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

SUMMARY 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 faul...

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Veröffentlicht in:	Geophysical journal international 2023-12, Vol.235 (3), p.2614-2639
Hauptverfasser:	Rodriguez, M, Sakellariou, D, Gorini, C, Janin, A, D'Acremont, E, Pourhiet, L Le, Chamot-Rooke, N, Tsampouraki-Kraounaki, K, Morfis, I, Rousakis, G, Henry, P, Lurin, A, Delescluse, M, Briole, P, Rigo, A, Arsenikos, S, Bulois, C, Fernández-Blanco, D, Beniest, A, Grall, C, Chanier, F, Caroir, F, Dessa, J-X, Oregioni, D, Nercessian, A
Format:	Artikel
Sprache:	eng
Schlagworte:	Environmental Sciences
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