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Preuves de la discordance de l’Ordovicien supérieur dans la zone axiale des Pyrénées : exemple du dôme de la Garonne (Espagne, France)

dc.contributor.authorGarcía-Sansegundo, Joaquín 
dc.contributor.authorGavaldá, Jordi
dc.contributor.authorAlonso Alonso, Juan Luis 
dc.date.accessioned2015-10-01T10:26:36Z
dc.date.available2015-10-01T10:26:36Z
dc.date.created2015-10-01spa
dc.date.issued2004
dc.identifier.citationComptes Rendus - Geoscience, 336(11), p. 1035-1040 (2004); doi:10.1016/j.crte.2004.03.009spa
dc.identifier.issn1631-0713
dc.identifier.urihttp://hdl.handle.net/10651/33345
dc.format.extentp. 1035-1040spa
dc.language.isospaspa
dc.relation.ispartofComptes Rendus - Geosciencespa
dc.rights©
dc.sourceScopusspa
dc.source.urihttp://www.scopus.com/inward/record.url?eid=2-s2.0-3042621822&partnerID=40&md5=97c42a580b62d7a92d3a3a4455b84b36
dc.titlePreuves de la discordance de l’Ordovicien supérieur dans la zone axiale des Pyrénées : exemple du dôme de la Garonne (Espagne, France)fr
dc.title.alternativeEvidence of the Upper Ordovician unconformity in the Hercynian Pyrenean Axial Zone: Garonne Dome (Spain, France)eng
dc.typeinfo:eu-repo/semantics/article
dc.type.dcmitextspa
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.crte.2004.03.009


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