Thesis Collection
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Browsing by Author "González Lodeiro, Francisco"
Now showing items 1-16 of 16
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Caracterización morfo-estructural del borde occidental de Sierra de Gádor (Cordillera Bética)
(2006)An integrated geomorphic and structural study has been performed along the western border of Sierra de Gádor (Betic Cordillera, SE Spain). To do this, we have calculated some of the most reliable geomorphic indexes for ... -
A comparison of the Neoproterozoic / Lower Palaeozoic lithostratigraphy of Morocco and southwestern Iberia. Geodynamic interpretations
(Sociedad Geológica de España, 2005)El Neoproterozoico del sudoeste de Iberia (Serie Negra y Formación Malcocinado) es contemporáneo de un magmatismo calcoalcalino (Precámbrico PIII del Anti-Atlas de Marruecos) que sella la Orogenia Cadomiense. El Cámbrico ... -
Las deformaciones hercinianas tardías en la región de Santa María la Real de Nieva (Sistema Central Español)
(Sociedad Geológica de España, 1988)The precambrian and paleozoic materials of Santa María la Real de Nieva outcrop has been affected by two Hercynian shear systems which developed after the main deformation phases and the intrusion of the granite rocks. The ... -
Diaclasas de tensión regionales en el Complejo Nevado-FiIábride y su relación con el contacto Alpujárride/Nevado-FiIábride (Sierra Nevada, Cordilleras Béticas)
(Sociedad Geológica de España, 1989)Nevado-Filábride rocks have been strained by a NW-SE principal set of systematic tension joints. The orientation of the least principal stress derived from the NevadoFilábride/Alpujárride contact fault gouge agree with the ... -
Edad y estructura de las rocas de Sierra Albarrana (SW dél Macizo Hespérico). Implicaciones regionales
(Sociedad Geológica de España, 1991)New structural and paleontological data prove that the rocks ofthe Sierra Albarrana area are of Lower Paleozoic age. Sierra Albarrana Quartzites probably correlates with the Lower Ordovician Quartzite of the Central Iberian ... -
El sistema de fallas normales de Sierra Nevada occidental desde el Mioceno Superior a la actualidad (Zonas Internas, Cordilleras Béticas)
(Sociedad Geológica de España, 1996)The Mecina Fault is a low-angle normal fault that superpose the Alpujarride over the NevadoFllabride and was active throughout Its whole extension before the Upper Miocene. From the Upper Miocene, high-angle normal faults ... -
Esfuerzos recientes en el sector sudoriental de la Depresión de Granada (Cordillera Bética central)
(Sociedad Geológica de España, 1997)The analysis of the seismic activity and the microtectonic study of outcrops located in the southeastern Granada Depression show that the stress states have been heterogeneous from the Upper Miocene up to the present. NE-SW ... -
Estructura profunda del sector central de las Cordilleras Béticas
(Sociedad Geológica de España, 1994)The analysis of the crustal structure of the central sector of the Betic Cordilleras, by means of deep reflection seismic profiles and gravimetry, shows that the Moho is nearly planar. The continental crust of the Iberian ... -
Estructuras extensionales en los materiales Aipujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas)
(Sociedad Geológica de España, 1992)The main deformation in the Tejeda and Canillas de Albaida Units is produced during a heterogeneous simple shearing regime that generates a planar-linear fabric. This simple shear has a topto-the-westsouhwest sense of ... -
High-pressure relics and structure of the Bou Azzer Neoproterozoic ophiolite (Anti-Atlas, Morocco)
(2008)La ofiolita de Bou Azzer marca la sutura del orógeno Pan-africano en el Anti-Atlas (Marruecos). En esta ofiolita se ha observado una paragénesis relicta de granate y rutilo, que sugiere un episodio inicial de alta presión. ... -
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 ... -
Sobre la estructura del Antiforme de El Cardoso y el Sinforme de Majaelrayo y su relación con la Falla de Berzosa
(Sociedad Geológica de España, 1988)The El Cardoso Antiform and the Majaelrayo Synform are structures which were generated during the third hercynian deformation phase (F) and are cross-cut by the Berzosa Fault, a normal accident with a dextral wrench ... -
Superposición de estructuras hercinianas en el sector de Buitrago-Somosierra (Sierra del Guadarrama, Sistema Central)
(Sociedad Geológica de España, 1991)The Preordovician rocks of the Buitrago-Somosierra area have undergone three penetrative phases of Hercynian deformation. The phases 1 & 2 are of tangential character, F1 probably generates a recumbent syncline Eastern ... -
Tasas de erosión en la cuenca de Guadix-Baza durante el Pleistoceno superior - Holoceno
(Sociedad Geológica de España, 2006)Erosion rates in the Guadix-Baza basin have been calculated drawing on a volumetric estimation of sediment loss by river erosion since the late Pleistocene. On this purpose we have perform a reconstruction of the geometrical ... -
La zona de cizalla del contacto entre el grupo de mantos del Mulhacén y la unidad del Veleta (Sierra Nevada y Sierra de los Filabres, Andalucía)
(Sociedad Geológica de España, 1986)The existence of an important ductil shear-zone developed in relation with the emplacement of the Mulhacen nappes group on the Veleta Unit (Betic Cordilleras) is manifested. The overlaping in the ENE sense is over 200 km ... -
Una zona de cizalla sinmetamórfica de importancia regional al SW de Sierra Albarrana (zona de Ossa Morena)
(Sociedad Geológica de España, 1991)A subvertical syn-metamorphic shear zone with dextral sense of movement is described. This shear sone is slightly obligue to the metamorphic zonation and the lithological contacts. The south eastern end of the Sierra ...
