El paleokarst de Nazaré (Cretácico Superior de la Cuenca Lusitana, Portugal)

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dc.contributor.authorPena dos Reis, R.
dc.contributor.authorCorrochano, A.
dc.contributor.authorArmenteros, Ildefonso
dc.date.accessioned2015-05-11T08:55:23Z
dc.date.available2015-05-11T08:55:23Z
dc.date.issued1997
dc.description.abstractIn the Nazare region, (west Portuguese coast) there is an exceptionally well exposed paleokarst associated with the Upper Cenomanian carbonate succession and the overlying siliciclastics series of probable Turonian-Campanian age. The progradational trend of this succession as well as its depositional geometries show that sinsedimentary tectonic activity influenced the different diagenetic and paleokarstic featuresen_US
dc.identifier.urihttp://hdl.handle.net/10272/10542
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.otherPaleokarsten_US
dc.subject.otherStable isotopesen_US
dc.subject.otherSedimentationen_US
dc.subject.otherCretaceousen_US
dc.subject.otherLusitanian Basinen_US
dc.titleEl paleokarst de Nazaré (Cretácico Superior de la Cuenca Lusitana, Portugal)en_US
dc.titleThe Nazaré paleokarst (Upper Cretaceous of the Lusitanian Basin, Portugal)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 22, (1997)