地震学
力矩震级标度
峰值地面加速度
地震灾害
地质学
光谱加速度
最大震级
自然灾害
地震小区分带
加速度
地震震级
地震力矩
危害
断层(地质)
麦卡利强度标度
线性构造
地震情景
大地测量学
环境地震烈度表
危害分析
城市地震危险性
地质灾害
诱发地震
增量动力分析
震级(天文学)
地震动
构造学
几何学
数学
物理
经典力学
天文
缩放比例
作者
T. G. Sitharam,P. Anbazhagan
出处
期刊:Natural Hazards
[Springer Nature]
日期:2006-10-17
卷期号:40 (2): 261-278
被引量:97
标识
DOI:10.1007/s11069-006-0012-z
摘要
Indian peninsular shield, which was once considered to be seismically stable, is experiencing many earthquakes recently. As part of the national level microzonation programme, Department of Science and Technology, Govt. of India has initiated microzonation of greater Bangalore region. The seismic hazard analysis of Bangalore region is carried out as part of this project. The paper presents the determination of maximum credible earthquake (MCE) and generation of synthetic acceleration time history plot for the Bangalore region. MCE has been determined by considering the regional seismotectonic activity in about 350 km radius around Bangalore city. The seismotectonic map has been prepared by considering the faults, lineaments, shear zones in the area and historic earthquake events of more than 150 events. Shortest distance from the Bangalore to the different sources is measured and then peak ground acceleration (PGA) is calculated for the different source and moment magnitude. Maximum credible earthquake found in terms of moment magnitude is 5.1 with PGA value of 0.146 g at city centre with assuming the hypo central distance of 15.88 km from the focal point. Also, correlations for the fault length with historic earthquake in terms of moment magnitude, yields (taking the rupture fault length as 5% of the total fault length) a PGA value of 0.159 g. Acceleration time history (ground motion) and a response acceleration spectrum for the corresponding magnitude has been generated using synthetic earthquake model considering the regional seismotectonic parameters. The maximum spectral acceleration obtained is 0.332 g for predominant period of 0.06 s. The PGA value and synthetic earthquake ground motion data from the identified vulnerable source using seismotectonic map will be useful for the PGA mapping and microzonation of the area.
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