RT Journal Article
T1 Deformación progresiva de la Zona Sudportuguesa: Plegamiento y cizallamiento de secuencias multicapa
T1 Progressive deformation in the South Portuguese Zone: Folding and shearing of multilayers
A1 Alonso Chaves, Francisco Manuel
A1 García Navarro, Encarnación
A1 Camacho Cerro, Manuel Alejandro
AB 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
PB Sociedad Geológica de España
YR 1998
FD 1998
LK http://hdl.handle.net/10272/10163
UL http://hdl.handle.net/10272/10163
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026