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V. Baqués, A. Travé and I. Cantarero Development of successive karstic systems within the Baix Penedès Fault zone (onshore of the Valencia Trough, NW Mediterranean) Geofluids 14

Version of Record online: 24 JUN 2013 | DOI: 10.1111/gfl.12044

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The Baix Penedès fault zone records successive karstic systems. The first karstification event developed after the main phase of the Paleogene compression and is affected by the Baix Penedès fault. Related to the syn-rift, two karstification events took place, and a late karstification event, with undeformed karstic fillings, attributed to the postrift stage. The observed multiphase karstification and cementation events must be taken into consideration when interpreting the karstified limestones located at offshore, where Mediterranean oilfields developed.

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