Source Mechanisms of Recent Earthquakes in Southern Saudi Arabia: Detecting of New Seismic Sources

Ahmed Hosny, Abdullah Mousa, Khaled Yousef, Lotfy Samy, Hamada Sadallah
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Abstract

Recently in 2020, in southern Saudi Arabia three felt earthquakes occurred in Asir region, in the Khamis Mushait, Ahad Rafidah, and AL-Shuqiq area, of magnitude 3.45, 3.1, and 3.5, respectively. The most interesting event was the earthquake that occurred in Khamis Mushait area, along a lake formed behind the Tadhah Dam (~7 km), fearing any damage to the dam’s body and the consequent destruction. Moment tensors for each event were computed for determining fault plane solutions, seismic moment, moment magnitude (Mw) and the CLVD ratio. In addition, the frequency contents in the waveforms of each event were identified. The obtained focal mechanisms represent different styles of faulting, normal movement with strike slip and strike slip with reverse. These tectonic movements on faults parallel to the Red Sea refer to the tensional forces due to the Red Sea rift system. These events occurred due to a natural tectonic movement, with considering the Khamis Mushait event as an induced event because of the lake behind the Dam. Many previous seismic hazard assessment studies have been conducted in southern Saudi Arabia without considering these recent seismic sources. Thus, our study provides new information related to detecting of new active seismic sources, which contributes to updating studies of seismic risk assessment in this region. In addition, our study pushes us to establish other additional seismic stations around these new seismic sources. This in turn will play a pivotal role in controlling seismic sources and then reassessing the seismic hazard in southern Saudi Arabia.
沙特阿拉伯南部近期地震的震源机制:新震源的探测
最近在2020年,在沙特阿拉伯南部的阿西尔地区,Khamis Mushait, Ahad Rafidah和AL-Shuqiq地区发生了三次感觉地震,分别为3.45,3.1和3.5级。最有趣的事件是发生在Khamis Mushait地区的地震,该地区位于塔达大坝(约7公里)后面形成的一个湖泊附近,人们担心大坝的身体会受到损害,从而导致破坏。计算每个事件的矩张量,以确定断层面解、地震矩、矩量级(Mw)和CLVD比。此外,还识别了各事件波形中的频率内容。所获得的震源机制代表了不同类型的断层,即正移带走滑和逆移带走滑。这些与红海平行的断层上的构造运动是指红海裂谷系统所产生的张力。这些事件的发生是由于自然构造运动,考虑到Khamis Mushait事件是由于大坝后面的湖泊而诱发的事件。以前在沙特阿拉伯南部进行的许多地震危险性评估研究都没有考虑到这些最近的震源。因此,我们的研究为新活动震源的探测提供了新的信息,有助于更新该地区地震危险性评估的研究。此外,我们的研究促使我们在这些新震源周围建立其他额外的地震台站。这反过来将在控制震源和重新评估沙特阿拉伯南部的地震危险性方面发挥关键作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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