Thesis Collection
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Browsing by Author "Capote, Ramón"
Now showing items 1-13 of 13
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Actividad neotectónica de la Falla de Alentejo-Plasencia en Extremadura (Macizo Hespérico)
(Sociedad Geológica de España, 1996)Signs of recent tectonic activity are found at the Extremadura sector of Alentejo-Plasencia fault. This fault was active during the alpine compressional period as a sinistraI strike-slip fault at the foreland of a collisional ... -
Estudio por interferometria de radar (Insar) del terremoto de Muía (Murcia) de febrero 1999 (mb: 4.8) aplicado a la caracterizacón de la fuente sismogenética
(Sociedad Geológica de España, 2001)The RADAR interferometry (INSAR) is a modern technique that offers the possibility to identify and quantify surface displacements using phase differences from two different RADAR images (Massonnet and Feigl, 1998). The ... -
Evidencias morfotectónicas de actividad reciente de la zona de falla de El Salvador en el segmento Ilopango-San Vicente
(Sociedad Geológica de España, 2005)El Salvador Fault Zone is one of the main strike-slip structures of the Central American volcanic arc. The February 2001 earthquake took place in the Ilopango – San Vicente segment of this fault zone. In this work we ... -
Evolución de las deformaciones alpinas en el Sistema Central Español (S.C.E.)
(Sociedad Geológica de España, 1989)The Alpine Structure in the Spanish Central System results from three main regional deformation phases (1-Ibérica, 2-Guadarrama, 3-Torrelaguna) with differents shortening directions, 1-N45E, 2-N750E, 3-N160-200E. The ... -
Interpretación sismotectónica de la serie sísmica de Gérgal (2002, Mw 4.8) mediante datos sismológicos y de interferometría de RADAR (INSAR)
(Sociedad Geológica de España, 2005)This work analyzes the geological source of the Mw 4.8 February 4 2002, Gérgal earthquake. The interpretation of local geological data, the relocation of the aftershocks sequence using a local velocity model, the focal ... -
La cristalinidad de la illita y las temperaturas de las últimas etapas de deformación en la zona de cizalla extensional de Santa María de La Alameda (Sistema Central, España)
(Sociedad Geológica de España, 2002)The illite crystallinity index of Kubler (1C) has been studied to establish the conditions of the last deformation stages in the Santa María de la Alameda shear zone. For this study, it has been used mainly the fine grained ... -
La fábrica de las rocas miloníticas de la Zona de Cizalla de Los Llanos (Calzadilla de los Barros, Badajoz)
(2009)The Los Llanos Shear Zone bounds the Cabeza Gorda and Zafra units located in the Ossa-Morena Zone (SW Iberian Massif). Within the Cabeza Gorda unit two peridotitic massifs crop out, named Sierra Cabeza Gorda and Cerro ... -
La geometría fractal de los bordes de grano del cuarzo como geotermómetro: Aplicación a la Zona de Cizalla Dúctil Extensional de Santa María de la Alameda (Sistema Central)
(Sociedad Geológica de España, 2001)Principles of fractal geometry have been applied to the description of quartz grain borders and to the assessment of deformation temperature in milonitic rocks at the Santa Maria de la Alameda Ductile Shear Zone (Central ... -
La Sierra de Cártama: Pliegue con actividad reciente en las Béticas Occidentales (Hoya de Málaga)
(Sociedad Geológica de España, 2001)In this work is shown how an active fold (the Sierra de Cartama fault) is marked by the drainage pattern and topography, besides of structural data. The Sierra de Cartama fold is an asymmetric fold with double plunge and ... -
La tectónica alpina de la Falla de Alentejo-Plasencia (Macizo Hespérico)
(Sociedad Geológica de España, 1996)Alentejo-Plasencia fault was active during the alpine compressional phases with a sinistral strike-slip movement in two main stages. The fault geometry was straight and no important bendings formed during Paleogene, when ... -
Modelo gravimétrico tridimensional del “stock” de Aguablanca (Badajoz)
(2006)The Aguablanca stock is located in the NE zone of the Santa Olalla Igneous Complex, in the Ossa-Morena Zone. Paleozoic rocks of the Bodonal-Cala Complex and Santa Olalla tonalites bound this gabbronorite stock. This rock ... -
Primeros resultados de huellas de fisión en apatito en el sector Lugo-Ancares (Noroeste de la Península Ibérica)
(2006)The Northwest of the Iberian Peninsula is characterised by the absence of Mesozoic sedimentary deposits, the Cenozoic sediments being scarce. Due to that, the chronology of the geological events in the area is difficult ... -
Tectónica extensional en el Sistema Central: La Zona de Cizalla Dúctil de Santa María de la Alameda (Madrid)
(Sociedad Geológica de España, 1999)The Santa Maria de Alameda (Madrid) Ductile Shear Zone is a complex mylonitic belt trending east -West and dipping 30°-60° southward. The hanging wall block sinks towards the South-Southeast. Its kinematics is in relation ...
