4.6 Article

Modelling of wave propagation and attenuation in the Osaka sedimentary basin, western Japan, during the 2013 Awaji Island earthquake

期刊

GEOPHYSICAL JOURNAL INTERNATIONAL
卷 204, 期 3, 页码 1678-1694

出版社

OXFORD UNIV PRESS
DOI: 10.1093/gji/ggv543

关键词

Earthquake ground motions; Seismic attenuation; Site effects; Computational seismology; Wave propagation

资金

  1. Earthquake and Volcano Hazards Observation and Research Program of MEXT
  2. Japan Society for the Promotion of Science (JSPS) [23310121, 25750146]
  3. Grants-in-Aid for Scientific Research [25750146, 23310121] Funding Source: KAKEN

向作者/读者索取更多资源

On 2013 April 13, an inland earthquake of M-w 5.8 occurred in Awaji Island, which forms the western boundary of the Osaka sedimentary basin in western Japan. The strong ground motion data were collected from more than 100 stations within the basin and it was found that in the Osaka Plain, the pseudo velocity response spectra at a period of around 6.5 s were significantly larger than at other stations of similar epicentral distance outside the basin. The ground motion lasted longer than 3 min in the Osaka Plain where its bedrock depth spatially varies from approximately 1 to 2 km. We modelled long-period (higher than 2 s) ground motions excited by this earthquake, using the finite difference method assuming a point source, to validate the present velocity structure model and to obtain better constraint of the attenuation factor of the sedimentary part of the basin. The effect of attenuation in the simulation was included in the form of Q(f) = Q(0)(f/f(0)), where Q(0) at a reference frequency f(0) was given by a function of the S-wave velocity, Q(0) = alpha V-S. We searched for appropriate Q(0) values by changing alpha for a fixed value of f(0) = 0.2 Hz. It was found that values of alpha from 0.2 to 0.5 fitted the observations reasonably well, but that the value of alpha = 0.3 performed best. Good agreement between the observed and simulated velocity waveforms was obtained for most stations within the Osaka Basin in terms of both amplitude and ground motion duration. However, underestimation of the pseudo velocity response spectra in the period range of 5-7 s was recognized in the central part of the Osaka Plain, which was caused by the inadequate modelling of later phases or wave packets in this period range observed approximately 2 min after the direct S-wave arrival. We analysed this observed later phase and concluded that it was a Love wave originating from the direction of the east coast of Awaji Island.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.6
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据