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Browsing by Author "García Hidalgo, J. F."
Now showing items 1-13 of 13
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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 ... -
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 ... -
Episodios sedimentarios en el Alcudiense Superior (Proterozoico) y su tránsito al Cámbrico en la zona centro meridional del Macizo Ibérico
(Sociedad Geológica de España, 1987)The evolution of the Upper Alcudian-Lower Cambrian basin is studied in the eastern Lusitanian-Alcudian Zone. Five sedimentary episodes with distinctive characteristics are considered -
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 ... -
Evolución sedimentaria reciente de las Tablas de Daimiel (Ciudad Real)
(Sociedad Geológica de España, 1995)Two sedim entary events have been distinguished in the recent evolu tio n o f the present Tablas de Daimiel National Park. The older one is characterized by the presence of siliceous sands and silts, and mudstones; the ... -
El nivel con carbonatos del «Alcudiense superior» en el Area de Cabezarrubias-Hinojosas (Valle de Alcudia, Ciudad Real)
(Sociedad Geológica de España, 1988)The levels which contain carbonates are the essential ones both for litostratigraphic correlation and facies analysis in the Upper Proterozoic series of the Central Iberian zone. In this work, several carbonatic outcrops ... -
Las pistas fósiles de los anticlinales de Alcudia y Abenójar (Zona Centroibénca). Edad de las series
(Sociedad Geológica de España, 1993)Cambrian-type (Bergaueria and Monomorphichnus) and other trace fossils (Hormosiroidea, Palaeophycus, Phycodes? and Belorhaphe?) are described in theAlcudia and Abenojar anticlines and compared with similar traces by other ... -
Las pistas fósiles del Alcudiense superior en el anticlinal de Ibor. Consideraciones cronoestratigráficas
(Sociedad Geológica de España, 1992)New discovery of trace fossils in the Upper Alcudian of the Ibor anticline indicate that its supposed Precambrian age should be maintained but tentatively, due to the presence of scarce Lower Cambrian trace fossils although ... -
Pistas fósiles en la «Serie de Carrascalejo». Implicaciones cronoestratigráficas
(Sociedad Geológica de España, 1992)Trace fossils (Cruziana and Rusophycus) are described for the first time in the Carrascalejo beds. The stratigraphy of this unit is also modified; the conglomeratic basal beds are included in the underlying Precambrian ... -
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) ... -
Un modelo sobre el control orbital de la sedimentación en medios de plataforma: el Albiense-Cenomaniense del Puerto del Remolcador (Maestrazgo, Castellón)
(Sociedad Geológica de España, 1996)There are marry papers dealing with orbital forcing on sedimentation, mainly on deep facies. The study of orbital forcing on platform sediments, however, depends on the development of accurate models, which can be contrasted ...
