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首页> 外文期刊>Engineering Geology >Modeling of SH- and P-SV-wave fields and seismic microzonation based on response spectra for Talchir Basin, India
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Modeling of SH- and P-SV-wave fields and seismic microzonation based on response spectra for Talchir Basin, India

机译:印度塔尔基尔盆地基于响应谱的SH和P-SV波场建模和地震微区划

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摘要

The P-SV- and SH-wave field in the Talchir Basin is simulated along eight profiles: four profiles strike across the basin and the other four along the basin. The hybrid method, which combines two computational techniques, modal summation and finite differences, is used to produce multiphase synthetic seismograms. An M=6 earthquake is considered, with hypocenter along the North Orissa Boundary Fault (NOBF) at a depth of 5 km and with the focal mechanism parameters: dip=90 deg, strike=160 deg and rake=180 deg. The peak acceleration (A_(MAX)) along each profile is determined considering the maximum acceleration obtained at the horizontal components. The response spectra ratio (RSR) as a function of frequency is computed for the eight profiles and the higher amplification is seen to increase in correspondence with the thicker sedimentary cover, especially for the radial component. Higher site amplification for all the profiles is observed in the frequency range from 0.5 to 1.4 Hz. To validate the obtained site-effects, the sources, for the profiles across the basin, are placed near to the southern end of the profile and the site amplifications are recomputed. Even if the spatial distribution of A_(MAX) is mainly controlled by the epicentral distance, i.e. the geometrical spreading prevails on local soil effects, the RSR shows a pattern that can be easily correlated with the local site conditions. The RSR at the intersection of the profiles is dependent not only upon the local lithology and sediment thickness but also upon the epicentral distance. The Talchir Basin is classified into three zones based on the RSR values: low RSR zone (1.6-1.9), intermediate RSR zone (2.0-2.8) and high RSR zone (2.9-5.2). The PGA estimated for the bedrock model by Bhatia et al. (1999) for the study region is around 0.05 to 0.10 g while the Indian seismic zonation map estimated it to be in the range from 0.1 to 0.2 g. In the present study, that considers the effects of lateral variations in the structure, the PGA is estimated to be as high as 0.55 g along the BA profile.
机译:塔尔基尔盆地的P-SV波和SH波场沿八个剖面进行了模拟:四个剖面跨越该盆地,其余四个沿该盆地。混合方法结合了模态求和和有限差分这两种计算技术,用于生成多相合成地震图。考虑了M = 6地震,震源位于北奥里萨邦边界断裂(NOBF),深度为5 km,震源机制参数为:倾角= 90度,走向= 160度,倾角= 180度。考虑到在水平分量处获得的最大加速度,确定沿每个轮廓的峰值加速度(A_(MAX))。计算了八个剖面的响应频谱比率(RSR)与频率的关系,并且观察到较高的放大倍数与较厚的沉积物覆盖层相对应,特别是对于径向分量而言。在0.5到1.4 Hz的频率范围内,观察到了所有轮廓的较高位点放大。为了验证所获得的场地效果,整个盆地剖面的源头都放在剖面的南端附近,并重新计算场地放大倍数。即使A_(MAX)的空间分布主要受震中距离控制,即几何扩展在局部土壤效应中占主导地位,RSR仍显示出易于与局部场地条件相关的模式。剖面相交处的RSR不仅取决于局部岩性和沉积物厚度,还取决于震中距离。塔尔基尔盆地根据RSR值分为三个区域:低RSR区(1.6-1.9),中RSR区(2.0-2.8)和高RSR区(2.9-5.2)。 Bhatia等人估计基岩模型的PGA。 (1999年)的研究区域约为0.05至0.10克,而印度地震区带图估计它的范围为0.1至0.2克。在本研究中,考虑到结构中横向变化的影响,沿BA轮廓估计PGA高达0.55 g。

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