Fig. 5From: Spatio-temporal characteristics of frictional properties on the subducting Pacific Plate off the east of Tohoku district, Japan estimated from stress drops of small earthquakesa Spatial distribution of smoothed stress drop estimated by S-wave analyses from 2003 to 2010, which is before the 2011 Tohoku earthquake. Thin contours show the coseismic displacement of the 2011 Tohoku earthquake at an interval of 2 m, the same as Fig. 3 (Iinuma et al. 2012). Please note that values were not assigned at grid points with less than four earthquakes within 20 km of the epicentral distance. b Stress drops from 2012 to 2018. Clear temporal changes are observed associated with the 2011 Tohoku earthquake in areas C and D, corresponding to edges of the coseismic slip. c Stress drops for all the analyzed period of 2003 through 2018Back to article page