Fig. 4From: Joint inversion of teleseismic, geodetic, and near-field waveform datasets for rupture process of the 2015 Gorkha, Nepal, earthquakeObserved (red) and synthetic (black) waveforms at a teleseismic stations and b strong motion and high-rate GPS stations. Station code, component, and peak amplitude (micrometer for teleseismic and centimeter for near-field) are written on the left of each waveform. Observed (red) and synthetic (black) ground deformations from c horizontal component of static GPS, d vertical component of static GPS, and e InSAR. Line-of-sight deformations were derived from the processed InSAR images (Lindsey et al. 2015) and are used for the joint source inversion. Red star denotes the main shock epicenterBack to article page