Fig. 10From: Surface rupture and characteristics of a fault associated with the 2011 and 2016 earthquakes in the southern Abukuma Mountains, northeastern Japan, triggered by the Tohoku-Oki earthquakeCorrelation of events on the Mochiyama fault and paleoearthquakes on the Yunodake and Itozawa faults. The bottom plot shows the timing of paleomegathrust earthquakes based on turbidite paleoseismology in the Japan Trench (Usami et al. 2018)Back to article page