Source model of the 2007 Noto-Hanto earthquake (M w 6.7) for estimating broad-band strong ground motion
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  • 作者:Susumu Kurahashi ; Kazuaki Masaki ; Kojiro Irikura
  • 关键词:Broad ; band strong ground motion ; empirical Green’s function method ; 2007 Noto ; Hanto earthquake ; selection of aftershock records as EGF ; source model
  • 刊名:Earth, Planets and Space
  • 出版年:2008
  • 出版时间:February 2008
  • 年:2008
  • 卷:60
  • 期:2
  • 页码:89-94
  • 全文大小:765KB
  • 参考文献:Aoi, S. and H. Sekiguchi, Rupture process of the 2007 Noto-Hanto earthquake obtained from strong motion data, http://?www.?k-net.?bosai.?go.?jp/?k-net/?topics/?noto070325/-/span> , 2007 (in Japanese).
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  • 作者单位:Susumu Kurahashi (12)
    Kazuaki Masaki (22)
    Kojiro Irikura (32)

    12. Graduate School of Engineering, Aichi Institute of Technology, Japan
    22. Faculty of Engineering, Aichi Institute of Technology, Japan
    32. Disaster Prevention Research Center, Aichi Institute of Technology, Japan
  • 刊物类别:Earth Sciences, general; Geology; Geophysics/Geodesy;
  • 刊物主题:Earth Sciences, general; Geology; Geophysics/Geodesy;
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1880-5981
文摘
A source model for estimating broad-band ground motions from the 2007 Noto-Hanto earthquake (M w 6.7) is estimated from a comparison of the observed records of the mainshock and synthesized motions based on the characterized asperity model using the empirical Green’s function method. The observed records of aftershocks used as the empirical Green’s functions are carefully selected to have almost the same radiation characteristics and source distance as the asperities of the mainshock. The best-fit source model consists of two asperities of different size. A large one is located just above the hypocenter, with an area of 6.3×6.3 km2 and stress drop of about 26 MPa. A smaller one is located north-east of the large one, with an area of 3.6×3.6 km2 and stress drop of about 10 MPa. The stress drop of the large one is about twofold higher than the average values of inland crustal earthquakes so far estimated, while that of smaller one is almost average. We found that the remarkable directivity pulses from the source model struck the northern part of the Noto peninsula, causing heavy damage in some towns there. Key words Broad-band strong ground motion empirical Green’s function method 2007 Noto-Hanto earthquake selection of aftershock records as EGF source model

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