Figure 6
From: Temporal variation in scattering and intrinsic attenuation due to earthquakes in East Asia

(a) The Qs–1 and Qi–1 value of the BEP, AEP, and all are compared for the stations. (b–d) Topographic maps showing the difference between the BEP and AEP (AEP–BEP) for the Qs–1, Qi–1, and Qt–1 value, respectively, of the Gyeongju earthquake at 1.5 Hz. Focal mechanism28 of mainshock are shown in (d). The styles and symbols are the same as those in Fig. 5.