首页    期刊浏览 2024年12月02日 星期一
登录注册

文章基本信息

  • 标题:Outer trench-slope faulting and the 2011 M w 9.0 off the Pacific coast of Tohoku Earthquake
  • 本地全文:下载
  • 作者:Thorne Lay ; Charles J. Ammon ; Hiroo Kanamori
  • 期刊名称:Earth, Planets and Space
  • 电子版ISSN:1880-5981
  • 出版年度:2011
  • 卷号:63
  • 期号:7
  • 页码:713-718
  • DOI:10.5047/eps.2011.05.006
  • 出版社:Springer Verlag
  • 摘要:The 11 March 2011 off the Pacific coast of Tohoku Earthquake ( M w 9.0) produced megathrust displacements of at least 40 m.The resulting tsunami devastated the Honshu coast southwest of regions struck by earthquake-generated tsunami in 1611, 1896 and 1933.The 1896 Meiji-Sanriku earthquake was also an underthrusting earthquake, but the 1933 Sanriku-oki earthquake was a trench-slope normal faulting event; both generated inundation heights of 10 to 25 m along the coast of Iwate prefecture.Possible occurrence of a great outer trench-slope earthquake seaward of the 2011 Tohoku Earthquake along a southwestward extension of the 1933 fault zone is a concern.The second largest 2011 aftershock, an outer rise M w 7.7 normal faulting earthquake occurred near the southern end of the 1933 rupture.Additional aftershock activity has been distributed along a trend below the trench and diffusely spread in the outer rise, seaward of the megathrust region where the largest slip occurred.Coulomb stress perturbations of at least 5–10 bars are calculated for outer rise normal fault geometries for mainshock slip models.Whether a future great trench slope event will occur is uncertain, but the potential tsunamigenic hazard can be gauged by the huge inundations accompanying the 1933 rupture. Key words Great normal faults tsunami 1933 Sanriku-oki outer rise earthquakes.
  • 关键词:Great normal faults ;tsunami ;1933 Sanriku-oki ;outer rise earthquakes
国家哲学社会科学文献中心版权所有