Electronic Supplement to
The 14 November, 2001 Kokoxili (Kunlunshan), Tibet, earthquake: Rupture transfer through a large extensional step-over

by M. Antolik, R. E. Abercrombie, and G. Ekström

 

Waveform fits to teleseismic body waves

These three figures show the observed and synthetic waveforms obtained from the point-source inversions for teleseismic P and SH waveforms at all of the stations used in the analysis. Pulse A, discussed in the text, is prominent on the P-wave records within the first 20 s at all stations to the west and southwest from the source. This pulse has negligible amplitude at stations to the northeast which indicates a change in focal mechanism during the earthquake rupture. While the main portion of the P waves and the SH waveforms can be adequately fit using a model with fewer sources [Figure 1 and Figure 2], only the 3-subevent model [Figure 3], which includes an oblique normal-faulting subevent within the first 20 s, can fit Pulse A at stations where it contains significant energy.


Figures

Figure 1. P and SH observed waveforms and synthetics for the single-source model. Synthetics are dashed. All the records used in the analysis are shown. Symbols are similar to Figures 3, 5, and 6 of the text. Vertical lines denote beginning and end of the time window used, and arrows indicate the picked onset time for each station. The numbers above each station identifier indicate the maximum amplitude of each trace in microns. Pulses A and B, as discussed in the text, are marked on the bottom two P wave records
 

Figure 2. P and SH observed waveforms and synthetics for the two-subevent model. The focal mechanisms and source time function shown are for the first subevent only (this focal mechanism was fixed as discussed in the text). Other symbols are the same as in Figure 1.
 

Figure 3. P and SH observed waveforms and synthetics for the three-subevent model. The focal mechanisms and source time function shown are for the second (oblique) subevent only. Other symbols are the same as in Figure E1.
 


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