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dc.contributor.authorGonzález Lodeiro, Francisco
dc.contributor.authorMartínez Catalán, José R.
dc.contributor.authorMacaya, J.
dc.contributor.authorÁlvarez, F.
dc.date.accessioned2020-06-26T10:43:40Z
dc.date.available2020-06-26T10:43:40Z
dc.date.issued1988
dc.identifier.urihttp://hdl.handle.net/10272/18403
dc.description.abstractThe El Cardoso Antiform and the Majaelrayo Synform are structures which were generated during the third hercynian deformation phase (F) and are cross-cut by the Berzosa Fault, a normal accident with a dextral wrench component The ductile shear zone that outcrops in the core the El Cardoso Antiform can be related to that which exists west of the Berzosa Fault and also to that which affects the overturned limb of the Hiendelaencina Anticlinees_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGeología estructurales_ES
dc.subject.otherOrógeno Hercinianoes_ES
dc.subject.otherSierra de Guadarramaes_ES
dc.subject.otherStructural geologyes_ES
dc.subject.otherHercynian Orogenyes_ES
dc.titleSobre la estructura del Antiforme de El Cardoso y el Sinforme de Majaelrayo y su relación con la Falla de Berzosaes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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