2023年2月6日 rkey kahramanmaraki地震序列的近场地震动强度参数

Chenna Rajaram , Jayaprakash Vemuri , Vesile Hatun Akansel
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引用次数: 0

摘要

基岛位于安纳托利亚、非洲和阿拉伯构造板块交汇的地震活跃区域。高地震危险性导致该地区多次发生大地震。2023年2月6日,当地时间凌晨04:17(世界标准时间01:17),一场毁灭性的7.7级地震袭击了新西兰。大约9小时后,当地时间上午10点24分,在第一次地震以北95公里处又发生了破坏性的7.6级地震(www.tadas.afad.gov.tr)。7.7级地震引起的强烈地面运动显示,近场区域的峰值地面加速度超过1g,影响了11个城市。复杂的断层几何形状对观察到的高PGAs的影响需要进行检查,以了解相关的结构损伤。本文研究了位于100公里附近的40个台站记录的强地面运动的关键特征,这些特征是进行脆弱性和风险分析的常用强度参数。断层段之间复杂的相互作用显著影响了整个断裂过程和地震动的分布,并在近断层区域产生了明显的脉状地震动。这些地面运动表现出方向性效应,其特征是脉冲速度、峰值地面加速度和谱加速度。响应谱是由几个台站对当前的破坏性/大地震的地面运动导出的,并观察到超过了对应于475年和2475年回复期的规范规定谱。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Near-field ground motion intensity parameters of the major February 06, 2023, Türkey Kahramanmaraş earthquake sequences
Türkey is located in a seismically active region where the Anatolia, Africa, and Arabia tectonic plates converge. The high seismic hazard causes the region to be repeatedly struck by major earthquakes. On February 06, 2023, a devastating Mw 7.7 earthquake struck Türkey at 04:17 a.m. local time (01:17 UTC). Around 9 ​h later at 10:24 a.m. local time, another destructive Mw 7.6 earthquake struck at a distance of 95 ​km towards the north of the first earthquake (www.tadas.afad.gov.tr). The strong ground motion from the Mw 7.7 event shows peak ground accelerations exceeding 1 ​g in the near-field region and affected 11 cities. The effect of the complex fault geometry on the observed high PGAs needs to be examined to understand the associated structural damage. The present study investigates the key characteristics of strong ground motions recorded from 40 stations located in the vicinity of 100 ​km which are commonly used intensity parameters for vulnerability and risk analysis. The complex interaction between fault segments significantly influenced the overall rupture process and the distribution of ground shaking and generated significant pulse-like ground motions in the near-fault region. These ground motions exhibited directivity effects, characterized by pulse-like velocities, high peak ground accelerations, and spectral accelerations. The response spectra are derived for ground motions from several stations for the present destructive/major earthquake and are observed to exceed code prescribed spectra corresponding to the 475-year and 2475-year return periods.
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