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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)Normal access

Authors: V. Baqués, A. Travé, E. Roca, M. Marín and I. Cantarero
Journal name: Petroleum Geoscience
Issue: Vol 18, No 1, February 2012 pp. 17 - 31
DOI: 10.1144/1354-079311-017
Organisations: Geological Society of London
Language: English
Info: Article, PDF ( 3.54Mb )
Price: € 30

Summary:
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.


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