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dc.contributor.authorRoca, E.
dc.contributor.authorSantanach, P.
dc.date.accessioned2020-07-09T10:56:28Z
dc.date.available2020-07-09T10:56:28Z
dc.date.issued1986
dc.identifier.urihttp://hdl.handle.net/10272/18495
dc.description.abstractThe Cerdanya basin is located at the SW end of the Tet fault, in its NW block. Its formation, during the Upper Miocene, was conditioned by dextral slip of this fault anf the normal slip of E-W trending faults that absorbed the movement of the formeres_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.otherFaultes_ES
dc.subject.otherBasines_ES
dc.subject.otherSlipes_ES
dc.subject.otherCerdanyaes_ES
dc.titleGénesis y evolución de la fosa de la Cerdanya (Pirineos Orientales)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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