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Extensional deformation in the upper allochthonous units of the eastern part of the Ordenes Complex (Galicia)

dc.contributor.authorMartínez Catalán, José R.
dc.contributor.authorArenas, R.
dc.date.accessioned2020-05-15T09:27:28Z
dc.date.available2020-05-15T09:27:28Z
dc.date.issued1991
dc.identifier.urihttp://hdl.handle.net/10272/17967
dc.description.abstractA penetrative extensional tectonics, which includes the existence of three important detachments, has been identified in the Sobrado area, in the eastern margin of the Ordenes Complex. It is related to the extensional collapse of an orogenic wedge built previously by crustal thickening and stacking of allochthonous terranes. The collapse could be linked to the emplacement of the terranes over their relative autochthones_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.otherExtensional tectonicses_ES
dc.subject.otherAllochthonous terraneses_ES
dc.subject.otherMafic-ultramafic complexeses_ES
dc.subject.otherGaliciaes_ES
dc.titleDeformación extensional de las unidades alóctonas superiores de la parte oriental del Complejo de Ordenes (Galicia)es_ES
dc.titleExtensional deformation in the upper allochthonous units of the eastern part of the Ordenes Complex (Galicia)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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