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Probabilistic Seismic Hazard Assessment for Northeast India Region

机译:印度东北地区的概率地震危险性评估

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摘要

Northeast India bounded by latitudes 20A degrees-30A degrees N and longitudes 87A degrees-98A degrees E is one of the most seismically active areas in the world. This region has experienced several moderate-to-large-sized earthquakes, including the 12 June, 1897 Shillong earthquake (M (w) 8.1) and the 15 August, 1950 Assam earthquake (M (w) 8.7) which caused loss of human lives and significant damages to buildings highlighting the importance of seismic hazard assessment for the region. Probabilistic seismic hazard assessment of the region has been carried out using a unified moment magnitude catalog prepared by an improved General Orthogonal Regression methodology (Geophys J Int, 190:1091-1096, 2012; Probabilistic seismic hazard assessment of Northeast India region, Ph.D. Thesis, Department of Earthquake Engineering, IIT Roorkee, Roorkee, 2013) with events compiled from various databases (ISC, NEIC,GCMT, IMD) and other available catalogs. The study area has been subdivided into nine seismogenic source zones to account for local variation in tectonics and seismicity characteristics. The seismicity parameters are estimated for each of these source zones, which are input variables into seismic hazard estimation of a region. The seismic hazard analysis of the study region has been performed by dividing the area into grids of size 0.1A degrees x 0.1A degrees. Peak ground acceleration (PGA) and spectral acceleration (S (a)) values (for periods of 0.2 and 1 s) have been evaluated at bedrock level corresponding to probability of exceedance (PE) of 50, 20, 10, 2 and 0.5 % in 50 years. These exceedance values correspond to return periods of 100, 225, 475, 2475, and 10,000 years, respectively. The seismic hazard maps have been prepared at the bedrock level, and it is observed that the seismic hazard estimates show a significant local variation in contrast to the uniform hazard value suggested by the Indian standard seismic code [Indian standard, criteria for earthquake-resistant design of structures, fifth edition, Part-I. Bureau of Indian Standards, New Delhi, 2002]. Not only holistic treatment of earthquake catalog and seismogenic zones has been performed, but also higher resolution in spatial distribution could be achieved. The COV maps have been provided with the strong ground-motion maps under various conditions to show the confidence in the results obtained. Results obtained in the present study would be helpful for risk assessment and other disaster mitigation-related studies.
机译:印度东北部是北纬20A度至30A度,东经87A度至98A度,是世界上地震活动最活跃的地区之一。该地区经历了几次中到大地震,包括1897年6月12日西隆地震(M(w)8.1)和1950年8月15日阿萨姆邦地震(M(w)8.7),这些地震造成了人员伤亡对建筑物的重大破坏凸显了该地区地震危险性评估的重要性。该地区的概率地震危险性评估使用统一的矩震级目录进行,该目录由改进的通用正交回归方法编制(Geophys J Int,190:1091-1096,2012;印度东北地区的概率性地震危险性评估,博士学位) 。IIT Roorkee地震工程系论文,Roorkee,2013年),并从各种数据库(ISC,NEIC,GCMT,IMD)和其他可用目录中汇编了事件。研究区域已细分为9个震源区,以说明构造和地震活动特征的局部变化。针对这些震源区中的每个震源区估计地震活动性参数,这些参数是区域地震危险性估计中的输入变量。通过将区域划分为大小为0.1A度x 0.1A度的网格,可以对研究区域进行地震危险性分析。在基岩水平上已评估了地面加速度峰值(PGA)和频谱加速度(S(a))值(0.2和1 s的时间),对应于超出概率(PE)分别为50%,20%,10%,2%和0.5% 50年后这些超出值分别对应100、225、475、2475和10,000年的返回期。已经在基岩层上绘制了地震危险图,并且可以观察到,与印度标准地震法规[印度标准,抗震设计标准结构图,第五版,第一部分。印度标准局,新德里,2002年]。不仅对地震目录和地震发生带进行了整体处理,而且在空间分布上可以实现更高的分辨率。 COV贴图在各种条件下均具有强大的地面运动贴图,以显示对所得结果的信心。在本研究中获得的结果将有助于风险评估和其他与减灾相关的研究。

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