Fig. 8From: Spatio-temporal characteristics of frictional properties on the subducting Pacific Plate off the east of Tohoku district, Japan estimated from stress drops of small earthquakesSpectral ratios for source models of Brune (1970) (blue) and Boatwright (1978) (red) as a function of frequency. Two panels have different corner frequencies of analyzed and EGF earthquakes (\(f_{0A}^{C}\) and \(f_{0E}^{C}\)); (a) 2.0 and 6.0 Hz and (b) 2.0 and 30.0 Hz, respectively, which are shown by black arrows. The factor \(R_{r}^{C}M_{0r}\) in Eqs. (9) and (14) is set to 10.0. We can clearly see that spectral ratios get asymptotically close to values of \(R_{r}^{C}M_{0r}\) and \(R_{r}^{C}M_{0r} \cdot \left( f_{0A}^{C}/f_{0E}^{C}\right) ^{2}\) for \(f \rightarrow 0\) and \(f \rightarrow +\infty\), respectivelyBack to article page