomic changes, suggest a progressive phenomenon of upward regression, in a carbonate-detrital ramp context. Deposition begins with outer shelf sandy marls which change to calcarenites interpreted as inner shelf submareal bars and belong to the Foramol assemblage. Finally, conglomerates with marine fauna are deposited and this points to litoral environment systemsen_US
dc.identifier.urihttp://hdl.handle.net/10272/8404
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherTortonianen_US
dc.subject.otherMessinianen_US
dc.subject.otherUpper Neogeneen_US
dc.subject.otherVejer de la Fronteraen_US
dc.subject.otherCádizen_US
dc.subject.otherRegressionen_US
dc.titleEl Neógeno superior marino en Vejer de la Frontera (Cádiz, SO España) y su evolución regresivaen_US
dc.titleUpper Neogene marine deposits in Vejer de la Frontera site (Cádiz, SW Spain) and their regressive evolutioneng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 42, (2007)