Thesis Collection
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Browsing by Author "Ruiz, G."
Now showing items 1-5 of 5
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Análisis secuencial de la Formación Arenas de Utrillas en el N. de la provincia de Cuenca (Cordillera Ibérica)
(Sociedad Geológica de España, 1993)Six depositional sequences have been recognized in the Cretaceous terrigenous facies of the Iberian Ranges in the studied area. The Ist and 2nd sequences show caracteristics of continental environments, the 3rd and 4th ... -
Cortejos sedimentarios en parasecuencias de 4e y 5S orden en el Cenomaniense de la rama aragonesa de la Cordillera Ibérica (España)
(Sociedad Geológica de España, 1996)Parasequences Jn the Upper Albian-Cenomanian of the Iberian Ranges are deepening and then shallowing upwards parasequences, in opposition to standard parasequences which shallow upwards. They were originated by cycles of ... -
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 ... -
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) ...
