Lateral Variations in Upper Mantle Discontinuities beneath Northeast China Revealed by Seismic Ambient Noise

Data description:

CCdata.zip:

Re-sampling Cross-Correlation functions (4Hz) which contain three seismic arrays.

CEA contains HL, JL, LN and NM networks. 

NECESSarray contains YP network. NECsaids contains DB network. 

All the stations are located east of 122E, between 41N and 46N. 

The cross-correlations are used to retrieved body-wave reflections from mantle transition zone discontinuities.

Syntheticdata.zip:

contains two parts: 1Dtests and 2D tests

1Dtets: 

synthetic waveforms calculated by Qseis (Wang, 1999) after data-processings.

H is increased from 0 to 30 km. 

The distance is 100 km.  

2Dtests: 

raw synthetic waveforms calculated by SPECFEM2D (Tromp et al., 2008).

Three models with depressed d660 (model 1-3) and with a slab on the d660 (model 4).  

100 receiver stations (surface), from 305 km to 1295 km in 10 km increments.

49 vertical single-force sources (surface), from 320 km to 1280 km in 20 km increments 

NECsaidsDescription.docx:

Detailed description about the NECsaids project conducted in northeast China from October, 2010 to September, 2017.

station_loc.txt:

Coordinate file (station, longitude, latitude) of the stations.

Reference

Wang, R. (1999). A simple orthonormalization method for stable and efficient computation of Green's functions. Bulletin of the Seismological Society of America, 89(3), 733-741. doi: 10.1785/BSSA0890030733

Tromp, J., Komatitsch, D. and Liu, Q. Y. (2008). Spectral-element and adjoint methods in seismology. Commun Comput Phys 3, 1-32.