Thesis Collection
Last Deposit
Browsing by Author "Galindo Zaldívar, Jesús"
Now showing items 1-20 of 38
-
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 ... -
Anomalías gravimétricas y estructura del abanico aluvial de La Zubia (Sierra Nevada occidental, Cordilleras Béticas)
(Sociedad Geológica de España, 2005)La Zubia alluvial fan is located at the boundary between the western slopes of Sierra Nevada and the Granada depression. The Alpujárride rocks of the northwestern flank of Sierra Nevada antiform constitute its metamorphic ... -
Anomalías gravimétricas y magnéticas en la Depresión de Granada (Cordilleras Béticas): tratamiento e interpretación
(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 ... -
Anomalías magnéticas y estructura profunda del Complejo Alcalino de Monchique (Zona Sudportuguesa)
(2013)Las anomalías magnéticas en el suroeste de la Península Ibérica están caracterizadas por un gran dipolo N-S alargado en dirección E-O. Los valores más intensos de anomalía están relacionados con los afloramientos ... -
Cinemática y paleoesfuerzos en la zona de falla transcurrente de Jebha-Chrafate (Rif septentrional, Marruecos)
(Sociedad Geológica de España, 2005)The Jebha-Chrafate is an ENE-WSW sinistral major transcurrent fault of the Rif Cordillera, formed during the southwestwards emplacement of the Internal Zones on the Flysch units and the External Zones. The analysis of ... -
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 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 ... -
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 ... -
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 U/Th de los travertinos de Beni Younech y correlación con las terrazas marinas cuaternarias de Ras Leona (SE del Estrecho de Gibraltar, Marruecos)
(2008)Three travertinic levels have been identified in the Beni Younech village, near the Quaternary marine terraces of Ras Leona Point, in the south-eastern coast of the Gibraltar Strait. These travertines developed probably ... -
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 pliegue sinsedimentario de Hinojares (sector de Pozo Alcón-Tíscar, provincia de Jaén, zona externa bética)
(2006)In the proximities of Hinojares (northern border of the Guadix-Baza basin), there is a growth syncline, formed in Plio-Quaternary sediments, showing progressive unconformities in its limbs. At its ESE prolongation, the ... -
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 ... -
Espesor de los sedimentos neógenos y cuaternarios en el Corredor del Almanzora a partir de datos gravimétricos (Cordillera Bética oriental)
(2007)New gravity data contribute to determine the geometry of the sedimentary infill in the Almanzora Corridor. Residual gravity anomalies was considered along 2D models to establish the deep structure of the basin, taking ... -
Establecimiento preliminar de la posición de la interfase agua dulce-agua salada en el sector de la desembocadura del río Guadalfeo (acuífero Motril-Salobreña) mediante técnicas geofísicas y registros de salinidad
(Universidad de Huelva, 2011)Se realizaron campañas geofísicas (Sondeos electromagnéticos en el dominio del tiempo y tomografía eléctrica) en el acuífero Motril-Salobreña para detectar la cuña salina que revelaron incertidumbres acerca de la ... -
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 de la Cuenca de Ugíjar a partir de datos gravimétricos y magnéticos (Zonas Internas, Cordillera Bética Central)
(2013)Nuevas medidas gravimétricas y magnéticas adquiridas en la Cuenca de Ugíjar contribuyen a determinar el espesor de su relleno sedimentario y las estructuras que deforman las rocas sedimentarias y el basamento. La combinación ...
