2011年东日本大地震:位移延伸至海沟轴

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英文篇名：The 2011 Tohoku-Oki earthquake:Displacement reaching the Trench axis 中文刊名：国际地震动态 英文刊名：Recent Developments in World Seismology 作者：Toshiya Fujiwara ; Shuichi Kodaira ; Tetsuo No ; Yuka Kaiho ; Narumi Takahashi ; Yoshiyuki Kaneda ; 左玉玲 出版日期：2012-01-25 机构：Institute for Research on Earth Evolution,Japan Agency for Marine-Earth Science and Technology,Natsushima-cho 2-15,Yokosuka 237-0061,Japan;IFREE,JAMSTEC,Showa-machi 3173-25,Kanazawa-ku,Yokohama 236-0001,Japan;Earthquake and Tsunami Research Project for Disaster Prevention,JAMSTEC,Showa-machi 3173-25,Kanazawa-ku,Yokohama 236-0001,Japan;中国地震局地球物理研究所; 年：2012 期：01 出版单位：国际地震动态

摘要

<正>2011年3月11日日本地震(MW9.0)后发生的大海啸被认为是由延伸至日本海沟处一条俯冲带浅部的断层破裂所致。这是不同的地震和大地测量反演程序所揭示的结果[1-2];然而,精确的同震位移逆倾斜向上极限值仍然没有被明确界定。在此,我们介绍

引文

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    [5]Material and methods are available as supporting material on Science Online.
    [6]Sato M,Ishikawa T,Ujihara N,et al.Displacement above the hypocenter of the 2011Tohoku-Oki earth-quake.Science,2011,332(6036):1 395
    [7]Ito Y,Tsuji T,Osada Y,et al.Frontal wedge deformation near the source region of the 2011Tohoku-Okiearthquake.Geophys.Res.Lett.,2011,38:L00G05,5PP.doi:10.1029/2011GL048355