synthetic receiver function waveforms for manuscript "Depth extent and V_p/V_s ratio of the Chenghai fault zone, Yunnan, China constrained from dense-array-based teleseismic receiver functions"

This is the synthetic data used in our submitted manuscript entitled<br> "Depth extent and V_p/V_s ratio of the Chenghai fault zone, Yunnan, China constrained from dense-array-based teleseismic receiver functions" These synthetic seismograms are calculated using the SEM-FK code<br> of Prof. Ping Tong:<br> Tong, P., C. Chen, and D. Komatitsch (2014), High-resolution seismic array imaging based on an SEM-FK hybrid method, Geophys. J. Int., 197(1), 369-395. The receiver function waveforms are calcuated using the iterative deconvolution method:<br> Ligorria, J. P., and C. J. Ammon (1999), Iterative deconvolution and receiver-function esti¬mation, Bull. Seismol. Soc. Am., 89 (5), 1395-1400. Explaination:<br> sta.x information of the stations in the format:<br> name of staions, x-axis location model1-LVZ the synthetic data used in Figure 4b,c<br> model2-42km-Moho the synthetic data used in Figure 4e<br> model2-35km-Moho the synthetic data used in Figure 4f<br> model3-with-noise the synthetic data used in Figure 5 in model* folders there are two subfolders named Left/ and Right/, which<br> means the incident planar wave is from left and right direction, respectively. The receiver function waveforms are named as ${station_name}.ri in SAC format<br> ~