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Published byKaarina Järvinen Modified over 5 years ago
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Fig. 2 Data for an example earthquake on 23 August 2015.
Data for an example earthquake on 23 August Record section of vertical-component seismograms recorded by (A) NAMASTE stations and (B) China-Nepal border stations used to read P- and S-wave arrival times. (C) Waveform inversion for the determination of a fault plane solution. Pz, vertical component of the P wave; Pr, radial component of the P wave; Sz, vertical component of the S wave; Sr, radial component of the S wave; Sh, transverse component of the S wave. (D) Total of 533 earthquakes in the Gorkha earthquake sequence we studied here, which occurred each month since April 2015. Ling Bai et al. Sci Adv 2019;5:eaav0723 Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).
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