Edad de los términos basales del Cretácico Superior de la Depresión Intermedia (Pirineos occidentales, Nafarroa)

dc.contributor.authorIriarte, Eneko
dc.contributor.authorCaron, M.
dc.date.accessioned2014-10-30T11:28:03Z
dc.date.available2014-10-30T11:28:03Z
dc.date.issued2003
dc.description.abstractThe age of Upper Cretaceous basal sediments of the Central Depression (Western Pyrenees) has been considered to range from Cenomanian to Santonian according to previous authors. Newly studied samples show 3 planktonic foraminifera associations corresponding to M. schneegansi Zone, D. concavata Zone and D. asymetrica Zone. Thus, the base of the Upper Cretaceous is diachronous. This diachronism is attributed to the onlap of both previously formed palaeoreliefs (Upper Albian to Upper Turonian) and synsedimentary horst and graben created during the Upper Turonian-Coniacian lapse of timeen_US
dc.identifier.urihttp://hdl.handle.net/10272/9038
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.otherPlanktonic foraminiferaen_US
dc.subject.otherUpper Cretaceousen_US
dc.subject.otherTuronianen_US
dc.subject.otherCentral Depressionen_US
dc.subject.otherNavarreen_US
dc.titleEdad de los términos basales del Cretácico Superior de la Depresión Intermedia (Pirineos occidentales, Nafarroa)en_US
dc.titleAge of Upper Cretaceous basal sediments of the Central Depression (Western Pyrenees, Navarre)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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