Fig. 10From: Applicability of source scaling relations for crustal earthquakes to estimation of the ground motions of the 2016 Kumamoto earthquakeComparison of the observed (black) and synthetic (red) ground motions of three components (east–west, north–south, and up–down). The available frequency range is from 0.3 to 10 Hz. a Acceleration in cm/s2, b velocity in cm/s, and c displacement in cm. The numbers in each trace indicate the maximum amplitudeBack to article page