Long-term Aftershock Properties of the Catastrophic 6 February 2023 Kahramanmaraş (Türkiye) Earthquake Sequence

IF 2.1 4区 地球科学 Acta Geophysica Pub Date : 2024-08-08 DOI:10.1007/s11600-024-01419-y
Onur Tan
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Abstract

Nine hours apart, two catastrophic earthquakes (Mw 7.8 and 7.6) occurred on 6 February 2023, in eastern Türkiye. The mainshocks destroyed several cities and villages in 11 provinces, including Kahramanmaraş, Hatay, Adıyaman, Malatya, Adana and Gaziantep. Over about 50,000 aftershocks were detected in the nine months. Because the resolution of hypocentral locations in the Turkish national earthquake catalogs is limited, about 31,000 events are relocated using the double-difference method in this study. The aftershock distribution and its relation to energy release on the faults and Coulomb stress change areas are investigated. The improved hypocenters give a clearer image to understand the activity on the faults. The event distribution indicates that the rupture of the first mainshock in Pazarcık (Mw 7.8) propagates unilaterally on the northernmost segment of the Dead Sea Fault Zone and then transfers to the East Anatolian Fault Zone at the Maraş Triple Junction. The bilaterally extending rupture causes dense aftershock activity on the fault zone from Samandağ to Pütürge. The second mainshock in Elbistan (Mw 7.6) was triggered because of the positive Coulomb stress change on the Çardak fault, which generates dense clusters at both ends of the fault. It is observed that a high number of aftershocks occur on the low slip patches, and the high-energy release areas have low activity because of the stress equilibrium on the fault surfaces.

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2023 年 2 月 6 日 Kahramanmaraş(土耳其)灾难性地震序列的长期余震特性
2023年2月6日,日本东部发生了两次灾难性地震(里氏7.8级和里氏7.6级),相隔9小时。主震摧毁了11个省的几个城市和村庄,包括kahramanmaraku、Hatay、Adıyaman、Malatya、Adana和Gaziantep。在9个月里发现了大约5万次余震。由于土耳其国家地震目录中震源位置的分辨率有限,因此本研究中使用双差法重新定位了大约31,000个事件。研究了断层和库仑应力变化区的余震分布及其与能量释放的关系。改进后的震源为了解断层上的活动提供了更清晰的图像。事件分布表明,Pazarcık第一次主震(Mw 7.8)的破裂在死海断裂带最北段单方面传播,然后在马拉卡拉三交叉点转移到东安纳托利亚断裂带。双边延伸的破裂在从samandaku到p ttrge的断裂带上引起了密集的余震活动。Elbistan的第二次主震(Mw 7.6)是由于Çardak断层上的正向库仑应力变化而触发的,这在断层两端产生了密集的集群。结果表明,在低滑动斑块上发生了大量余震,由于断层表面的应力平衡,高能释放区具有较低的活动性。
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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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