Evolución paleogeógráfica de la Cuenca Ibérica en el Cretácico Superior

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dc.contributor.authorSegura, M.
dc.contributor.authorGarcía Hidalgo, J. F.
dc.contributor.authorCarenas, B.
dc.contributor.authorGil, J.
dc.contributor.authorGarcía, A.
dc.date.accessioned2014-10-22T10:55:15Z
dc.date.available2014-10-22T10:55:15Z
dc.date.issued2004
dc.description.abstractIn the Iberian Basin, during Upper Albian - Middle Campanian, several shallow carbonate platforms were developed. These platforms grade landwards, westwards to the Hesperian Massif, to silicidastic, littoral and coastal sediments. Two major depositional megasequences (2nd order) and 12 depositional sequences (3rd order) have been recognized. Detailed paleogeographical maps for the eleven basal depositional sequences are presented in this paper. Temporal ranging of these maps is about 2 My, from Upper Albian (102 My) to Lower Campanian (83 My)en_US
dc.identifier.urihttp://hdl.handle.net/10272/8937
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.otherPalaeogeographyen_US
dc.subject.otherIberian Basinen_US
dc.subject.otherUpper Cretaceousen_US
dc.titleEvolución paleogeógráfica de la Cuenca Ibérica en el Cretácico Superioren_US
dc.titlePalaeogeographic evolution of the Iberian Basin along the Upper Cretaceouseng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 36, (2004)