Fig. 10
From: Detection of repeating earthquakes and their application in characterizing slow fault slip
Comparison of the relationship between the sequence-averaged recurrence interval (Tr) and seismic moment (Mo) for different study areas. Please note that the recurrence interval is normalized by the ratio of plate convergence rates between California and other regions. The original figures and details can be found in Nadeau and Johnson (1998) (San Andreas fault), Chen et al. (2007) (Central Taiwan), Yu (2013) (Tonga-Kermadec), and Dominguez et al. (2016) (Mexico). For NE Japan, only the data before the Tohoku-oki earthquake and sequences with 8 or more recurrences are selected from the catalog of Uchida and Matsuzawa (2013)