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Geodynamical framework and hydrocarbon plays of a salt giant: the NW Mediterranean Basin

AutorGranado, Pablo; Urgeles, Roger ; Sàbat, F.; Albert-Villanueva, Eduard; Roca, Eduard; Muñoz, Josep A.; Mazzuca, Nicoletta; Gambini, Roberto
Fecha de publicaciónnov-2016
EditorGeological Society of London
CitaciónPetroleum Geoscience 22(4): 309-321 (2016)
ResumenThe NW Mediterranean Basin developed during the Oligocene-Miocene rifting of the Eastern Iberian-European magma-poor continental margin. The margin developed as a result of back-arc extension associated with the rollback of the retreating Calabrian-Tethys subduction zone. Reinterpretation of 2D regional seismic reflection data suggests that rifting took place by hyperextension of the Iberian-European lithosphere. This process led to the seawards arrangement of distinct crustal domains: namely, proximal, necking and distal. The late post-rift Messinian salinity crisis (MSC) gave rise to significant margin erosion and canyon incision, the lowstand sedimentary by-products of which were largely deposited prior to the Messinian evaporitic sequences. Mesozoic-Cenozoic and Messinian-Recent salt tectonics events have been recognized. A regional hydrocarbon play concept is proposed here for shelf-deep-water settings, including pre-salt, Messinian and post-salt plays
DescripciónThematic set: The Messinian salinity crisis.-- 13 pages, 8 figures, 2 tables
Versión del editorhttps://dx.doi.org/10.1144/petgeo2015-084
Identificadoresdoi: 10.1144/petgeo2015-084
issn: 1354-0793
e-issn: 2041-496X
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