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Browsing by Author "Rodríguez Fernández, L. R."
Now showing items 1-9 of 9
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The Argentine Frontal Cordillera between 30° OO'and 31° 30'S latitude: polycyclic structure and tectonic evolution
(Sociedad Geológica de España, 2002)En el sector de la Cordillera Frontal Argentina comprendido entre los 30° y 31° 30' de latitud S, se diferencian dos conjuntos de rocas con naturaleza y estructuración diferentes: un substrato paleozoico y una cobertera ... -
Carbonífero superior en la Cordillera Frontal (Provincia de San Juan, Argentina): características e implicaciones regionales
(Sociedad Geológica de España, 2002)Previous dating of the limestones at the upper part of the Agua Negra in the Quebrada de las Ánimas provided an unconclussive age of Silurian-Devonian. A palynological analysis has been carried out with the aim of improving ... -
Deformaciones tectónicas desde el Tortoniense en el Campo de Dalias (Cordilleras Béticas)
(Sociedad Geológica de España, 2002)The Campo de Dalias is an emerged zone located at the northern boundary of Alboran Sea. The Neogene-Quaternary sediments of the Campo de Daifas are deformed by E-W open folds that also uplift Sierra de Cádor. The field ... -
Estructura de la Cuenca de Níjar a partir de datos gravimétricos (Cordillera Bética oriental)
(Sociedad Geológica de España, 2004)The Nijar Basin, filled by Miocene to Quaternary sediments, is located between Sierra Alhamilla and Sierra de Cata. This basin is affected by the NE-SW trending sinistral Carboneras Fault, and also by a set of NW-SE oriented ... -
Estructura del Campo de Dalías a partir de datos gravimétricos y sísmicos
(Sociedad Geológica de España, 2004)The analysis of new gravity data and multichannel seismic profiles of the Campo de Dalías give new insight about the main features of the deep structure. The progressive development since the Tortonian of folds determine ... -
Estructura extensional e inversion tectónica en los Andes argentinos entre los 30° 30' y 31° 00' S
(Sociedad Geológica de España, 1996)In the Andean Frontal Cordillera two tectonostratigraphlc main groups can be defined: a gondwanic basament constituted by devonian and Permo-Carboniferous marine sedimentary rocks, intruded by Upper Paleozoic granitic ... -
Evolución estructural de la zona de cizalla extensional de Berzosa-Riaza, sector de Somosierra, Sistema Central Español
(Sociedad Geológica de España, 1996)In this paper, a new structural analysis of the Somosierra sector of the Spanish Central System is presented. Two main tectonothermal events are recorded: D1 is compressional and related to the variscan collision that ... -
Nuevos datos sobre estratigrafía del Ordovícico y estructura varisca en el Macizo de Santa María la Real de Nieva
(Sociedad Geológica de España, 2004)We present a new geological map of the lower Ordovician materials cropping out in the Santa Maria la Real de Nieva Massif. The Ordovician sequence, Fm. Capas de Domingo García, comprises two separate stratigraphic units. ... -
Superposición de estructuras en el Anticlinal de Santa María de las Hoyas. Borde meridional de la Cadena Ibérica (provincias de Burgos y Soria)
(Sociedad Geológica de España, 2002)The Santa María de las Hoyas anticline is located in the southern front of the Iberian Chain in the limit of Burgos and Soria provinces. The the geological map and the cross-sections show a carbonated formations of the ...
