Fig. 10From: Temporal change in seismic wave attenuation using highly stable vibration sourcesExamples of the synthetic azimuthal pattern. Azimuthal variations of delays calculated by synthetic dataset are shown as examples. We showed three examples with 10, 5, and 0 ms of \(\updelta {\mathrm{t}}_{0}\) in Eq. (8). We provide \(\mathrm{A}=1,\updelta {\mathrm{t}}_{1}=1 \left[\mathrm{ms}\right],\updelta {\mathrm{t}}_{2}=2 \left[\mathrm{ms}\right]\) in Eqs. (8) and (9) for this calculationBack to article page