Fig. 5

Moment tensor solution of the M_w 4.7 (M_L 5.8 M_Lv 5.3) Lamjung mainshock determined using the Time-Domain Deviatoric Moment Tensor Inversion method of Dreger (2003). The observed data (in black) and the synthetic data (in red) calculated using the Earth’ model called CRUST2 show an overall good agreement for the three components of the 8 stations used in the inversion. The solution obtained at 16 km depth indicates a moment magnitude (Mw) 4.7 reverse mechanism with nearly pure double-couple (DC) NEE–SWW faulting. Data are filtered between 20 and 40 s period for stations in Nepal, and between 40 and 80 s period for further stations (LSA and TARG)