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Pous, Jaume ; Muñoz Martín, Alfonso ; Olaiz Campos, Antonio José ; Seillé, H. ; De Vicente Muñoz, Gerardo | Sociedad Geológica de España. | 2012We present a magnetotelluric profile across the Duero basin, the Central System and the Madrid basin, acquired in the framework of the TOPO-IBERIA project. The MT profile consists of 24 magnetotelluric sites over a 200 km, NS oriented profile. F[...]texto impreso
Olaiz Campos, Antonio José ; Muñoz Martín, Alfonso ; Gascone, L. ; De Vicente Muñoz, Gerardo ; Mantilla Pimiento, A. | Sociedad Geológica de España. | 2012The Madrid basin, over 20.000 km2 , located in Central Spain. Its evolution is conditioned by basement uplifts (Central System and Toledo Mountains) during the Alpine orogeny. The Madrid basin is connected with the Loranca basin at its NE corner[...]texto impreso
De Vicente Muñoz, Gerardo ; Muñoz Martín, Alfonso ; Olaiz, A.J. ; Vegas, Ramón ; Antón López, Loreto ; Martín Velázquez, Silvia ; Giner Robles, J. ; Rodriguez Pascua, M.A. | Sociedad Geológica de España | 2019La idea del origen compresivo del Sistema Central (SC) se debe a Birot y Solé Sabarís (1954) [1], antes del establecimiento del papel que la tectónica de placas juega en el desarrollo de las estructuras intraplaca. Sin embargo, sus observaciones[...]texto impreso
El registro geológico de las deformaciones alpinas en el interior de Iberia durante el Cenozoico, indica la presencia de varios campos de paleoesfuerzos. Desde el análisis de poblaciones de microestructuras, se han propuesto varios campos (“Pire[...]texto impreso
Muñoz Martín, Alfonso ; De Vicente Muñoz, Gerardo ; Olaiz Campos, Antonio José ; Antón López, Loreto ; Vegas, Ramón ; Granja Bruña, José Luis | Sociedad Geológica de España. | 2012This work shows a new on-line stress map for Iberian Peninsula obtained from the inversion of earthquakes focal mechanisms calculated with the centroid moment tensor. An amount of 299 focal mechanisms have been selected with several quality crit[...]texto impreso
En este trabajo se realizan una serie de modelos estructurales de elementos finitos sobre la geometría en profundidad del cinturón de pliegues y cabalgamientos alpinos de la Sierra de Altomira. El objetivo de estos modelos es comprobar numéricam[...]texto impreso
Antón López, Loreto ; Muñoz Martín, Alfonso ; De Vicente Muñoz, Gerardo | Cambridge University Press | 2018-05-17Formerly closed drainage basins provide exceptional settings for quantifying fluvial incision and landscape dissection at different time scales. Endorheic basins trap all the sediment eroded within the watershed, which allows estimates of post–b[...]texto impreso
Martín-González, Fidel ; Fernández Lozano, Javier ; De Vicente Muñoz, Gerardo ; Crespo Martín, Cristina | Elsevier | 2020-12-29The role of inherited weaknesses in metamorphic basements with respect to the geometry and tectonic evolution of subsequent orogens formation forms a cornerstone of structural reconstructions, especially in non-inverted orogens with old Variscan[...]texto impreso
Fernández Lozano, Javier ; Gutiérrez Alonso, Gabriel ; Willingshofer, Erns ; Sokoutis, Dimitrios ; De Vicente Muñoz, Gerardo ; Cloetingh, Sierd | Geological Society of America | 2019The present-day topography in Iberia is related to geodynamic processes dealing with lithospheric-scale deformation. However, little attention has been paid to the role of inherited crustal- or lithospheric-scale structures involved in the recen[...]texto impreso
Fernández Lozano, Javier ; Gutiérrez Alonso, Gabriel ; Sokoutis, D. ; Willingshofer, Ernst ; De Vicente Muñoz, Gerardo ; Cloetingh, Sierd | Sociedad Geológica de España. | 2016La península ibérica constituye un laboratorio natural para el conocimiento de la deformación intraplaca alpina. Aunque la actual topografía es el resultado de los últimos eventos tectónicos ocurridos entre el Eoceno y el Mioceno inferior, la ev[...]texto impreso
Fernández Lozano, Javier ; Sokoutis, Dimitrios ; Willingshofer, Ernst ; Muñoz Martín, Alfonso ; De Vicente Muñoz, Gerardo ; Cloetingh, Sierd | Sociedad Geológica de España | 2010Analogue modelling contributes to the interpretation of lithosphere scale folds in Iberia as a result of largescale convergence during Oligocene-Miocene times between the Iberian and European Plates. Different tectonothermal events affected the [...]texto impreso
Muñoz Martín, Alfonso ; De Vicente Muñoz, Gerardo ; Fernández Lozano, Javier ; Cloetingh, Sierd ; Willingshofer, Ernst ; Sokoutis, Dimitrios ; Beekman, Fred | Elsevier | 2010-09-22Large-scale folding is a key mechanism of lithospheric deformation and has been described in many parts of the Earth, both for the continental and oceanic lithospheres. Some aspects of this process such as the presence of coupling/decoupling bet[...]texto impreso
Olaiz, A.J. ; Mantilla Pimiento, A. ; Muñoz Martín, Alfonso ; De Vicente Muñoz, Gerardo | EAGE | 2015-06-01The Madrid Basin is an intraplate Cenozoic basin located in the central area of the Iberian Peninsula. Basement is characterized by a wide range of lithologies, from meta-sediments to granites. Sedimentary section is associated with a carbonatic[...]texto impreso
De Vicente Muñoz, Gerardo ; Cunha, P.P. ; Muñoz Martín, Alfonso ; Cloetingh, S.A.P.L. ; Olaiz, A. ; Vegas, Ramón | AGU | 2018The intraplate deformation of Iberia during the Cenozoic produced a series of ranges and deformation belts with a wide variety of structural trends. The Spanish-Portuguese Central System is the most prominent feature crossing over the whole of c[...]texto impreso
Antón López, Loreto ; De Vicente Muñoz, Gerardo ; Muñoz Martín, Alfonso ; Stokes, Martin | Elsevier | 2013-10-22Well-constrained case studies of transient landscape responses are needed to improve our understanding of erosion processes associated with drainage captures. The Duero basin is an excellent location for such a study because the landscape is cur[...]
