Dabrio González, Cristino JoséLópez-Garrido, A. C.2023-06-212023-06-2119700366-600X10375https://hdl.handle.net/20.500.14352/64542The succession of different stages of deformation, the last of them having taken place in the middle Miocene, has determined the imbricated structure of the Sierra de Cazorla and the easternmost boundary of the Guadalquivir Basin. The evolution of the structural features is analyzed and a tectonic interpretation of the resulting structure is attempted.spajournal articleopen accessTectónica regionalPrebéticoCuenca del GuadalquivirGeología estratigráficaGeodinámica2506.19 Estratigrafía2507 Geofísica