Thesis Collection
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Browsing by Author "Jabaloy, A."
Now showing items 1-13 of 13
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Active faults in the Granada Depression and Zafarraya areas (Betic Cordilleras)
(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 ... -
Deformaciones plio-cuaternarias en la region de Rabat
(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)
(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 ... -
Deformaciones transtensivas en la Dorsal Sur de Scotia (NE Península Antàrtica)
(Sociedad Geológica de España, 1996)The South Scotia Ridge is studied by swath bathymetry, multichannel seismic and magnetometry profiles, obtained during the HESANT 92/93 cruise. The ridge is composed by thinned continental crust fragments and to the north ... -
El límite Cuenca Powell/Mar de Weddell. Estructura y relación con la fragmentación Cenozoica de la Península Antàrtica
(Sociedad Geológica de España, 1996)Late Paleogene to Neogene continental fragmentation of the Northern Antarctic Peninsula caused the development of small oceanic-floored basins such as Powell Basin. On the basis of MCS profiles and swath bathymetry collected ... -
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 actuales en la región del Arco de Scotia
(Sociedad Geológica de España, 1996)The study of the stresses in the Scotia Arc, determined by right dihedra diagrams of earthquake focal mechanisms, illustrates the present-day tectonics of the region. The Scotia Arc is a large sinistral fault zone, with ... -
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 del graben asimétrico de Albuñuelas (Granada)
(Sociedad Geológica de España, 2018)El graben asimétrico de Albuñuelas se localiza en el extremo sureste de la cuenca intramontañosa de Granada. Su estructura se define por un sistema de fallas normales E-O que hunden el bloque de depósitos sedimentarios ... -
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 sedimentarias de deformación interpretadas como sismitas en el Mioceno Superior (Turoliense) de la cuenca de Granada (Cordillera Bética)
(2006)We studied various Upper Miocene (Turolian) layers of superimposed soft-sediment deformation structures induced by liquefaction in the Granada basin (Betic Cordillera). These are principally load structures: sagging and ... -
Geometry and kinematic of post-Aquitanian brittle deformation in the Alpujárride rocks and their relation with the Alpujárride/ Nevado-FiIábride contact
(Sociedad Geológica de España, 1991)An extensional britt/e detachment with a top-to-the-west directed movement exists between the Alpujárride and Nevado-FiIábride Complexes (Betic Cordilleras): The Mecina Detachment Fault. Extensional duplexes and thinning ... -
Pliegues tumbados en los Alpujárrides de Sierra de Las Estancias (Cordilleras Béticas orientales)
(Sociedad Geológica de España, 1997)The structure of Los Blanquizares-Oria Alpujárríde unit in northern Sierra de Las Estancias is mainly determined by kilometric recumbeot North vergent folds. Foliation axial planar to these folds is a crenulation foliation ...
