Pena dos Reis, R.Corrochano, A.Armenteros, Ildefonso2015-05-112015-05-111997http://hdl.handle.net/10272/10542In 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 featuresspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/PaleokarstStable isotopesSedimentationCretaceousLusitanian BasinEl paleokarst de Nazaré (Cretácico Superior de la Cuenca Lusitana, Portugal)The Nazaré paleokarst (Upper Cretaceous of the Lusitanian Basin, Portugal)journal articleopen access