Contemporary seismic moment budget along the Nepal Himalaya derived from high-resolution InSAR and GPS velocity field

IF 2.3 4区 地球科学 Acta Geophysica Pub Date : 2024-07-31 DOI:10.1007/s11600-024-01411-6
Himanshu Verma, Yogendra Sharma, Kuo-En Ching, Sumanta Pasari
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Abstract

Throughout history, several large-magnitude earthquakes have caused damage to the Himalayan region and humanity. To understand the present-day strain rate distribution and associated seismic moment budget, a high-resolution velocity field is an essential component. The present study estimates the contemporary seismic moment budget along three spatial sections over the Nepal Himalaya using the state-of-the-art high-resolution velocity field. For this, (1) we integrate 5 years of InSAR data with 77 available GPS observations over the Nepal Himalaya; (2) we then calculate strain rate distribution (dilatational and maximum shear strain rates) from this integrated velocity field, and (3) at last, we compare the geodetic moment accumulation rate estimated from strain rate tensors with the seismic moment release rate based on an earthquake database of 500 years. The results reveal that: (1) the geodetic strain rate is not homogeneous over the Nepal Himalaya, rather along the main central thrust, a relatively higher strain rate is observed; (2) the geodetic moment rate from west to east across three sections ranges from \(23.39\times 10^{18}\) to \(16.59\times 10^{18}\) Nm/yr, with the minimum of \(8.05\times 10^{18}\) Nm/yr in central Nepal, whereas the seismic moment rate varies between \(5.02\times 10^{18}\) and \(11.41\times 10^{18}\) Nm/yr, with the minimum of \(3.69\times 10^{18}\) Nm/yr in central Nepal; (3) the difference between geodetic and seismic moment rates from west to east provides a moment deficit rate of \(18.37\times 10^{18}\) to \(5.18\times 10^{18}\) Nm/yr, with the minimum of \(4.36\times 10^{18}\) Nm/yr in central Nepal, and more importantly, (4) the inferred moment deficit rate suggests that the western and eastern Nepal have an earthquake potential of magnitude \(M_w\) 8.5 and \(M_w\) 8.1, respectively, whereas the central Nepal has energy budget equivalent to an \(M_w\) 7.9 event. In summary, the present study provides spatial distribution of earthquake potential in Nepal Himalaya using the most updated high-resolution InSAR and GPS velocity field, and the findings inevitably contribute to the time-dependent earthquake hazard analysis of the study region.

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从高分辨率 InSAR 和 GPS 速度场得出的尼泊尔喜马拉雅山脉当代地震力矩预算
历史上,数次大震级地震给喜马拉雅地区和人类造成了破坏。要了解当今的应变率分布和相关的地震力矩预算,高分辨率速度场是必不可少的组成部分。本研究利用最先进的高分辨率速度场估算了尼泊尔喜马拉雅山脉三个空间断面的当代地震力矩预算。为此,(1) 我们整合了尼泊尔喜马拉雅山脉 5 年的 InSAR 数据和 77 个可用的 GPS 观测数据;(2) 然后,我们根据整合后的速度场计算应变率分布(扩张应变率和最大剪切应变率);(3) 最后,我们将应变率张量估算出的大地力矩累积率与基于 500 年地震数据库的地震力矩释放率进行比较。结果显示(1) 尼泊尔喜马拉雅山脉的大地应变率并不均匀,相反,在中央主推线上,应变率相对较高;(2) 三个地段的大地力矩率从西向东从 23.39times 10^{18}\ 到 (16.59times 10^{18}\ Nm/yr),尼泊尔中部的最小值为 (8.05times 10^{18}\ Nm/yr),而地震力矩率在(5.02times 10^{18}\ 和 (11.41times 10^{18}\ Nm/yr)之间变化,最小值为 (3.69times 10^{18}\ Nm/yr)。69times 10^{18}) Nm/yr;(3) 大地测量和地震力矩率之间的差异自西向东提供了(18.37times 10^{18}\) to\(5.18times 10^{18}) Nm/yr的力矩亏损率,最小值为(4.36times 10^{18}) Nm/yr,更重要的是,(4)推断出的力矩亏损率表明,尼泊尔西部和东部的地震潜力分别为(M_w\ )8.5级和(M_w\ )8.1级,而尼泊尔中部的能量预算相当于(M_w\ )7.9级事件。总之,本研究利用最新的高分辨率 InSAR 和 GPS 速度场提供了尼泊尔喜马拉雅地区潜在地震的空间分布情况,研究结果必然有助于对研究区域进行随时间变化的地震灾害分析。
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来源期刊
Acta Geophysica
Acta Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.80
自引率
13.00%
发文量
251
期刊介绍: Acta Geophysica is open to all kinds of manuscripts including research and review articles, short communications, comments to published papers, letters to the Editor as well as book reviews. Some of the issues are fully devoted to particular topics; we do encourage proposals for such topical issues. We accept submissions from scientists world-wide, offering high scientific and editorial standard and comprehensive treatment of the discussed topics.
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