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Centroid depth of earthquakes is essential for seismic hazard mitigation.But,various studies provided different solutions for the centroid depth of the damaging2013 Lushan earthquake,thus hindering further studies of the earthquake processes.To resolve its centroid depth and assess the uncertainties,we apply the teleseismic cut and paste method to invert for centroid depth with teleseismic body waves in the epicentral distance of 30°–90°.We performed the inversion for P waves only as well the case of both P and SH waves and found that both cases lead to depth solutions with difference less than 0.5 km.We also investigated the effects on depth inversion from azimuth gap of seismic stations,source duration,and corner frequency of filter.These various tests show that even azimuthal distribution of seismic stations is helpful for accurate depth inversion.It is also found that estimate of centroid depth is sensitive to source duration.Moreover,the depth is biased to larger values when corner frequency of low-pass filter is very low.The uncertainty in the velocity model can also generate some error in the depth estimation(*1.0 km).With all the above factors considered,the centroid depth of Lushan earthquake is proposed to be around 12 km,with uncertainty about 2 km.
Centroid depth of earthquakes is essential for seismic hazard mitigation. But, various studies provide different solutions for the centroid depth of the damaging 2013 Lushan earthquake, thus hindering further studies of the earthquake processes. To resolve its centroid depth and assess the uncertainties, we apply the teleseismic cut and paste method to invert for centroid depth with teleseismic body waves in the epicentral distance of 30 ° -90 ° .We performed the inversion for P waves only as well as the case of both P and SH waves and found that both cases lead to depth solutions with difference less than 0.5 km. We also investigated the effects on depth inversion from azimuth gap of seismic stations, source duration, and corner frequency of filter. These various tests show that even azimuthal distribution of seismic stations is helpful for accurate depth inversion .It also also found that estimate of centroid depth is sensitive to source duration. Moreover, the depth is biased to larger values when c orner frequency of low-pass filter is very low. The uncertainty in the velocity model can also generate some error in the depth estimation (* 1.0 km) .With all the above factors considered, the centroid depth of Lushan earthquake is proposed to be around 12 km, with uncertainty about 2 km.