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dc.contributor.authorCampos, J.
dc.contributor.authorGarcía Dueñas, V.
dc.contributor.authorGonzález Lodeiro, Francisco
dc.contributor.authorOrozco, Miguel
dc.date.accessioned2020-07-10T07:42:51Z
dc.date.available2020-07-10T07:42:51Z
dc.date.issued1986
dc.identifier.urihttp://hdl.handle.net/10272/18498
dc.description.abstractThe existence of an important ductil shear-zone developed in relation with the emplacement of the Mulhacen nappes group on the Veleta Unit (Betic Cordilleras) is manifested. The overlaping in the ENE sense is over 200 km implying that most of the shortening in the Nevado Filabride occurred irrespectively of the convergence between Africa and Europees_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.otherDuctil sheares_ES
dc.subject.otherNappeses_ES
dc.subject.otherBetic Cordillerases_ES
dc.titleLa zona de cizalla del contacto entre el grupo de mantos del Mulhacén y la unidad del Veleta (Sierra Nevada y Sierra de los Filabres, Andalucía)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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