Probabilistic Seismic Hazard Assessment of Sitamarhi near the Central Himalayan Region

IF 1.2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Abhik Paul, P. Chakrabortty, A. Burman, Sapan Kumar
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Abstract

Sitamarhi, situated in the North-Bihar region of the Himalayan foothills is one of the seismically vulnerable regions of India. This region faced several devastating earthquakes, such as the 1934 and 1988 Bihar Nepal earthquake and the 2015 Nepal earthquake due to the movement of tectonic plates. The purpose of the present study is to exhibit the uniform hazard spectrum (UHS) and peak ground acceleration (PGA) values based on the probabilistic seismic hazard method using different seismotectonic parameters. The Gutenberg Richter (G-R) seismicity parameters ‘a’ and ‘b’ were estimated on the basis of regional earthquake magnitude data for the studied region. Regional earthquakes data were taken from the United States Geological Survey (USGS), International Seismological Centre (ISC), Indian Meteorological Department (IMD), and Seismotectonic Atlas of India. The region of interest for the probabilistic seismic hazard analysis (PSHA) is within a 500 km radius considering past seismicity and 62 seismotectonic sources which were identified in the study area. Large-scale geological features were utilised to describe the regional seismic source zones, which were used to derive the relationship between return period and ground motion parameters. Estimated PGA values are 0.92g for 2% and 0.68g for 10% probability of exceedance in 50 years time period, respectively. This research infer that the West Patna fault (WPF) and Sitamarhi fault (SMF) are the two maximum contributors in PGA for the Sitamarhi region.
喜马拉雅中部地区附近锡塔马里的地震危害概率评估
锡塔马里位于喜马拉雅山麓的北比哈尔地区,是印度地震易发地区之一。由于构造板块的运动,该地区曾多次发生破坏性地震,如 1934 年和 1988 年的尼泊尔比哈尔邦地震以及 2015 年的尼泊尔地震。本研究的目的是利用不同的地震构造参数,展示基于概率地震危险法的均匀危险谱(UHS)和峰值地面加速度(PGA)值。古登堡里氏(G-R)地震参数 "a "和 "b "是根据研究区域的地区震级数据估算的。地区地震数据来自美国地质调查局(USGS)、国际地震中心(ISC)、印度气象局(IMD)和印度地震构造图集。考虑到过去的地震活动和研究区域内已确定的 62 个地震构造源,地震危险概率分析(PSHA)的关注区域在 500 公里半径范围内。利用大尺度地质特征描述了区域震源带,并以此推导出重现期与地动参数之间的关系。估计的 PGA 值分别为 0.92g(50 年内超限概率为 2%)和 0.68g(10%)。这项研究推断,西巴特那断层(WPF)和锡塔马里断层(SMF)是锡塔马里地区 PGA 值最大的两个来源。
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来源期刊
Journal of the Geological Society of India
Journal of the Geological Society of India 地学-地球科学综合
CiteScore
2.20
自引率
7.70%
发文量
233
审稿时长
6 months
期刊介绍: The Journal aims to promote the cause of advanced study and research in all branches of geology connected with India, and to disseminate the findings of geological research in India through the publication.
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