郝宪生, 彭一民, 王志良. 1985: 北京市区埋藏基岩凹陷地形对地震动的影响. 地震学报, 7(3): 326-336.
引用本文: 郝宪生, 彭一民, 王志良. 1985: 北京市区埋藏基岩凹陷地形对地震动的影响. 地震学报, 7(3): 326-336.
HAO XIANSHENG, PENG YIMIN, WANG ZHILIANGcom sh advanc. 1985: EFFECTS OF THE DEPRESSION IN THE TOPOGRAPHY OF BEDROCK UNDERLYING BEIJING ON EARTHQUAKE GROUND MOTION. Acta Seismologica Sinica, 7(3): 326-336.
Citation: HAO XIANSHENG, PENG YIMIN, WANG ZHILIANGcom sh advanc. 1985: EFFECTS OF THE DEPRESSION IN THE TOPOGRAPHY OF BEDROCK UNDERLYING BEIJING ON EARTHQUAKE GROUND MOTION. Acta Seismologica Sinica, 7(3): 326-336.

北京市区埋藏基岩凹陷地形对地震动的影响

EFFECTS OF THE DEPRESSION IN THE TOPOGRAPHY OF BEDROCK UNDERLYING BEIJING ON EARTHQUAKE GROUND MOTION

  • 摘要: 北京市区沿三里河——西四——德胜门有一条地震高烈度异常带,其产生异常的原因众说不一。目前北京地区仍存在中等强度地震的波及与威胁,同时该区高层建筑正在日新月异的发展,因而探明这条高烈度异常的成因看来是很必要的。本文回顾了有关场地工程地质条件对地震动的影响的研究进展,详细分析了该区的工程地质和基岩构造情况,利用经作者扩展的SAP 5程序计算了典型剖面的地震反应。结果表明深度在1000——1500米的基岩凹陷对这一高烈度异常似有着控制性的影响。由于地面振动的卓越周期在1.0秒左右,将对该区的长周期结构(如高层建筑和烟囱等)带来不利影响。

     

    Abstract: There is a belt of abnormally high seismic intensity along the line of Sanlihe-Xisi-Deshengmen in Beijing city during the Tangshan earthquake. Various hypothesis as to the cause of this abnormal belt have been suggested.Because the earthquake risk of Beijing city is not negligble and more and more highrise buildings are being erected,it might be necessary to find out the cause resulting in this belt of high seismic risk.Through detailed researches on a typical geological profile and its earthquake response by using the extended SAP 5 program,the following main results are obtained:1.It is found that a depression of the underlying bedrock to a depth of 1000-1500 meters plays a dominant role in causing the belt of abnoralty intense earthquake damage in Beijing.2.The calculated predominant periods of the response spectra at different sites above the depression are from 0.85-0.95 see.These conclusions are likely to be helpful to the earthquake-resistant design of high-rise builings in the urban area of Beijing or other similar zones.

     

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