Along-Strike Variation of Rupture Characteristics and Aftershock Patterns of the 2023 Mw 7.8 Türkiye Earthquake Controlled by Fault Structure

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Seismological Research Letters Pub Date : 2024-03-14 DOI:10.1785/0220230378
Zhifan Wan, Rendong Dong, Dun Wang, Shiqing Xu, Zhifeng Wang, Qi Wang
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Abstract

On 6 February 2023, an Mw 7.8 earthquake occurred along the East Anatolian fault zone (EAFZ) in southeastern Türkiye, representing the strongest earthquake in the region in nearly 80 yr. We investigate rupture characteristics and aftershock patterns of the earthquake through focal mechanism calculation, backprojection analysis, and finite-fault inversion. The results show bilateral rupture propagation of the mainshock with transient supershear speed in the southwest portion of the EAFZ, as well as shallower coseismic slip and abundant normal-faulting aftershocks in the same portion. We attribute these earthquake behaviors to the along-strike variation of fault structure of the EAFZ, which features a more complex fault geometry accompanied by numerous short normal faults in the southwest portion. These results shed light on fault segmentation, rupture speed variation, and slip partitioning along the EAFZ, advancing our understanding of fault structural control on earthquake behaviors in a complex multisegment fault system.
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受断层结构控制的 2023 年图尔基耶 7.8 级地震破裂特征的沿震变化和余震模式
2023 年 2 月 6 日,土耳其东南部东安纳托利亚断裂带(EAFZ)发生了 Mw 7.8 级地震,这是该地区近 80 年来最强烈的地震。结果表明,在 EAFZ 西南部,主震以瞬时超剪切速度进行了双边破裂传播,同时在同一地区还发生了较浅的共震滑移和大量的正断层余震。我们将这些地震行为归因于 EAFZ 断层结构的沿走向变化,其特点是西南部的断层几何形状更为复杂,并伴有大量短的正断层。这些结果揭示了断层分段、破裂速度变化以及沿 EAFZ 的滑动分区,加深了我们对复杂的多段断层系统中断层结构对地震行为控制的理解。
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来源期刊
Seismological Research Letters
Seismological Research Letters 地学-地球化学与地球物理
CiteScore
6.60
自引率
12.10%
发文量
239
审稿时长
3 months
期刊介绍: Information not localized
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