The prediction of seismic amplification effect in three-dimensional sedimentary basins and its application

Zhenning Ba, Shaocong Mu, Jingxuan Zhao, Yushan Zhang, Sanhong Chen
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Abstract

Numerous studies have shown that the basin amplification effect is influenced by characteristic parameters such as basin geometry and media impedance contrast, but quantitative analysis of the effect for three-dimensional (3D) basins is still rare. In this paper, the basin amplification effect is quantified through an aggravation factor (AGF ), which is defined as the ratio between 3D and 1D acceleration response spectra along the basin surface. Considering the 3D geometry of the actual basin, we investigate the sensitivity of aggravation factors to inclination angles, shape ratios, and impedance contrasts by establishing 78 3D trapezoidal sedimentary basin models with different characteristic parameters. Furthermore, we perform a statistical analysis of the aggravation factors and propose their prediction formulas, which are applied to the Euroseistest basin and the Shidian basin. The above analysis reveals that: (1) The effects of inclination angle and shape ratio on the aggravation factor are concentrated in the edge part and central part of the basin, respectively, while the impedance contrast has less influence on the aggravation factor along the basin surface; (2) From the prediction results for the Euroseistest basin, the aggravation factor of the 3D model is higher than that of the 2D model with a maximum error of 22%, while the distribution pattern of the aggravation factor along the surface is similar; and (3) The predicted results for the Shidian basin show that the basin with a small inclination angle has a larger aggravation factor in the edge part and even exceeds the central part; for example, the highest aggravation factor is 2.155 in the edge part of the basin with an inclination angle of 6°.
三维沉积盆地地震放大效应预测及其应用
大量研究表明,盆地放大效应受盆地几何形状和介质阻抗对比等特征参数的影响,但对三维盆地效应的定量分析尚不多见。本文通过加重因子(AGF)来量化流域的放大效应,加重因子定义为沿流域表面的三维与一维加速度响应谱之比。结合实际盆地的三维几何特征,建立了78个具有不同特征参数的三维梯形沉积盆地模型,研究了加重因子对倾角、形状比和阻抗对比的敏感性。在此基础上,对其加重因子进行了统计分析,提出了加重因子的预测公式,并将其应用于塔里木盆地和石甸盆地。上述分析表明:(1)倾角和形状比对加重因子的影响分别集中在盆地边缘和中部,而沿盆地表面的阻抗对比对加重因子的影响较小;(2)从欧洲地震盆地的预测结果来看,三维模型的加重因子高于二维模型,最大误差为22%,而加重因子沿地表的分布格局相似;③石甸盆地的预测结果表明,倾角小的盆地边缘加重因子较大,甚至超过中部;例如,当倾角为6°时,盆地边缘部分的加重系数最高,为2.155。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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