Synthetic sensitivity analysis of high frequency radiation of 2011 Tohoku-Oki (M W 9.0) earthquake
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  • 作者:Haoran Meng (1)
    Yongshun John Chen (1)
  • 关键词:Tohoku ; Oki earthquake ; High frequency radiation ; Frequency ; dependent rupture behavior
  • 刊名:Earthquake Science
  • 出版年:2014
  • 出版时间:August 2014
  • 年:2014
  • 卷:27
  • 期:4
  • 页码:355-364
  • 全文大小:1,925 KB
  • 参考文献:1. Hong (2010) Lg attenuation in a region with both continental and oceanic environments. Bull Seismol Soc Am. doi:10.1785/0120090057
    2. Huang Y, Meng L, Ampuero J-P (2012) A dynamic model of the frequency-dependent rupture process of the 2011 Tohoku-Oki earthquake. Earth Planets Space. doi:10.5047/eps.2012.05.011
    3. Ide S, Baltay A, Beroza GC (2011) Shallow dynamic overshoot and energetic deep rupture in the 2011 / M W9.0 Tohoku-Oki Earthquake. science. doi:10.1126/science.1207020
    4. Ishii M (2011) High-frequency rupture properties of the / M W9.0 off the Pacific coast of Tohoku Earthquake. Earth Planets Space. doi:10.5047/eps.2011.07.009
    5. Iwakiri K, Hoshiba M (2012) High-frequency (>10?Hz) content of the initial fifty seconds of waveforms from the 2011 Off the Pacific Coast of Tohoku Earthquake. Bull Seismol Soc Am. doi:10.1785/0120110241
    6. Kiser E, Ishii M (2011) The 2010 / M W 8.8 Chile earthquake: triggering on multiple segments and frequency-dependent rupture behavior. Geophys Res Lett. doi:10.1029/2011GL047140
    7. Koper KD, Hutko AR, Lay T (2011a) Along-dip region variation of teleseismic short-period radiation from the 11 March 2011 Tohoku earthquake ( / M W9.0). Geophys Res Lett. doi:10.1029/2011GL049689
    8. Koper KD, Hutko AR, Lay T, Ammon CJ, Kanamori H (2011b) Frequency-dependent rupture process of the 2011 / M W9.0 Tohoku Earthquake: comparison of short-period P wave backprojection images and broadband seismic rupture models. Earth Planets Space. doi:10.5047/eps.2011.05.026
    9. Lay T, Kanamori H, Ammon CJ, Koper KD, Hutko AR, Ye L, Yue H, Rushing TM (2012) Depth-varying rupture properties of subduction zone megathrust faults. J Geophys Res. doi:10.1029/2011JB009133
    10. Meng L, Ampuero JP, Luo Y, Wu W, Ni S (2012) Mitigating artifacts in back-projection source imaging with implications on frequency-dependent properties of the Tohoku-Oki Earthquake. Earth Planets Space. doi:10.5047/eps.2012.05.010
    11. Romanowicz B, Mitchell BJ (2007) Deep earth structure-Q of the Earth from crust to core. Elsevier B.V, Amsterdam
    12. Sato H, Fehler M, Maeda T (2013) Seismic wave propagation and scattering in the heterogeneous earth: second edition. Springer Press, New York
    13. Wang D, Mori J (2011) Frequency-dependent energy radiation and fault coupling for the 2010 / M W8.8 Maule, Chile, and 2011 / M W9.0 Tohoku, Japan, earthquakes. Geophys Res Lett. doi:10.1029/2011GL049652
    14. Yao H, Gerstoft P, Shearer PM, Mecklenbr?uker C (2011) Compressive sensing of the Tohoku-Oki / M W 9.0 earthquake: frequency-dependent rupture modes. Geophys Res Lett. doi:10.1029/2011GL049223
    15. Ye L, Lay Thorne, Kanamori Hiroo (2013) Ground shaking and seismic source spectra for large earthquakes around the megathrust fault offshore of northeastern Honshu, Japan. Bull Seismol Soc Am. doi:10.1785/0120120115
    16. Yue H, Lay T (2013) Source rupture models for the / M W9.0 2013 Tohoku Earthquake from joint inversions of high-rate geodetic and seismic data. Bull Seismol Soc Am. doi:10.1785/0120120119
  • 作者单位:Haoran Meng (1)
    Yongshun John Chen (1)

    1. Institute of Theoretical and Applied Geophysics, School of Earth and Space Sciences, Peking University, Beijing, 100871, China
  • ISSN:1867-8777
文摘
Frequency-dependent rupture behavior of subduction zone interplate megathrust faults has been observed by back-projection method in different frequency bands (from 0.05 to 5?Hz). It has been suggested that the down-dip region of the Tohoku megathrust radiated strongly at high frequencies (>10?Hz) compared with that of the up-dip region. By assuming the same source time function of each fault patch, we perform a synthetic sensitivity analysis to compare the energy received from the shallower parts (and further way from the receiver sites) with that from the deeper parts (and closer to the receiver sites) of the rupture. Our results indicate that regional on-shore recordings are probably not adequate to constrain the presence of far-off shore high frequency radiations because of the strong attenuation of this region.

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