埃及南部阿斯旺地区大于3.0级地震的动力源和地震动参数量化

IF 2.2 4区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Hamada Saadalla , Saleh Qaysi , Abdalla Abdelnabi , Mona Hamada
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引用次数: 0

摘要

本文对2010 - 2024年埃及南部阿斯旺地区阿斯旺地震宽带网络记录的震级ML≥3.0的地震动态震源参数进行了估算。采用带参考点的线性最小二乘分析方法,采用光谱反演方法分离观测位移光谱中的源、接收机和路径效应。首先,去除沿射线路径的衰减效应和位置特异性效应,推导出每个事件的源光谱。采用Brune模型,利用s波位移源谱估计动力源参数及其标度关系。从导出的位移谱中,我们估计了每个事件的源参数,包括地震矩、角频率、断层半径和静态应力降。结果表明,应力降和震源半径随矩量的增大而增大。研究地震的应力降在0.4 ~ 4.8 MPa之间,表明水库引发地震的应力降可能比构造或地壳地震小。震源半径在139.8 ~ 294.5 m之间,角点频率随矩量级的增大而减小,在4.3 ~ 9.0 Hz之间。为了评估阿斯旺地震带及其周边地区的地震危险性,在新阿斯旺市、阿斯旺大学、萨哈里市和库尔库尔村四个地点对当地震级ML≥3.5的地震进行了随机模拟分析。模型参数包括峰值地加速度(PGA)、峰值地速度(PGV)、峰值地位移(PGD)和伪谱加速度(PSA)。结果表明,2010年11月7日发生在阿斯旺大学的地震在震源距离为2 km的情况下,模拟出了最高的PGA (24.2 cm/s2)、PGV (0.4 cm/s)和PGD (0.013 cm)。此外,在同一事件中,阿斯旺大学和萨哈里市的PSA值最高,分别为72.6 cm/s2和65.9 cm/s2。这些发现为评估阿斯旺地区的地震危险性提供了重要的见解,有助于更好地了解埃及南部的地震风险。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Quantifying dynamic source and ground motion parameters for earthquakes bigger than 3.0 in Aswan region, southern Egypt
The dynamic source parameters of earthquakes with local magnitudes ML 3.0, recorded by the Aswan seismic broadband network between 2010 and 2024 in the Aswan region of southern Egypt, have been estimated. A spectral inversion method was applied to separate the source, receiver, and path effects from the observed displacement spectra using linear least squares analysis with a reference site. Initially, the attenuation effects along the ray path and site-specific effects were removed to derive the source spectra for each event. The Brune model was then employed to estimate the dynamic source parameters and their scaling relationships using S-wave displacement source spectra. From the derived displacement spectra, we estimated source parameters for each event, including seismic moment, corner frequency, fault radius, and static stress drop. The results indicate that both stress drop and source radius increase with moment magnitude. The observed stress drops for the studied earthquakes range from 0.4 to 4.8 MPa, suggesting that reservoir-triggered earthquakes may exhibit lower stress drops compared to tectonic or crustal earthquakes. The source radius varies from 139.8 to 294.5 m, while the corner frequency decreases with increasing moment magnitude, ranging from 4.3 to 9.0 Hz. To assess earthquake hazards in the Aswan seismic zone and its surrounding areas, stochastic simulation analyses were conducted for earthquakes with local magnitudes ML ≥ 3.5 at four sites: New Aswan City, Aswan University, Sahary City, and Kurkur Village. The modeled parameters include peak ground acceleration (PGA), peak ground velocity (PGV), peak ground displacement (PGD), and pseudo-spectral acceleration (PSA). The results revealed that the highest PGA (24.2 cm/s2), PGV (0.4 cm/s), and PGD (0.013 cm) were simulated at Aswan University for the earthquake on November 7, 2010, with an epicentral distance of 2 km. Additionally, the highest PSA values were 72.6 cm/s2 and 65.9 cm/s2 at Aswan University and Sahary City, respectively, for the same event. These findings provide essential insights for evaluating seismic hazards in the Aswan region, contributing to a better understanding of earthquake risks in southern Egypt.
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来源期刊
Journal of African Earth Sciences
Journal of African Earth Sciences 地学-地球科学综合
CiteScore
4.70
自引率
4.30%
发文量
240
审稿时长
12 months
期刊介绍: The Journal of African Earth Sciences sees itself as the prime geological journal for all aspects of the Earth Sciences about the African plate. Papers dealing with peripheral areas are welcome if they demonstrate a tight link with Africa. The Journal publishes high quality, peer-reviewed scientific papers. It is devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be considered. Papers must have international appeal and should present work of more regional than local significance and dealing with well identified and justified scientific questions. Specialised technical papers, analytical or exploration reports must be avoided. Papers on applied geology should preferably be linked to such core disciplines and must be addressed to a more general geoscientific audience.
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