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Browsing by Author "Soria, Ana Rosa"
Now showing items 1-18 of 18
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Actividad de fallas durante el depósito de la Formación Camarillas (Barremiense) en la subcuenca de Galve (E de España)
(Universidad de Huelva, 2013)En la subcuenca de Galve, fallas normales ENE-OSO (fallas de Remenderuelas, Camarillas y El Batán) fueron activas en el Barremiense, durante la sedimentación de la Formación Camarillas. Estas fallas, analizadas en un corte ... -
Bioestratigrafía de la Fm. Escucha a partir del estudio de foraminíferos planctónicos y nanofósiles en el sector de Alcaine, Teruel
(2008)This paper presents the first biostratigraphic data obtained from nannofossils in combination with planktonic foraminifera from the lower part of the Escucha Formation. Samples have been obtained from offshore marly ... -
Caracterización de la Formación Villar del Arzobispo al sur de Zaragoza (Titónico, Cordillera Ibérica)
(2006)The Villar del Arzobispo Formation (middle Tithonian–lowermost Berriasian) has been recognized for the first time in the two classical outcrops of Villanueva de Huerva and Aguilón (Zaragoza, nor thern Iberian Chain). It ... -
Desarrollo de estructuras agradacionales generadas por oleaje en lagos someros carbonatados. Un ejemplo del Oligoceno superior de la Cuenca del Ebro
(Sociedad Geológica de España, 1997)During the upper Oligocene a carbonated shallow lacustrine system developed in the central sector of the Ebro Basin. The lacustrine system was closely related to alluvial systems spreading from the margins to the centre ... -
El anticlinal de Muel-Jaulín (Zaragoza) y su relación con la extensión cretácica
(Sociedad Geológica de España, 1997)The Muel-Jaulin region shows structures related to the Lower Cretaceous extension and the Tertiary compression respectively. Cretaceous normal faults constitute the northern border of the Aguilôn Cretaceous basin, appearing ... -
El Parque Geológico de Aliaga
(Sociedad Geológica de España, 1996)The purpose of the Geological Park of Aliaga is to teach and divulge Geology, by guiding visitors along 11 points and routes of special interest which are signalyzed and show abundant information placards. It is placed ... -
El sistema fluvio-lacustre de Añavieja: facies y evolución sedimentaria durante el Holoceno. Cordillera Ibérica. NE de España
(2010)The study of the Holocene sediments from AÑ1, AÑ2 and DV1 cores, drilled between Añavieja and Dévanos (Soria), has allowed to define nine sedimentary facies: black and grey lutites, brown lutites with carbonate nodules, ... -
Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica
(Sociedad Geológica de España, 1997)The marginal zones of the Maestrazgo Basin (Las Parras and Galve basins) and the Algarve Basin show a similar evolution during basin formation (mainly Jurassic and Early Cretaceous) and inversion (Oligocene-Early Miocene). ... -
Estudio preliminar sobre la tectónica sinsedimentaria del Cretácico inferior en el borde septentrional de la Cubeta de Aliaga (Cordillera Ibérica)
(Sociedad Geológica de España, 1996)The Aliaga sub-basin was developed during the Early Cretaceous in an extensional context. Structures near the northern border of this sub-basin (normal faults, syntectonic unconformities and facies and thickness changes ... -
Expansión de un sistema lacustre en el tránsito Jurásico Cretácico (Cubeta de Aliaga, Prov. Teruel)
(Sociedad Geológica de España, 1995)In the Aliaga subbasin (Central Iberian Range) crops out a mainly calcareous serie corresponding to the Tithonic-Berriasian Villar Arzobispo Formation. There are important litological differences between this serie and ... -
Icnitas de vertebrados en las facies Buntsandstein (Triásico inferior) del Macizo de Montalbán (Peñarroyas, prov. de Teruel)
(Sociedad Geológica de España, 1995)The discovery of a new outcrop in lower Triassic fluvial sediments with diapsida footprints has been made in the locality of Peñarroyas (Teruel, Spain). There are 19 footprints which 18 has been interpreted as belonging ... -
Los depósitos terrigenos de la base de la secuencia de depósito Aptiense superior. Subcuenca de las Las Parras (provincia de Teruel)
(Sociedad Geológica de España, 1999)The bottom ofVillarroya de los Pinares formation, that is, the bottom of Upper Aptian D.S., is made up of terrigenous sediments. These materials show a retrogradational vertical evolution. This evolution started with fluvial ... -
Los sedimentos del límite Cretácico/Terciario en El Tecolote (México): evidencias de aloctonía
(Sociedad Geológica de España, 2001)Sediments from the Cretaceous-Tertiary interval were studied at the El Tecolote area (northeastern México). The composite section consists of Maastrichtian marls belonging to the Méndez Formation, and a clastic unit with ... -
Sedimentologia y paleogeografía de la secuencia de deposito Aptiense inferior (Facies Urgón) en la subcuenca de Las Parras. (Teruel)
(Sociedad Geológica de España, 1999)The Lower Aptian D.S. is made up of materials which settled in shallow carbonate ramp enviroments. This sequence shows a retrogradational evolution, that is, from internal to mid ramp enviroments. The vertical evolution ... -
Sedimentology and sedimentary evolution of the Artoles Fm in Miravete de la Sierra (Teruel, Iberian Chain)
(Sociedad Geológica de España, 2015)Este trabajo analiza la sedimentología y evolución sedimentaria de la Fm.Artoles (Barremiense) en el perfil estratigráfico Camino de Miravete (subcuenca de Galve, España). El análisis sedimentológico ha permitido diferenciar ... -
Subambientes sedimentarios del sector noroeste de la laguna de Gallocanta. Provincia de Zaragoza
(Sociedad Geológica de España, 1999)The study carried out in nortwestern sector of the carbonate-saline lake of Gallocanta point out that lutite, sapropel and salt deposition dominate in this lake, although in some zones sandstone and gravel deposition is ... -
Tectónica extensional cretácica en la subcuenca de Oliete (Cordillera Ibérica central)
(Sociedad Geológica de España, 1997)The control of the extensional tectonics on the geometry of the Oliete Subbasin during Early Barremian-Basal Aptian (Early Cretaceous) is examinated. Both, the main NW-SE trending of the basin, its asymetrical geometry and ... -
Un sistema de fallas normales sinsedimentarias en las unidades de facies Urgon de Aliaga (Teruel, Cordillera Ibérica)
(Sociedad Geológica de España, 1997)System of conjugate, E-W to NE-SW striking normal faults is reconstructed from mapping and structural analysis of deformation in the Urgon deposits of the Aliaga region. Those were mainly active during the Aptian age, ...
