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Browsing by Author "Ruano, Patricia"
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Active faults in the Granada Depression and Zafarraya areas (Betic Cordilleras)
Reicherter, K. R.; Jabaloy, A.; Galindo Zaldívar, Jesús; Ruano, Patricia (Sociedad Geológica de España, 1999)Pliocene to Holocene alluvial and colluvial deposits in the Granada Depression and surrounding areas display a wide range of features of recent faulting related to coseismic ruptures. The majority of the faults studied are ... -
Anomalías gravimétricas y magnéticas en la Depresión de Granada (Cordilleras Béticas): tratamiento e interpretación
Jiménez Pintor, J.; Galindo Zaldívar, Jesús; Ruano, Patricia; Morales, J. (Sociedad Geológica de España, 2001)The Granada Depression, located in the central sector of the Betic Cordilleras, is an intramountain depression filled mainly by detritic, evaporite and carbonate rocks since Miocene. Gravity anomaly minima are associated ... -
Caracterización de la geometría del Polje de Zafarraya a partir de prospección gravimétrica (Cordillera Bética)
Fernández García, Carlos; Ruano, Patricia (Sociedad Geológica de España, 2016)The Zafarraya Polje is a Neogene endorheic basin, which lies on the contact between internal and external Zones of the Betic Cordillera. This basin limits on its southern boundary with the Ventas de Zafarraya fault, related ... -
Deformaciones plio-cuaternarias en la region de Rabat
Akil, Mustafa; Galindo Zaldívar, Jesús; Tahayt, A.; Jabaloy, A.; Chabli, A.; Ruano, Patricia; Chalouan, Ahmed (Sociedad Geológica de España, 2000)The Rabat region, located in the northern border of the Moroccan Meseta, is generally considered as a present-day stable region. However, the fluvial and marine sedimentary rocks, with Pliocene and Quaternary ages, are ... -
Deformaciones recientes en el frente de la Cordillera Rifeña (Prerif, Marruecos)
Chalouan, Ahmed; Galindo Zaldívar, Jesús; Bargach, K.; Jabaloy, A.; Ahmamou, M’Fedal; Ruano, Patricia; Benmakhlouf, M.; Sanz de Galdeano, Carlos; Akil, Mustafa (Sociedad Geológica de España, 2000)The Prerif ridges form pari of the foreland of the Rif Mountains. They are formed by superposed slices, with folds and faults, originated during the late Miocene WSWwards displacement of the Prerif units. At present, they ... -
Estructura de la cuenca sedimentaria de Tabernas-Sorbas mediante prospección gravimétrica y magnética (Zonas Internas, Cordillera Bética Oriental)
Li, Qiao; Ruano, Patricia; Pedrera Parias, Antonio; Galindo Zaldívar, Jesús (Universidad de Huelva, 2012)Se han determinado las anomalías gravimétricas y magnéticas en tres perfiles perpendiculares a la cuenca Tabernas-Sorbas (Zonas Internas, Cordillera Bética oriental). Los modelos gravimétricos muestran una morfología asimétrica ... -
Geometría y estructuras de la cuenca neógena de Loja a partir de datos gravimétricos (Andes Ecuatorianos)
Galindo Zaldívar, Jesús; Soto, John; Ruano, Patricia; Tamay, José; Lamas, Francisco; Guartán, José; Azañón, José Miguel; Paladines, Agustín (2010)The recent tectonic evolution of the central Andes is driven by the subduction of the oceanic Nazca plate below the South America continental crust. This process has produced relief uplift and the isolation and deformation ... -
Hidrogeoquímica y microbiología en Los Hervideros del Campo de Calatrava (Ciudad Real)
Yélamos, J. G.; Redondo, R.; Castro, F. de; Galván, A.; Martínez Rubio, J.; Ruano, Patricia; Senderos, A. J.; ViIIarroya, F. I.; Rebollo Ferreiro, Luis F. (Sociedad Geológica de España, 1999)CÓZ-rich springs and wells in the Campo de Calatrava commonly are named Hervideros. This .ground water is originated by deep circulation along the fractures of the paleozoic rocks of the area, with residence times ... -
Primeras evidencias de paleoterremotos en la falla de Carboneras: estudio paleosismológico en el segmento de La Serrata
Moreno, Ximena; Masana, E.; Gràcia, E.; Pallàs, R.; Ruano, Patricia; Coll, Miquel; Stepancíková, P.; Santanach, P. (2006)A paleoseismological analysis was performed along the La Serrata segment of the Carboneras fault (Eastern Betics) in order to establish its seismic potential. The site was selected after a general geomorphological analysis ... -
Relaciones entre tectónica y sedimentación asociadas a las Rides Prérifaines en la Cuenca de Volubilis (frente del Rif, Marruecos)
Roldán García, Francisco Javier; Galindo Zaldívar, Jesús; Chalouan, Ahmed; Anahnah, Farida; Ahmamou, M’Fedal; Ruano, Patricia; Ruiz Constán, Ana; Sanz de Galdeano, Carlos; Ben Makhlouf, Mohamed; Marín Lechado, Carlos; López Garrido, Ángel Carlos; Pedrera Parias, Antonio (2009)The Volubilis Neogene basin (Morocco) was part of the South Rif Corridor that connected the Atlantic Ocean with the Mediterranean. This basin recorded the tectonic - sedimentary interactions of a foreland basin subjected ... -
The seismic crustal structure of the Ossa-Morena zone and its geological interpretation
Simancas Cabrera, J. F.; Carbonell, R.; González Lodeiro, Francisco; Pérez Estaún, A.; Juhlin, C.; Ayarza, P.; Azor, A.; Martínez Poyatos, D.; Ruiz de Almodóvar Sel, Gabriel; Pascual Martínez, Emilio
; Sáez Ramos, Reinaldo
; Kashubin, A.; Alonso Chaves, Francisco Manuel
; Álvarez Marrón, J.; Bohoyo, Fernando; Castillo, S.; Donaire Romero, Teodosio
; Expósito, Inmaculada; Flecha, I.; Galadí, E.; Galindo Zaldívar, Jesús; González Barrionuevo, Felipe
; González Cuadra, P.; Macías, I.; Martí, D.; Martín, A.; Martín Parra, L. M.; Nieto Liñán, José Miguel
; Palm, H.; Ruano, Patricia; Ruiz, M.; Toscano Grande, Antonio
(Universidad Complutense de Madrid, 2004)
The IBERSEIS deep reflection seismic experiment has provided a crustal image of the Variscan orogen of southwest Iberia. A brief presentation of the entire seismic profile is given, and then the Ossa-Morena Zone (OMZ) and ...