Vegas, RamónRincón Calero, P. J.2017-02-212017-02-211995http://hdl.handle.net/10272/13360The analysis of brittle structures and regional physiographic features in the province of Ciudad Real (Central Spain), leads to establish a model of neotectonic deformation in relation with the foreland of the eastern Betic Cordillera. In this model, a weak compressive stress field is responsible for flexural bending of the crust and the lithosphere, and the occurrence of the Neogene-Quaternary volcanism in the Campo de CalatravaspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Brittle mesostructureFault population analysisLithospheric bendingBetic forelandCentral Spainjournal articleopen access