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土耳其Mw7.9级帕扎尔吉克地震和Mw7.6级埃尔比斯坦地震之间地面运动的特征。

Characteristic in ground motions between the Mw7.9 Pazarcık earthquake and the Mw7.6 Elbistan earthquake in Türkiye.

作者信息

Xu Peibin, Liu Xingguo, Li Lin

机构信息

School of Civil Engineering, Harbin University, No.109 Zhongxing Road, Harbin, 150086, China.

出版信息

Sci Rep. 2025 Jul 1;15(1):21753. doi: 10.1038/s41598-025-06597-3.

Abstract

On February 6, 2023, two destructive earthquakes occurred in Türkiye, namely, the Pazarcık earthquake with moment magnitude 7.9 and the Elbistan earthquake with moment magnitude 7.6. A larger number of strong motion recordings were obtained in both events, facilitating the examination of their ground motion characteristics. Using four ground-motion prediction equations (GMPEs)-two regional and two global-we computed total residual (R), between-events residual (δB), within-event residual (δW) and adjustment coefficient of anelastic attenuation (Δc), for peak ground acceleration (PGA), pseudo-spectral accelerations (PSAs) and 5-95% significant duration. Both regional and global GMPEs exhibit period- and distance-dependent for R, which can be attributed to discrepancy in tectonic settings and geological conditions among different regional datasets used in their development, leading to variations in ground motion. Predominantly negative δB values at periods T < 0.2 s for both earthquakes (except for positive values in the Pazarcık event for the Kale2015 model) indicate: source effects are weaker than the average levels represented by the GMPEs, and stronger than those characterized by specific-regional model Kale2015 for the Pazarcık earthquake. The observed increasing trend in δB values at periods T > 0.6 s, which can be attributed to supershear rupture (via Mach wave amplification) and forward rupture directivity. Predominantly negative Δc values (Pazarcık earthquake: -0.0002 to -0.0073; Elbistan earthquake: -0.0001 to -0.0204) indicate faster anelastic attenuation in the affected zone of both earthquakes than regional averages presented by all GMPEs, aligning with prior studies of the East Anatolian Fault. These results provided valuable insights for improving regional seismic hazard models.

摘要

2023年2月6日,土耳其发生了两次破坏性地震,即矩震级为7.9级的帕扎尔吉克地震和矩震级为7.6级的埃尔比斯坦地震。在这两次地震中都获得了大量强震记录,便于研究它们的地面运动特征。我们使用四个地面运动预测方程(GMPEs)——两个区域方程和两个全球方程——计算了峰值地面加速度(PGA)、伪谱加速度(PSAs)和5 - 95%显著持续时间的总残差(R)、事件间残差(δB)、事件内残差(δW)和滞弹性衰减调整系数(Δc)。区域和全球GMPEs的R都表现出周期和距离依赖性,这可归因于其开发中使用的不同区域数据集在构造环境和地质条件上的差异,导致地面运动的变化。两次地震在周期T < 0.2秒时,δB值主要为负(帕扎尔吉克地震中Kale2015模型的情况除外,该模型在此处为正值),这表明:震源效应比GMPEs所代表的平均水平弱,但比帕扎尔吉克地震特定区域模型Kale2015所表征的更强。在周期T > 0.6秒时,δB值呈现出上升趋势,这可归因于超剪切破裂(通过马赫波放大)和向前破裂方向性。Δc值主要为负(帕扎尔吉克地震:-0.0002至-0.0073;埃尔比斯坦地震:-0.0001至-0.0204),表明两次地震影响区内的滞弹性衰减比所有GMPEs给出的区域平均值更快,这与先前对东安纳托利亚断层的研究结果一致。这些结果为改进区域地震危险性模型提供了有价值的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a5ed/12216333/13342c3f4ce6/41598_2025_6597_Fig1_HTML.jpg

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