Fig. 4From: Estimation of the source process of the 2015 Gorkha, Nepal, earthquake and simulation of long-period ground motions in the Kathmandu basin using a one-dimensional basin structure model a Comparison of the observed (black) and synthetic (red) near-field waveforms in three components. Station name and maximum value are shown above each trace. b Comparison of the observed (black) and synthetic (red) teleseismic waveforms in the vertical component. Number beside each station name is the maximum amplitude of the observed waveform. Numbers at the end of waveforms are the station azimuth (upper number) and epicentral distance (lower number) in degreesBack to article page