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A scenario of ground shaking hazard in intracratonic circular basins developed by basin-generated surface waves: an earthquake engineering perspective

机译:盆地引起的表面波开发的跨辐射圆形盆地的地面震动场景:地震工程视角

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摘要

This paper presents the comparative scenario of ground motion amplifications in the 2D semi-cylindrical (SC) basin and 3D semi-spherical (SS) intracratonic basin caused by the basin-generated surface (BGS) waves and the associated spatial variations of average spectral amplification, differential ground motion (DGM) and average aggravation factor (AAF). The time-domain seismic responses of both the basins were computed using a recently developed 3D fourth-order accurate viscoelastic finite-difference algorithm based on the well-known GMB-EK rheological model. The analysis of simulated results revealed that AAF and DGM are comparable near the basin-edge in both the basins but the differences are increasing towards the centre of basins due to the focusing of the BGS-waves in the SS-basin. The obtained many-fold increase of 1D/2D-AAFs and DGM at the centre of the SS-basin as compared to the SC-basin reflects the inadequacy of 1D or 2D response of an intracratonic circular basin for the seismic hazard assessment. It may be inferred that the level of damage near the edges of the 2D and 3D circular basins may be comparable but unexpected damage may occur in the central part of a circular basin due to the focusing of the BGS-waves.
机译:本文介绍了由盆地产生的表面(BGS)波引起的2D半圆柱(SC)盆地和3D半球形(SS)腹腔盆地的地面运动放大的比较情况及平均光谱放大的相关空间变化,差分地面运动(DGM)和平均恶化因子(AAF)。基于众所周知的Gmb-ek流变模型,使用最近开发的3D四阶精确粘弹性有限差分算法计算了两种盆地的时域地震响应。模拟结果的分析表明,AAF和DGM在盆地中的盆边缘附近相当,但由于SS-盆中的BGS波的聚焦,差异朝向盆地的中心增加。与SC-盆液相比,在SS-盆地的中心获得的1D / 2D-AAF和DGM的多倍增加,反映了跨辐射圆形盆地对地震危害评估的1D或2D响应的不足。可以推断,2D和3D圆形盆地的边缘附近的损坏水平可以是可比的,但由于BGS波的聚焦,圆形盆地的中心部分可能发生意外损坏。

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