Fig. 2From: Stress change generated by the 2019 İstanbul–Silivri earthquakes along the complex structure of the North Anatolian Fault in the Marmara SeaRupture zones of the historical earthquakes and the seismic gap based on revised historical earthquakes. a Parsons (2004), b Armijo et al. (2005) and Pondard et al. (2007), c Yaltırak (2015) and Bulut et al. (2019)Back to article page