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Earth, Planets and Space
Fig. 2 | Earth, Planets and Space

Fig. 2

From: Numerical earthquake model of the 20 April 2015 southern Ryukyu subduction zone M6.4 event and its impact on seismic hazard assessment

Fig. 2

The stations used in the source inversion and waveform comparisons between synthetics and observations. a Teleseismic body waves (P wave), and b local strong motion waveforms. Black lines are observations, and red lines are synthetics. The number beneath the station (blue triangle) indicates the peak value of observation. For the teleseismic waveform, both the synthetics and observations were employed a band-pass filter between 0.01 and 0.5 Hz. For the local strong motion data, the vertical component waveforms were integrated from acceleration to velocity and then a band-pass filter was applied between 0.02 and 0.1 Hz. The waveform misfits of the teleseismic and local strong motion data are 0.20 and 0.38, respectively

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