@article{10272/10464,
year = {1997},
url = {http://hdl.handle.net/10272/10464},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {Pliegues tumbados en los Alpujárrides de Sierra de Las Estancias (Cordilleras Béticas orientales)},
title = {Recumbent folds in the Alpujárrides of the Sierra de Las Estancias (Eastern Betic Cordilleras)},
author = {Galindo Zaldívar, Jesús and Jabaloy, A. and Campos, J. and Fernández Fernández, Estefanía},
}