Estructura en escamas del sector noroccidental de la Sierra de Cazorla (zona prebética) y del borde de la depresión del
Guadalquivir (provincia de Jaén)
Loading...
Official URL
Full text at PDC
Publication date
1970
Advisors (or tutors)
Editors
Journal Title
Journal ISSN
Volume Title
Publisher
Granada : Secretariado de Publicaciones de la Universidad, C.S.I.C, Sección de Geología de la Facultad de Ciencias
Citations
Exportar
Citation
Abstract
The 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.