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
"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
of Prof. Ping Tong:
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:
Ligorria, J. P., and C. J. Ammon (1999), Iterative deconvolution and receiver-function esti¬mation, Bull. Seismol. Soc. Am., 89 (5), 1395-1400.

Explaination:
sta.x   information of the stations in the format:
        name of staions, x-axis location

model1-LVZ  the synthetic data used in Figure 4b,c
model2-42km-Moho  the synthetic data used in Figure 4e
model2-35km-Moho  the synthetic data used in Figure 4f
model3-with-noise  the synthetic data used in Figure 5

in model* folders there are two subfolders named Left/ and Right/, which
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
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