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Gómez Ballesteros, María ; Rivera, Jesus ; Muñoz, Araceli ; Muñoz Martín, Alfonso ; Acosta, Juan ; Carbó Gorosabel, Andrés ; Uchupi, E. | 2008We infer that the Alboran Basin, the first western Mediterranean Basin found after crossing Gibraltar, is an orogenic float underlained by a de´ collement system, a multi-layered ductile shear extending from 10km to between 30 and 40km below sea[...]texto impreso
Rodríguez Zurrunero, Alvaro ; Granja Bruña, José Luis ; Muñoz Martín, Alfonso ; Leroy, Sylvie ; Ten Brink, Uri S. ; Gorosabel-Araus, J.M. ; Gómez de la Peña, Laura ; Druet Vélez, María ; Carbó Gorosabel, Andrés | Elsevier | 2020-02-07The North American (NOAM) plate converges with the Caribbean (CARIB) plate at a rate of 20.0 ± 0.4 mm/yr. towards 254 ± 1º. Plate convergence is highly oblique (20-10º), resulting in a complex crustal boundary with along-strike segmentation, str[...]texto impreso
Along the Eastern Greater Antilles (Hispaniola and Puerto Rico area) takes place the interaction between the Caribbean and North-American plates. This interaction produced inside a broad band of deformation with a complex and active tectonics. H[...]texto impreso
Carbó Gorosabel, Andrés ; Muñoz Martín, Alfonso ; Martín Dávila, José ; Catalán, Manuel ; Garcia, Alicia | 2001La Isla Decepción es la parte emergida de un volcán muy joven y activo. Se encuentra situada en el SO del Estrecho de Bransfield, que separa la Península Antártica de las islas Shetland del Sur. En este trabajo se muestran los resultados del lev[...]texto impreso
Andrews, Brian D. ; Ten Brink, Uri S. ; Danforth, William W. ; Chaytor, Jason D. ; Granja Bruña, José Luis ; Llanes Estrada, Pilar ; Carbó Gorosabel, Andrés | Geological Survey (Estados Unidos | 2013Multibeam bathymetric data collected in the Puerto Rico Trench and northeastern Caribbean region are compiled into a seamless bathymetric terrain model for broad-scale geological investigations of the trench system. These data, collected during [...]texto impreso
Druet Vélez, María ; Muñoz Martín, Alfonso ; Granja Bruña, José Luis ; Carbó Gorosabel, Andrés ; Llanes Estrada, Pilar ; Catalán, Manuel | Taylor & Francis | 2019-08-12The NW Iberian continental margin has a complex structure, resulting from the succession of several rifting episodes close to a ridge triple junction, and a superimposed partial tectonic inversion stage. The wide-ranging physiography matches the[...]texto impreso
Druet Vélez, María ; Muñoz Martín, Alfonso ; Granja Bruña, ALFONSO ; Carbó Gorosabel, Andrés ; Llanes Estrada, Pilar ; Maestro, Adolfo ; Bohoyo, Fernando ; Martín Dávila, José | Taylor and Francis Inc. | 2019-07-12The NW Iberian continental margin has a complex structure, resulting from the succession of several rifting episodes close to a ridge triple junction, and a superimposed partial tectonic inversion stage. The wide-ranging physiography matches the[...]texto impreso
Druet Vélez, María ; Muñoz Martín, Alfonso ; Granja Bruña, José Luis ; Carbó Gorosabel, Andrés ; Acosta, Juan ; Llanes Estrada, Pilar ; Ercilla, Gemma | Sociedad Geológica de España | 2016El margen continental de Galicia presenta una estructura muy compleja, debido a dos efectos principales. Por un lado, se trata de un margen de rift pobre en magma, generado en las proximidades del punto triple R-R-R que dio lugar a la apertura s[...]texto impreso
Vicente Muñoz, Gerardo de ; Vegas, Ramón ; Muñoz Martín, Alfonso ; Silva Barroso, Pablo Gabriel ; Andriessen, Paul ; Cloetingh, Sierd ; González Casado, José Manuel ; Van Wees, Jan Diederik ; Álvarez García, Juan ; Carbó Gorosabel, Andrés ; Olaiz Campos, Antonio José | Elsevier | 2007The Spanish Central System is a Cenozoic pop-up with an E-W to NE-SW orientation that affects all the crust (thick-skinned tectonics). It shows antiform geometry in the upper crust with thickening in the lower crust. Together with the Iberian Ch[...]texto impreso
Granja Bruña, José Luis ; Carbó Gorosabel, Andrés ; Muñoz Martín, Alfonso ; Gómez Ballesteros, María | 2006The Muertos Deformed Belt (MDB) is a tectonic feature located within the Northeastern Caribbean Plate Boundary Zone. This deformed belt is occupying a broad band of active compression regime with an east-west trend along the south of Hispaniola [...]texto impreso
García Mayordomo, Julián ; Pérez Santisteban, Itziar ; Pantín, V. ; Muñoz Martín, Alfonso ; Carbó Gorosabel, Andrés | Sociedad Geológica de España. | 2008En este estudio se contrastan los resultados que ofrecen dos técnicas de uso habitual en el Laboratorio de Geotecnia del CEDEX, el AEOS y el PS-logging, con los de una técnica relativamente novedosa, el Re-Mi (o sísmica pasiva). Para ello se emp[...]texto impreso
Pérez Santisteban , Itziar ; García Mayordomo, Julián ; Muñoz Martín, Alfonso ; Carbó Gorosabel, Andrés | Elsevier Science B.V., Amsterdam. | 2011-01Results obtained by SASW and PS-logging (in-hole) seismic techniques are compared with the relatively new ReMi (Refraction microtremor) method at a common site with a well-known soil profile: a recently constructed high-speed railway embankment.[...]texto impreso
Druet Vélez, María ; Muñoz Martín, Alfonso ; Granja Bruña, José Luis ; Carbó Gorosabel, Andrés ; Acosta, Juan ; Llanes Estrada, Pilar ; Ercilla, Gemma | AGU | 2018-04The magma?poor rifted continental margin of Galicia has an extremely complex structure. Its formation involved several rifting episodes that occurred ultimately during the early Cretaceous near a ridge triple junction, which produced a change in[...]texto impreso
Druet Vélez, María ; Muñoz Martín, Alfonso ; Granja Bruña, José Luis ; Carbó Gorosabel, Andrés ; Acosta, Juan ; Llanes Estrada, Pilar ; Ercilla, Gemma | AGU | 2018-03-27The magma?poor rifted continental margin of Galicia has an extremely complex structure. Its formation involved several rifting episodes that occurred ultimately during the early Cretaceous near a ridge triple junction, which produced a change in[...]texto impreso
Bergamín de la Viña, Juan Francisco ; Carbó Gorosabel, Andrés | Instituto Geológico y Minero de España (Madrid) | 1985En la región de Campo de Calatrava se ha realizado un estudio gravimétrico detallado, cubriendo una zona de unos 4.500 Km2• Sobre el mapa de anomalías de Bouguer se localizan tres áreas de anomalías negativas, con valores que oscilan entre los 8[...]
