Source characterisation of June 2023 Doda (Kashmir) earthquake

IF 1.1 4区 地球科学 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
MAUSAM Pub Date : 2025-06-28 DOI:10.54302/mausam.v76i3.6684
Sindu Kumari, Ambikapathy Ammani, DELNA JOY K., VISHWARANJAN OJHA, SANDEEP ARORA
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引用次数: 1

Abstract

On the 13th of June 2023, at 13:33:42 IST, an earthquake of magnitude Ml5.1 occurred in the Doda region of Jammu & Kashmir (J&K). The earthquake's epicenter was at coordinates 33.15 N and 75.89 E, with a shallow depth of 10 km. This seismic event unfolded within the geological context of the Himalayan orogeny, which has taken shape as a consequence of the collision between the Indian plate and the Eurasian plate. The Himalayan region, characterized by the intricate dynamics of these tectonic collisions, harbours numerous significant regional and local fault systems. A substantial portion of these fault lines remains active, continually generating seismic activity throughout the Himalayan region and its adjacent areas. Despite causing minor structural damage to a few buildings in the source region, this particular earthquake was well-documented and was accurately located by the Indian National Seismic Network, which is operated by the National Centre for Seismology (NCS), Ministry of Earth Sciences (MoES). Notably, the NCS-MoES maintains three Seismological observatories in Jammu & Kashmir (specifically in Jammu, Srinagar, and Udhampur), along with two additional Seismological observatories in Ladakh (in Hanley and Alchi). In the present study, we have harnessed waveform data collected from a network of 15 Seismological observatories managed by NCS-MoES, strategically positioned across J&K, Ladakh, and Himachal Pradesh. Our research endeavours to estimate the source characteristics including the precise determination of the earthquake's geographical location. Our analysis employed specialized software tools, SEISAN for epicenter localization and ISOLA for fault plane solution. Moreover, these derived seismic parameters served as foundational data for further analyses. Specifically, we leveraged these parameters to quantify the energy released and determine the source radius. These additional insights provided a comprehensive characterization of this earthquake and its implications.
2023年6月多达(克什米尔)地震震源特征
2023年6月13日13时33分42秒,查谟克什米尔(J&;K)的多达地区发生5.1级地震。震中位于北纬33.15度,东经75.89度,震源深度为10公里。这次地震发生在喜马拉雅造山运动的地质背景下,这是印度板块和欧亚板块碰撞的结果。喜马拉雅地区以这些构造碰撞的复杂动力学为特征,拥有许多重要的区域和局部断层系统。这些断层线的很大一部分仍然活跃,在整个喜马拉雅地区及其邻近地区不断产生地震活动。尽管这次地震对震源地区的一些建筑物造成了轻微的结构破坏,但它被记录得很好,并被印度国家地震台网准确定位。印度国家地震台网由地球科学部国家地震学中心(NCS)运营。我们的研究努力估计震源特征,包括精确确定地震的地理位置。我们的分析使用了专门的软件工具,SEISAN用于震中定位,ISOLA用于断层面解决。此外,这些导出的地震参数为进一步分析提供了基础数据。具体来说,我们利用这些参数来量化释放的能量并确定源半径。这些额外的见解为这次地震及其影响提供了一个全面的特征。
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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来源期刊
MAUSAM
MAUSAM 地学-气象与大气科学
CiteScore
1.20
自引率
0.00%
发文量
1298
审稿时长
6-12 weeks
期刊介绍: MAUSAM (Formerly Indian Journal of Meteorology, Hydrology & Geophysics), established in January 1950, is the quarterly research journal brought out by the India Meteorological Department (IMD). MAUSAM is a medium for publication of original scientific research work. MAUSAM is a premier scientific research journal published in this part of the world in the fields of Meteorology, Hydrology & Geophysics. The four issues appear in January, April, July & October.
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