RT Journal Article
T1 Pliegues tumbados en los Alpujárrides de Sierra de Las Estancias (Cordilleras Béticas orientales)
T1 Recumbent folds in the Alpujárrides of the Sierra de Las Estancias (Eastern Betic Cordilleras)
A1 Galindo Zaldívar, Jesús
A1 Jabaloy, A.
A1 Campos, J.
A1 Fernández Fernández, Estefanía
AB The structure of Los Blanquizares-Oria Alpujárríde unit in northern Sierra de Las Estancias is mainly determined by kilometric recumbeot North vergent folds. Foliation axial planar to these folds is a crenulation foliation in schists. Large folds are deformed by mylonite bands and by the Alpujárríde-Maláguide fault structures. The interference with late open folds develops large 'tête plongeante' structures in the area. In addition, other late deformation structures (normal and strike-slip faults and dykes) have been recognized in the area
PB Sociedad Geológica de España
YR 1997
FD 1997
LK http://hdl.handle.net/10272/10464
UL http://hdl.handle.net/10272/10464
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 1 jun 2026