RT Journal Article
T1 Estructura en escamas del sector noroccidental de la Sierra de Cazorla (zona prebética) y del borde de la depresión delGuadalquivir (provincia de Jaén)
A1 Dabrio González, Cristino José
A1 López-Garrido, A. C.
AB 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 resultingstructure is attempted.
PB Granada : Secretariado de Publicaciones de la Universidad, C.S.I.C, Sección de Geología de la Facultad de Ciencias
SN 0366-600X
YR 1970
FD 1970
LK https://hdl.handle.net/20.500.14352/64542
UL https://hdl.handle.net/20.500.14352/64542
LA spa
DS Docta Complutense
RD 10 abr 2025