Fig. 2.From: Average slip rate at the transition zone on the plate interface beneath the Kii Peninsula, Japan, estimated from deep low-frequency tremorsPlot of the seismic moment of short-term slow slip events (SSEs) observed geodetically (NIED, 2009; Sekine et al., 2010) versus the cumulative apparent moment of a corresponding episode of DLF tremors (circles). The black solid line represents the best-fit line with the slope of 1.7×1018 N/m/s for all data in the northern area and the gray dashed line the best-fit line with the slope of 1.7×1018 N/m/s for the data in the northern northern Kii area.Back to article page