《Table 1.Apparent velocities and phases in the record of OBS09》

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《Crustal S-wave velocity structure across the northeastern South China Sea continental margin: implications for lithology and mantle exhumation》

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A statistical measure of fit in chi-squared（χ2）close to one is used to evaluate the mismatch between observed and calculated travel times（Zelt and Smith，1992）.After the S-wave modeling，the fitting RMS errors are less than 200 ms andχ2 are less than 2for most of the S-wave phases（Table 2）.The ray coverage map（Figure 7c）of all observed arrival locations further shows that the crust and most interfaces are well covered by 10–40 times，indicating high reliability and resolution of our S-wave model.