Características paleoambientales de las «facies de tránsito» (Plioceno inferior) en el sector N.O de la Cuenca del Guadalquivir (Albaida del Aljarafe, Sevilla, España)

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dc.contributor.authorMuñiz Guinea, Fernando
dc.contributor.authorMayoral Alfaro, Eduardo
dc.date.accessioned2015-11-18T11:08:59Z
dc.date.available2015-11-18T11:08:59Z
dc.date.issued1996
dc.description.abstractThe paleontological evidences (bivalves and crustacean decapods, mainly) of the «transitional facies» in Albaida del Aljarafe (SW. sector of the Guadalquivir Basin), indicate a relatively deep infralitoral plattform highly influenced by coastal terrigenous supply The paleoichnocoenosis data corroborate also, this assumptionen_US
dc.identifier.urihttp://hdl.handle.net/10272/11360
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherBivalvesen_US
dc.subject.otherCrustacean decapodsen_US
dc.subject.otherPaleoichnocoenosisen_US
dc.subject.otherLower Plioceneen_US
dc.subject.otherGuadalquivir Basinen_US
dc.titleCaracterísticas paleoambientales de las «facies de tránsito» (Plioceno inferior) en el sector N.O de la Cuenca del Guadalquivir (Albaida del Aljarafe, Sevilla, España)en_US
dc.titlePaleoenvironmental characteristics of the «transitional facies» (Lower Pliocene) in the Northwestern sector of the Guadalquivir Basin (Albaida del Aljarafe, Seville, Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication
relation.isAuthorOfPublication09329d77-a33d-4b35-a174-002572a31b33
relation.isAuthorOfPublication.latestForDiscovery09329d77-a33d-4b35-a174-002572a31b33

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Geogaceta -- Nº 20-1, (1996)