This is a reference P- and S-wave velocity model of the crust and uppermost mantle in the southwest China, obtained by joint body and surface wave tomography (doi: http://www.cses.ac.cn/?p=3747).
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Model Data Format: Lon Lat Dep(km) Vp(km/s) Vs(km/s)
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Method: Joint inversion of body wave (P and S-wave) travel time and Rayleigh wave dispersion data (Fang et al., (2016), JGR).
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Grid space: Horizontally 0.5 degree interval, vetically at depth 0, 5, 10, 15, 20, 25, 30, 35, 40, 50, 60, 70 km.
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Depth is relative to the surface (0 km).
If you have any questions, please feel free to contact Huajian Yao ([email protected]) or Ying Liu ([email protected]).