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 …

We studied source mechanism parameters and slip distributions of earthquakes with Mw≥
5.0 occurred during 2000–2008 along the Hellenic subduction zone by using teleseismic P …

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 …

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 …

DP-wave velocity structure and Vp/Vs variations in the crust along the North Anatolian Fault
Zone (NAFZ) in north-central Anatolia were investigated by the inversion of local P-and S …

We analyze S-receiver functions to investigate variations of lithospheric thickness below the
entire region of Turkey and surrounding areas. The teleseismic data used here have been …

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 …

We analyze the spatiotemporal evolution of seismicity during a sequence of moderate (an M
w 4.7 foreshock and M w 5.8 mainshock) earthquakes occurring in September 2019 at the …

The factors controlling fluid emission dynamics at ocean margins are poorly understood. In
particular, there are significant uncertainties on how fluid seepage at cold seeps may have …

The Marnaut cruise (May–June 2007) investigated the submerged part of the North
Anatolian fault system, an active tectonic area in the Sea of Marmara. Already known and …