28 Nov 2022
28 Nov 2022
Status: this preprint is open for discussion.

Oblique rifting triggered by slab tearing and back-arc extension: the case of the Alboran rift in the eastern Betics

Marine Larrey1,2, Frederic Mouthereau1, Damien Do Couto3, Emmanuel Masini4, Anthony Jourdon5, Syvlain Calassou2, and Veronique Miegebielle2 Marine Larrey et al.
  • 1Université Paul Sabatier, Géosciences Environnement Toulouse, GET UMR 5563, Toulouse, France
  • 2TOTAL S.A., Centre Scientifique & Technique Jean Féger, Pau, France
  • 3Sorbonne Université, CNRS-INSU, Institut des Sciences de la Terre Paris, ISTeP UMR 7193, F-75005 Paris, France
  • 4M&U sas, France
  • 5Institute of Geophysics, Ludwig-Maximilians-Universität München, Germany

Abstract. The tectonic evolution of highly oblique continental margins that result from back-arc extension above lithospheric STEP faults is poorly understood. Here, we investigate the case of the Alboran margin in the eastern Betics characterized by crustal thinning of 15–10 km, oblique to the direction of slab retreat. The current deformation patterns indicate that oblique back-arc rifting is underway. However, it is unclear whether these conditions are those that prevailed during the formation of the metamorphic domes and intramontane basins. We review the temporal and spatial evolution of Neogene sedimentary basins and brittle deformation in the eastern Betics, and exploit offshore seismic reflection lines to propose a crustal-scale section across the oblique margin. The history of sediment infill and rates of subsidence combined with the analyses of fault slip data, confirm that brittle extension oriented from N20° E to EW occurred during an interval spanning from the Serravallian-early Tortonian to the late Tortonian (14–8 Ma). This extension is found associated with both normal and strike-slip regimes and the evolution of the strike-slip corridors flanking the metamorphic domes. The transtensional model forms a coherent scheme linking the ductile deformation associated with metamorphic domes and the formation of EW- and NW-SE/NNW-SSE-directed sedimentary basins in the brittle upper crust during the Tortonian. The oblique extension, which is closely associated with STEP faulting, occurred during the regional convergence between Africa and Iberia since the Miocene. Only recently, around 8 Ma, the slab detached, leading to local tectonic inversion. Such a type of narrow oblique rifted margin associated with transform-like plate boundaries is not unique but is expected to be hardly preserved in the geological record due to the transient nature of retreating subduction systems.

Marine Larrey et al.

Status: open (until 22 Feb 2023)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2022-1166', Peter Haughton, 02 Dec 2022 reply
    • AC1: 'Reply on CC1', Frédéric Mouthereau, 03 Dec 2022 reply

Marine Larrey et al.


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Short summary
Extension leading to the formation of ocean-continental transition can be highly oblique to the main direction of crustal thinning. Here we explore the case of a continental margin exposed in the Betics, north of the Alboran margin, that developed in back-arc setting perpendicular to the direction of retreating Gibraltar subduction. We show that transtension is the main mode of crustal deformation that best explains the formation of metamorphic domes, extensional basins and brittle faults.