@article{10272/10163,
year = {1998},
url = {http://hdl.handle.net/10272/10163},
abstract = {Folds, reverse faults and thrusts in the South Portuguese Zone (SW Iberia) have been classically related with the progressive deformation of the Variscan thrust -fold belt. All structures verge toward South and Southwest. The style of folds in multilayers is analysed in this work. Ductile, brittle-ductile and brittle shear zones cut across the tight folds wisch exibit a WNW-ESE trend. The dip of axial surfaces varies from moderately inclined to upright. Detailed research in the Valverde del Camino anticlinal has revealed the existence of dome-basin patterns of folds related with the thrusts. The regional structures such as the Puebla de Guzmán and Valverde del Camino anticlinorium are associated with the geometry of thrusts},
publisher = {Sociedad Geológica de España},
keywords = {Thrust-folds belts},
keywords = {Progressive deformation},
keywords = {South Portuguese Zone},
title = {Deformación progresiva de la Zona Sudportuguesa: Plegamiento y cizallamiento de secuencias multicapa},
title = {Progressive deformation in the South Portuguese Zone: Folding and shearing of multilayers},
author = {Alonso Chaves, Francisco Manuel and García Navarro, Encarnación and Camacho Cerro, Manuel Alejandro},
}