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Please use this identifier to cite or link to this item: https://hdl.handle.net/2445/34457
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dc.contributor.authorBaqués, V.-
dc.contributor.authorTravé i Herrero, Anna-
dc.contributor.authorRoca i Abella, Eduard-
dc.contributor.authorMarín, Miquel-
dc.contributor.authorCantarero Abad, Irene-
dc.date.accessioned2013-04-05T16:44:25Z-
dc.date.available2013-04-05T16:44:25Z-
dc.date.issued2012-
dc.identifier.issn1354-0793-
dc.identifier.urihttps://hdl.handle.net/2445/34457-
dc.description.abstractThe structural position of the Upper Jurassic-Lower Cretaceous carbonates located in the central part of the Catalan Coastal Ranges corresponds to the southwestern end of the Vallès-Penedès Fault. This fault was reactivated at different times during successive extensional and compressional events and several generations of fractures and cementations were formed.-
dc.format.extent15 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.relation.isformatof10.1144/1354-079311-017-
dc.relation.ispartofPetroleum Geoscience, 2012, vol. 18, p. 17-31-
dc.relation.urihttp://dx.doi.org/10.1144/1354-079311-017-
dc.rights(c) EAGE/Geological Society of London, 2012-
dc.sourceArticles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)-
dc.subject.classificationCarbonats-
dc.subject.classificationSerralada Litoral Catalana-
dc.subject.otherCarbonates-
dc.subject.otherCatalan Coastal Range (Catalonia)-
dc.titleGeofluid behaviour in successive extensional and compressional events: a case study from the southwestern end of the Vallès-Penedès Fault (Catalan Coastal Ranges, NE Spain)-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/acceptedVersion-
dc.identifier.idgrec606596-
dc.date.updated2013-04-05T16:44:25Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
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