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)

Baqués, V.Travé i Herrero, AnnaRoca i Abella, EduardMarín, MiquelCantarero Abad, Irene2013-04-052013-04-0520121354-0793https://hdl.handle.net/2445/34457The 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.15 p.application/pdfeng(c) EAGE/Geological Society of London, 2012CarbonatsSerralada Litoral CatalanaCarbonatesCatalan Coastal Range (Catalonia)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)info:eu-repo/semantics/article6065962013-04-05info:eu-repo/semantics/openAccess