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Progressive deformation in the South Portuguese Zone: Folding and shearing of multilayers

dc.contributor.authorAlonso Chaves, Francisco Manuel 
dc.contributor.authorGarcía Navarro, Encarnación 
dc.contributor.authorCamacho Cerro, Manuel Alejandro
dc.description.abstractFolds, 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 thrustsen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherThrust-folds beltsen_US
dc.subject.otherProgressive deformationen_US
dc.subject.otherSouth Portuguese Zoneen_US
dc.titleDeformación progresiva de la Zona Sudportuguesa: Plegamiento y cizallamiento de secuencias multicapaen_US
dc.titleProgressive deformation in the South Portuguese Zone: Folding and shearing of multilayerseng

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