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Fig. 6 | Earth, Planets and Space

Fig. 6

From: Influence of low-velocity superficial layer on long-period basin-induced surface waves in eastern Osaka basin

Fig. 6

Surface wave propagation – semblance analysis. Left upper panel: The synthetics band passed for the semblance analysis (0.2–0.38 Hz) for model Vsmin500 at a particular station of each of the FD arrays used for semblance analysis. The right panel shows the time series of the slowness vectors (in black) with detected slowness in m/s (from semblance technique). The corresponding polarization azimuths are represented by the red sticks. See also Fig. 4

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