2026-06-26T15:51:24Zhttps://docta.ucm.es/rest/oai/request

oai:docta.ucm.es:20.500.14352/525482024-08-02T13:34:12Zcom_20.500.14352_14col_20.500.14352_15

Olaiz Campos, Antonio José Vicente Muñoz, Gerardo De Vegas Martínez, Ramón González Casado, José Manuel Muñoz Martín, Alfonso Álvarez, J. 2023-06-20T12:47:55Z 2023-06-20T12:47:55Z 2004 1576-5172 https://hdl.handle.net/20.500.14352/52548 http://www.sociedadgeologica.es/publicaciones_geotemas.html We describe and study structural evidences concerning to Alpine tectonics at NE sector o f the Spanish Central System (SCS). In Valdesotos area, the Hercynian basement is uplifted over Mesozoic sediments, throughout a main SW verging thrust. Fault population analysis and geological mapping has been used to look at the relation between structures in the basement and in the cover. As a consequence of accommodation of strains in the basement, kink folds are developed, such as secondary thrust and folds in the tegument. All these meso- and macrostructures seem to answer to a shortening in agreement with the Cenozoic deformation. spa open access El cabalgamiento de Valdesotos: consecuencias de la acomodación del acortamiento cenozoico en el zócalo del Sistema Central journal article