GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 1.1 GNGTS 2024 Fig. 1 – Seismotectonic setngs of the study area. The solid lines are the main fault segments of the EAFZ (afer Duman and Emre, 2013): (1) Amanos, (2) Pazarcık, (3) Erkenek, (4) Pütürge, (5) Palu, (6) Bingöl and (7) Sürgü-Çardak -Savrun segments, respectvely. Seismicity: the blue dots are relocated afershocks of the 2023 sequence (Lomax, 2023); red stars are the locaton of the main events and their moment tensor soluton (KOERI); yellow stars represent the major historical events (Ambraseys 1989). The botom inset shows a sketch of the main fault systems in and around Turkey, and the dashed box is the area of the main fgure. The upper inset shows an example of InSAR data: the unwrapped interferogram showing the cumulatve coseismic displacement feld from the ALOS-2 ascending track. References Ambraseys N.N.; 1989: Temporary seismic quiescence: SE Turkey. Geophys. J. Int., 96(2), doi:10.1111/j.1365-246X.1989.tb04453.x. Barbot S., Luo H., Want T., Hamiel Y., Piatbratova O., Javed M.T., Braitenberg C., Gurbuz G.; 2023: Slip distributon of the February 6, 2023 Mw 7.8 and Mw 7.6, Kahramanmaras Turkey earthquake sequence in the East Anatolian Fault Zone. Seismica, 2(3), doi:10.26443/seismica.v.2i3.502. Cheloni D., Falcucci E., Gori S.; 2019: Half-Graben Rupture Geometry of the 30 October 2016 Mw 6.6 Mt. Vetore-Mt. Bove Earthquake. J. Geophys. Res., 124, doi:10.1029/2018JB015851.