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Micropaleontology, Chronostratigraphy and Sedimentology of the Cretaceous/Tertiary boundary in NW Cuba

dc.contributor.authorMolina, Eustoquio
dc.contributor.authorArenillas, J. I.
dc.contributor.authorArz, José Antonio
dc.contributor.authorDíaz, C.
dc.contributor.authorGarcia, D.
dc.contributor.authorMeléndez Hevia, Alfonso
dc.contributor.authorRojas, R.
dc.date.accessioned2014-11-19T11:13:19Z
dc.date.available2014-11-19T11:13:19Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/10272/9359
dc.description.abstractSeveral sections have been studied in western Cuba in order to date the sediments derived of the nearby Yucatan meteorite impact event. The sections of Peñalver, Minas, La Victoria, La Yuca, Santa Isabel, Cacarajicara and Moneada contain thick sediments along the Cretaceous-Tertiary transition, showing clear evidence of a large meteorite impact. The Chronostratigraphy of the Via Blanca, Peñalver, Cacarajicara, Moneada and Apolo Formations have been revised, placing the K/T boundary at the base of the Peñalver, Cacarajicara and Moneada formations. Planktic foraminifera of the Via Blanca Formation allowed to date the uppermost autochtonous sediments as P. hantkeninoides Biozone (latest Maastrichtian)en_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherCretaceousen_US
dc.subject.otherTertiaryen_US
dc.subject.otherPlanktic Foraminiferaen_US
dc.subject.otherImpacten_US
dc.titleMicropaleontología, Cronoestratigrafía y Sedimentología del límite Cretácico/Terciario en el NO de Cubaen_US
dc.titleMicropaleontology, Chronostratigraphy and Sedimentology of the Cretaceous/Tertiary boundary in NW Cubaeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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