Geofluid behaviour in successive extensional and compressional events: a case study from the southwestern end of the Vallès-Penedès Fault (Catalan Coastal Ranges, NE Spain)

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dc.contributor	Universitat de Barcelona
dc.contributor.author	Baqués, V.
dc.contributor.author	Travé i Herrero, Anna
dc.contributor.author	Roca i Abella, Eduard
dc.contributor.author	Marín, M.
dc.contributor.author	Cantarero Abad, Irene
dc.date	2013-04-05T16:44:25Z
dc.date	2013-04-05T16:44:25Z
dc.date	2012
dc.date	2013-04-05T16:44:25Z
dc.identifier.citation	1354-0793
dc.identifier.citation	606596
dc.identifier.uri	http://hdl.handle.net/2445/34457
dc.format	15 p.
dc.format	application/pdf
dc.language.iso	eng
dc.relation	10.1144/1354-079311-017
dc.relation	Petroleum Geoscience, 2012, vol. 18, p. 17-31
dc.relation	http://dx.doi.org/10.1144/1354-079311-017
dc.rights	(c) EAGE/Geological Society of London, 2012
dc.rights	info:eu-repo/semantics/openAccess
dc.subject	Carbonats
dc.subject	Serralada Litoral Catalana
dc.subject	Carbonates
dc.subject	Catalan Coastal Range (Catalonia)
dc.title	Geofluid 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.type	info:eu-repo/semantics/article
dc.type	info:eu-repo/semantics/acceptedVersion
dc.description.abstract	The 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.