We presented attenuation characteristics of S waves in the crust of Ordos massif. Using 487 pieces of digital oscil- lograms of 19 seismic events recorded by 32 seismologic stations located on Ordos massif and its sur...We presented attenuation characteristics of S waves in the crust of Ordos massif. Using 487 pieces of digital oscil- lograms of 19 seismic events recorded by 32 seismologic stations located on Ordos massif and its surroundings, we have calculated the parameter of three-segment geometric attenuation and give the relation of inelastic attenuation Q value with frequency in the crust of Ordos massif, site responses of 32 stations, and source parameters of 19 events by the genetic algorithm. The results indicate that Q value (at 1 Hz) of S-wave in the crust of Ordos massif is much larger than that in the geologically active tectonic region. The site responses of the 32 stations in the high-frequency section do not show clear amplification effect except one or two stations, while in the low-frequency section, there is difference among the stations. The logarithmic value of seismic moment and the magnitude ML of 19 seismic events has a very good linear relationship.展开更多
基金National Scientific Research Target Project of China (2004BA601B01-04-03) during the tenth Five-year Plan, Joint Seismological Science Foundation of China (104047) and the Application Lab of Digital Seismic Wave Data in Center for Analysis and Prediction.
文摘We presented attenuation characteristics of S waves in the crust of Ordos massif. Using 487 pieces of digital oscil- lograms of 19 seismic events recorded by 32 seismologic stations located on Ordos massif and its surroundings, we have calculated the parameter of three-segment geometric attenuation and give the relation of inelastic attenuation Q value with frequency in the crust of Ordos massif, site responses of 32 stations, and source parameters of 19 events by the genetic algorithm. The results indicate that Q value (at 1 Hz) of S-wave in the crust of Ordos massif is much larger than that in the geologically active tectonic region. The site responses of the 32 stations in the high-frequency section do not show clear amplification effect except one or two stations, while in the low-frequency section, there is difference among the stations. The logarithmic value of seismic moment and the magnitude ML of 19 seismic events has a very good linear relationship.
