Fig. 10From: Estimation of 1-D velocity models beneath strong-motion observation sites in the Kathmandu Valley using strong-motion records from moderate-sized earthquakesSimulation of the second Mw5.1 earthquake. The simulated waveforms at TVU and PTN have similar amplitudes with the observed waveform; however, at THM, the simulation is overestimated. The result from the initial model is also shown, in gray. Waveform matching was conducted using trial and error for time windows indicated by the red arrows Back to article page