Thesis Collection
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Browsing by Author "Carenas, B."
Now showing items 1-5 of 5
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El Albense - Cenomanense medio de la Sierra de Altomira
(Sociedad Geológica de España, 1993)The Cretaceous transgression in the Sierra de Altomira starts with sandy (Utrillas Fm.) and dolomitic sediments (Villa de Ves Mb.), its detailed sequential analysis allow the recognition of five depositional sequences with ... -
Discontinuidades estratigráficas y secuencias deposicionales del Cretácico medio (Albiense superior-Turoniense medio) en la Cordillera Ibérica central y el Sistema Central meridional
(Sociedad Geológica de España, 1996)The Middle Cretaceous in the Iberian Ranges is a 2nd order cycle with an Upper Albian - Middle Turonian age. The cycle is bounded by two major unconformities and comprise 8 depositional sequences (3rd orderI The four basal ... -
Evolución paleogeógráfica de la Cuenca Ibérica en el Cretácico Superior
(Sociedad Geológica de España, 2004)In 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 ... -
Relaciones genéticas entre las unidades litoestratigráficas del Cretácico medio y superior de la Cordillera Ibérica Occidental
(Sociedad Geológica de España, 1996)During last 20 years the Midc/le and Upper Cretaeous in the Iberian Ranges have been widley studied. Stratigraphic correlations between regional series, however, have been problematic since there exist common faces changes, ... -
Secuencias deposicionales del Cretácico superior no terminal (Turoniense superior - Campaniense inferior) en la zona central de la Península Ibérica (Cordillera Ibérica y Sistema Central)
(Sociedad Geológica de España, 1996)The Upper Cretaceous (Upper Turonian - Lower Campanian) in the central Iberian Peninsula is divided into 4 depositional sequences with an eustatic origin, which are correlated to the UZA 3-1 to UZA 3.4 of Haq et al. (1988) ...
