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Sea-level changes and depositional environments in the İzmit Gulf, eastern Marmara Sea, during the late glacial–Holocene period

Autor: Çağatay, M.N., Görür, N., Polonia, A., Demirbağ, E., Sakınç, M., Cormier, M.-H., Capotondi, L., McHugh, C., Emre, Ö., Eriş, K.

Publikováno v: In Marine Geology 2003 202(3):159-173

The North Anatolian Fault within the Sea of Marmara: a new interpretation based on multi-channel seismic and multi-beam bathymetry data

Autor: İmren, C., Le Pichon, X. ^*, Rangin, C., Demirbağ, E., Ecevitoğlu, B., Görür, N.

Publikováno v: In Earth and Planetary Science Letters 2001 186(2):143-158

Active submarine tectonism and formation of the Gulf of Saros, Northeast Aegean Sea, inferred from multi-channel seismic reflection data

Autor: Kurt, H. ^*, Demirbaǧ, E., Kuşçu, İ.

Publikováno v: In Marine Geology 2000 165(1):13-26

Steady late quaternary slip rate on the Cinarcik section of the North Anatolian fault near Istanbul, Turkey

Autor: Kurt, H., Sorlien, C. C., Seeber, L., Steckler, M.S, Shillington, D.J., Cifci, G., Cormier, M.H., Dessa, J.-X., Atgin, O., Dondurur, D., Demirbag, E., Okay, S., Imren, C., Gurcay, S., Carton, H.

Publikováno v: Geophysical Research Letters
Geophysical Research Letters, American Geophysical Union, 2013, 40 (17), pp.4555-4559. ⟨10.1002/grl.50882⟩
Geophysical Research Letters, 2013, 40 (17), pp.4555-4559. ⟨10.1002/grl.50882⟩

International audience; The distribution of plate motion between multiple fault strands and how this distribution may evolve remain poorly understood, despite the key implications for seismic hazards. The North Anatolian Fault in northwest Turkey is

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::8ee726b3e6c1fe8c2ab001c77f0d1a07
https://hal.archives-ouvertes.fr/hal-00876529