Near Real-Time Detection and Moment Tensor Inversion of the 11 May 2022, Dharchula Earthquake

Pankaj Kumar, V. Silwal, Rinku Mahanta, V. Maurya, Kamal, Mukat Lal Sharma, Ambikapathy Ammani
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Abstract

On 11 May 2022, an earthquake of Mw 5.2 occurred in the Dharchula region of Uttarakhand Himalayas, India. The Uttarakhand State Earthquake Early Warning System (UEEWS) detected and transmitted the warning within 11.61 s from the origin time, taking only 4.26 s for processing, location, and magnitude estimation and warning dissemination. The complete analysis was performed using three seconds of waveforms. Using the initial earthquake parameters provided by the UEEWS, moment tensor inversion was performed using the broadband seismometers network installed in northern India. The moment tensor (MT) inversion was performed for the event using both the body waves and the surface waves. The first motion polarity was used along with waveform data to enhance the solution’s stability. This paper discusses the importance of real-time event detection and efforts towards real-time MT source inversion of earthquakes in the Uttarakhand Himalayas. Relocation of two past earthquakes near Dharchula is also undertaken in this study. The outcome of this study provides insights into mitigating seismic hazards, understanding earthquake source mechanisms, and enhancing knowledge of local fault structures.
2022 年 5 月 11 日达丘拉地震的近实时探测和力矩张量反演
2022 年 5 月 11 日,印度北阿坎德邦喜马拉雅山达丘拉地区发生了 5.2 级地震。北阿坎德邦地震预警系统(Uttarakhand State Earthquake Early Warning System,UEEWS)在从起始时间算起的 11.61 秒内检测到并发出警报,仅用了 4.26 秒进行处理、定位、震级估计和警报发布。整个分析过程使用了三秒钟的波形。使用 UEEWS 提供的初始地震参数,利用安装在印度北部的宽带地震仪网络进行了力矩张量反演。利用体波和面波对事件进行了力矩张量(MT)反演。第一运动极性与波形数据一起使用,以增强解决方案的稳定性。本文讨论了实时事件检测的重要性,以及对北阿坎德邦喜马拉雅山脉地震进行实时 MT 震源反演的努力。本研究还对达丘拉附近过去发生的两次地震进行了重新定位。这项研究的成果为减轻地震危害、了解震源机制和增进对当地断层结构的了解提供了见解。
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