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Damage prediction of long-period structures during subduction earthquakes - Part 1: Long-period ground motion prediction in the Osaka basin for futureNankai Earthquakes -

机译:俯冲地震中长周期结构的破坏预测-第1部分:大阪盆地未来的长周期地震动预测-南开地震-

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The Nankai Trough earthquakes which are subduction earthquakes with magnitude greater than 8 have occurred at intervals of 90 to 150 years. The probability of earthquake occurrence within 30-years from January 1, 2008 are estimated at 60 70% and 50 % for the next Tonankai and Nankai earthquakes, respectively, showing very high possibility of the earthquake occurrence. It is very important to predict the long-period ground motions from the next Nankai Trough earthquakes for mitigating their disastrous effects. In this study, we show results of the prediction of future Nankai earthquake in Part 1 and the damage prediction map of high-rise buildings in the Osaka basin in Part 2. This paper (Part 1) focuses on the prediction of the long-period (>2.5s) ground motions in the Osaka basin during future Nankai earthquake using the 3D finite difference method and an earthquake scenario proposed by the Headquarters for Earthquake Research Promotion in Japan. The characteristics of the predicted long-period ground motions for the hypothetical Nankai earthquake are related with the geometry between the source and observation points, and with the thicknesses of the sediments of the basin. The duration of the long-period ground motions in an area located in the central part of the Osaka city is more than 4 minutes, and the largest peak ground velocities (PGVs) exceed 80cm/s. The predominant period is around 6 second. These results indicate the possibility of earthquake damage due to future subduction earthquakes in large-scale constructions such as tall buildings and oil storage tanks in the Osaka area.
机译:南海海槽地震是大于8级的俯冲地震,间隔90至150年。从2008年1月1日起的30年内,下一次Tonankai和Nankai地震的发生概率估计分别为60 70%和50%,这表明发生地震的可能性很高。预测下一次南开海槽地震的长周期地震动对于减轻其灾难性影响非常重要。在本研究中,我们在第1部分中展示了未来南开地震的预测结果,在第2部分中展示了大阪盆地中高层建筑的破坏预测图。本文(第1部分)着重于长期预测使用3D有限差分法和日本地震研究促进总部提出的地震方案,在未来的南开地震中,大阪盆地的地震运动(> 2.5s)。假设的南开地震预测的长周期地震动的特征与震源和观测点之间的几何形状以及盆地沉积物的厚度有关。位于大阪市中部地区的长时间地面运动持续时间超过4分钟,最大峰值地面速度(PGV)超过80cm / s。主要时间约为6秒。这些结果表明,在大阪地区高层建筑和储油罐等大型建筑中,未来的俯冲地震可能会造成地震破坏。

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