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2016-08-01

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Si us plau utilitzeu sempre aquest identificador per citar o enllaçar aquest document: https://hdl.handle.net/2445/183555

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

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Recurs relacionat

https://doi.org/10.1144/petgeo2015-084

Resum

The North Western 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 roll-back 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 seaward arrangement of distinct crustal domains, namely proximal, necking and distal. The late post-rift Messinian Salinity Crisis (MSC) gave place to significant margin erosion and canyon incision whose lowstand sedimentary by-products were largely deposited prior to the Messinian evaporitic sequences. Mesozoic-Cenozoic and Messinian to recent salt tectonics events have been recognized. A regional hydrocarbon play concept is here proposed for shelf to deep waters settings, including pre-salt, Messinian and post-salt plays.

Matèries

Tectònica salina, Geodinàmica, Mediterrània (Costa)

Matèries (anglès)

Tectonique du sel, Geodynamics, Mediterranean Coast

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Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

Citació

GRANADO, Pablo, et al. Geodynamical framework and hydrocarbon plays of a salt giant: the North Western Mediterranean Basin. Petroleum Geoscience. 2016. Vol. 22, num. 4, pags. 309-321. ISSN 1354-0793. [consulted: 19 of August of 2026]. Available at: https://hdl.handle.net/2445/183555

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