Titre :

Evolution of the North Anatolian Fault from a diffuse to a localized shear zone in the North Aegean Sea during the Plio-Pleistocene

Auteur(s) :

Rodriguez, M [Auteur]
Laboratoire de géologie de l'ENS [LGENS]
Sakellariou, D [Auteur]
Gorini, Christian [Auteur]
Institut des Sciences de la Terre de Paris [iSTeP]
Janin, A [Auteur]
Laboratoire de géologie de l'ENS [LGENS]
d'Acremont, Elia [Auteur]
Institut des Sciences de la Terre de Paris [iSTeP]
Le Pourhiet, Laetitia [Auteur]
Institut des Sciences de la Terre de Paris [iSTeP]
Chamot-Rooke, Nicolas [Auteur]
Laboratoire de géologie de l'ENS [LGENS]
Tsampouraki-Kraounaki, K [Auteur]
Morfis, I [Auteur]
Rousakis, G [Auteur]
Henry, P [Auteur]
Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement [CEREGE]
Lurin, A [Auteur]
Laboratoire de géologie de l'ENS [LGENS]
Delescluse, M [Auteur]
Laboratoire de géologie de l'ENS [LGENS]
Briole, P [Auteur]
Laboratoire de géologie de l'ENS [LGENS]
Rigo, A [Auteur]
Laboratoire de géologie de l'ENS [LGENS]
Arsenikos, S [Auteur]
Beicip Franlab
Bulois, C [Auteur]
Laboratoire de géologie de l'ENS [LGENS]
Fernández-Blanco, D [Auteur]
Instituto de Ciencias del Mar de Barcelona [ICM]
Beniest, A [Auteur]
Vrije Universiteit Amsterdam [Amsterdam] [VU]
Grall, Céline [Auteur]
Lamont-Doherty Earth Observatory [LDEO]
LIttoral ENvironnement et Sociétés [LIENSs]
Chanier, Frank [Auteur]
Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 [LOG]
Université de Lille
Caroir, Fabien [Auteur]
Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 [LOG]
Dessa, Jean-Xavier [Auteur]
Géoazur [GEOAZUR 7329]
Oregioni, D [Auteur]
Géoazur [GEOAZUR 7329]
Nercessian, A [Auteur]
Institut de Physique du Globe de Paris [IPGP (UMR_7154)]

Titre de la revue :

Geophysical Journal International

Pagination :

2614-2639

Éditeur :

Oxford University Press (OUP)

Date de publication :

2023-12-18

ISSN :

0956-540X

Mot(s)-clé(s) en anglais :

Transform faults
Submarine tectonics and volcanism
Continental tectonics: strike-slip and transform

Résumé en anglais : [en]

The North Anatolian Fault is the ∼1200-km-long active continental transform boundary between Anatolia and Eurasia. This strike-slip system initiated around 10–12 Ma and experienced diachronous episodes of strain localization ...
Lire la suite >The North Anatolian Fault is the ∼1200-km-long active continental transform boundary between Anatolia and Eurasia. This strike-slip system initiated around 10–12 Ma and experienced diachronous episodes of strain localization along its strike. The structural evolution of the ∼350-km-long fault segments crossing the North Aegean Sea remains to be accurately investigated. There, the modern North Anatolian Fault is localized along two main branches: the northern branch ends at the North Aegean Trough and the southern branch ends at the Edremit-Skyros Trough. The Evia Basin is located in the North Aegean Domain between the North Anatolian Fault and the Corinth Rift. This study presents seismic reflection lines crossing the aforementioned structures of the North Aegean Domain, which document their subsurface structure and the sedimentary record of their activity since the Messinian. The seismic-reflection data set is tied to regional-scale stratigraphic markers, which constrains the age of main tectonic events related to the formation of the North Anatolian Fault. The seismic-reflection lines show that the two main branches of the North Anatolian Fault became localized structures at 1.3–2 Ma, coevally with the formation of the Evia Basin. Since 2 Ma, the North Aegean Troughs developed as a series of horsetail basins propagating westwards at the termination of the branches of the North Anatolian Fault. On a regional scale, the wide and diffuse North Anatolian transtensive shear zone active from Serravalian to Late Pliocene turned into a narrower shear zone at the two main branches of the North Anatolian Fault since the Early Pleistocene. This abrupt episode of strain localization occurred in the frame of the major Early Pleistocene change in stress regime from NE–SW to N–S extension, which has been observed throughout the Aegean Sea.Lire moins >

Langue :

Anglais

Comité de lecture :

Oui

Audience :

Internationale

Vulgarisation :

Non

Collections :

• Laboratoire d'Océanologie et de Géosciences (LOG) - UMR 8187

Source :

Harvested from HAL