[HTML][HTML] Maximum earthquake magnitudes along different sections of the North Anatolian fault zone

M Bohnhoff, P Martínez-Garzón, F Bulut, E Stierle… - Tectonophysics, 2016 - Elsevier
Constraining the maximum likely magnitude of future earthquakes on continental transform
faults has fundamental consequences for the expected seismic hazard. Since the recurrence …

Dinocyst assemblages and water surface conditions in the Sea of Marmara during MIS 6 and 5 from two long cores

SAG Leroy, P Henry, F Marret, C Paillès, L Licari… - Quaternary Science …, 2023 - Elsevier
Abstract The Sea of Marmara is the connection between the vast Black Sea-Caspian Sea
basin (Pontocaspian) and the Global Ocean via the Mediterranean Sea. Its water levels and …

Tectonic and sedimentary controls on widespread gas emissions in the Sea of Marmara: Results from systematic, shipborne multibeam echo sounder water column …

S Dupré, C Scalabrin, C Grall… - Journal of …, 2015 - Wiley Online Library
Understanding of the evolution of fluid‐fault interactions during earthquake cycles is a
challenge that acoustic gas emission studies can contribute. A survey of the Sea of Marmara …

The geometry of the North Anatolian transform fault in the Sea of Marmara and its temporal evolution: implications for the development of intracontinental transform …

AMC Şengör, C Grall, C Imren… - Canadian Journal of …, 2014 - cdnsciencepub.com
The North Anatolian Fault is a 1200 km long strike-slip fault system connecting the East
Anatolian convergent area with the Hellenic subduction zone and, as such, represents an …

Propagation of a strike-slip plate boundary within an extensional environment: the westward propagation of the North Anatolian Fault

X Le Pichon, AMC Şengör, J Kende… - Canadian Journal of …, 2016 - cdnsciencepub.com
We document the establishment of the Aegea–Anatolia/Eurasia plate boundary in Pliocene–
Pleistocene time. Before 2 Ma, no localized plate boundary existed north of the Aegean …

Interseismic strain build-up on the submarine North Anatolian Fault offshore Istanbul

D Lange, H Kopp, JY Royer, P Henry, Z Çakir… - Nature …, 2019 - nature.com
Using offshore geodetic observations, we show that a segment of the North Anatolian Fault
in the central Sea of Marmara is locked and therefore accumulating strain. The strain …

The implications of fault zone transformation on aseismic creep: Example of the North Anatolian Fault, Turkey

M Kaduri, JP Gratier, F Renard, Z Çakir… - … Research: Solid Earth, 2017 - Wiley Online Library
Aseismic creep is observed at surface along several segments of the North Anatolian right‐
lateral active fault in Turkey, a major plate boundary between Eurasia and Anatolia …

Seafloor geodesy revealed partial creep of the North Anatolian Fault submerged in the Sea of Marmara

R Yamamoto, M Kido, Y Ohta… - Geophysical …, 2019 - Wiley Online Library
In this study, the creep rate across the North Anatolian Fault was directly measured in the
western Sea of Marmara using the seafloor acoustic ranging technique; the data reveal …

The north Anatolian fault and the north Anatolian shear zone

AMC Şengör, C Zabcı - Landscapes and landforms of Turkey, 2019 - Springer
Abstract The North Anatolian Shear Zone (NASZ) and its most prominent member, the North
Anatolian Fault (NAF), initiated some 11 million years ago, together form the northern …

Evidence for a minimum 52±1 km of total offset along the northern branch of the North Anatolian Fault in northwest Turkey

K Akbayram, CC Sorlien, AI Okay - Tectonophysics, 2016 - Elsevier
Abstract The North Anatolian Fault (NAF) splits into two major branches in northwestern
Turkey with most of the present strain accumulation and Holocene displacement being …