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Geometric effects resulting from the asym-metry of dipping fault: Hanging wall/foot-wall effects

机译:由倾角不对称引起的几何效应:悬壁/底壁效应

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摘要

Root-mean-square distance Drms with characteristic of weighted-average is introduced in this article firstly. Drms can be used to capture the general proximity of a site to a dipping fault plane comparing with the rupture distance Drup and the seismogenic distance Dseis. Then, using Drup Dseis and Drms, the hanging wall/footwall effects on the peak ground acceleration (PGA) during the 1999 Chi-Chi earthquake are evaluated by regression analysis. The logarithm residual shows that the PGA on hanging wall is much greater than that on footwall at the same Drup or Dseis when the Drup or Dseis is used as site-to-source distance measure. In contrast, there is no significant difference between the PGA on hanging wall and that on footwall at the same Drms when Drms is used. This result confirms that the hanging wall/footwall effect is mainly a geometric effect caused by the asymmetry of dipping fault. Therefore, the hanging wall/footwall effect on the near-fault ground motions can be ignored in the future attenuation analysis if the root-mean-square distance Drms is used as the site-to-source distance measure.
机译:本文首先介绍具有加权平均特征的均方根距离Drms。与破裂距离Drup和震源距离Dseis相比,Drms可用于捕获站点到倾覆断层平面的大致距离。然后,通过回归分析,使用Drup Dseis和Drms对1999年集集地震期间的悬壁/底壁对峰值地面加速度(PGA)的影响进行评估。对数残差表明,当将Drup或Dseis用作站点到源距离的度量标准时,在同一Drup或Dseis处,吊壁上的PGA远大于下盘壁上的PGA。相比之下,使用Drms时,在相同Drms的吊壁上的PGA和在下墙的PGA之间没有显着差异。该结果证实,悬壁/底壁效应主要是由倾角不对称引起的几何效应。因此,如果将均方根距离Drms用作站点到源的距离度量,则在将来的衰减分析中可以忽略近断层地震动对悬挂壁/底壁的影响。

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