大震源破裂指向性效应——以2023年2月6日土耳其特大地震为例

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
O. V. Pavlenko, V. A. Pavlenko
{"title":"大震源破裂指向性效应——以2023年2月6日土耳其特大地震为例","authors":"O. V. Pavlenko,&nbsp;V. A. Pavlenko","doi":"10.1134/S1069351323060149","DOIUrl":null,"url":null,"abstract":"<p>An overview of the results obtained by foreign seismologists based on the records of Turkish seismic networks AFAD (State Agency for Disaster Management under the Ministry of Internal Affairs) is presented. The sequence of earthquakes began with the <i>M</i>7.8 main shock and includes thousands of aftershocks. The strongest events occurred in the first twelve hours, with the sources of two <i>M</i>7.0+ events located 100 km apart. Earthquakes have caused ground motions that are destructive to structures, the so-called “pulse-like waveforms,” and epicentral distances, as was previously noted, are not a good indicator of attenuation of waves from earthquakes with extended ruptures.The records of stations in the near-fault zones clearly revealed the directivity effects of seismic radiation. The <i>M</i>7.8 earthquake (main shock) was larger than expected in the current tectonic setting. The near-field records traced an early transition to the super-shear (~1.55<i>V</i><sub><i>s</i></sub>) rupture propagation on the Narli lateral fault, where the rupture originated and then passed into the East Anatolian fault. The early transition to the super-shear stage obviously contributed to the further propagation of the rupture and the initiation of slips on the East Anatolian fault. A dynamic fracture model has been constructed that matches the various results of inversions obtained by different authors and reveals spatially inhomogeneous rupture propagation velocities. Super-shear velocities exceeding the shear wave velocity <i>V</i><sub><i>s</i></sub> are observed along the Narli lateral fault and at the southwestern end of the East Anatolian fault. Since the late 1990s, seismologists have been working on incorporating the rupture directivity effects of extended sources into the probabilistic seismic hazard analysis procedures, but no consensus has been reached so far, and progress in this area can only be expected with the accumulation of a sufficient amount of observational data.</p>","PeriodicalId":602,"journal":{"name":"Izvestiya, Physics of the Solid Earth","volume":"59 6","pages":"912 - 928"},"PeriodicalIF":0.9000,"publicationDate":"2023-11-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Rupture Directivity Effects of Large Seismic Sources, Case of February 6th 2023 Catastrophic Earthquakes in Turkey\",\"authors\":\"O. V. Pavlenko,&nbsp;V. A. Pavlenko\",\"doi\":\"10.1134/S1069351323060149\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>An overview of the results obtained by foreign seismologists based on the records of Turkish seismic networks AFAD (State Agency for Disaster Management under the Ministry of Internal Affairs) is presented. The sequence of earthquakes began with the <i>M</i>7.8 main shock and includes thousands of aftershocks. The strongest events occurred in the first twelve hours, with the sources of two <i>M</i>7.0+ events located 100 km apart. Earthquakes have caused ground motions that are destructive to structures, the so-called “pulse-like waveforms,” and epicentral distances, as was previously noted, are not a good indicator of attenuation of waves from earthquakes with extended ruptures.The records of stations in the near-fault zones clearly revealed the directivity effects of seismic radiation. The <i>M</i>7.8 earthquake (main shock) was larger than expected in the current tectonic setting. The near-field records traced an early transition to the super-shear (~1.55<i>V</i><sub><i>s</i></sub>) rupture propagation on the Narli lateral fault, where the rupture originated and then passed into the East Anatolian fault. The early transition to the super-shear stage obviously contributed to the further propagation of the rupture and the initiation of slips on the East Anatolian fault. A dynamic fracture model has been constructed that matches the various results of inversions obtained by different authors and reveals spatially inhomogeneous rupture propagation velocities. Super-shear velocities exceeding the shear wave velocity <i>V</i><sub><i>s</i></sub> are observed along the Narli lateral fault and at the southwestern end of the East Anatolian fault. Since the late 1990s, seismologists have been working on incorporating the rupture directivity effects of extended sources into the probabilistic seismic hazard analysis procedures, but no consensus has been reached so far, and progress in this area can only be expected with the accumulation of a sufficient amount of observational data.</p>\",\"PeriodicalId\":602,\"journal\":{\"name\":\"Izvestiya, Physics of the Solid Earth\",\"volume\":\"59 6\",\"pages\":\"912 - 928\"},\"PeriodicalIF\":0.9000,\"publicationDate\":\"2023-11-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Izvestiya, Physics of the Solid Earth\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1134/S1069351323060149\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Izvestiya, Physics of the Solid Earth","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1134/S1069351323060149","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

摘要

本文概述了外国地震学家根据土耳其地震网AFAD(内务部下属的国家灾害管理机构)的记录所获得的结果。地震序列从7.8级主震开始,包括数千次余震。最强的地震发生在前12小时,两个7.0级地震的震源相距100公里。地震引起的地面运动对建筑物具有破坏性,即所谓的“脉冲状波形”,而震中距离,如前所述,并不能很好地指示具有扩展破裂的地震波的衰减。近断裂带台站记录清楚地揭示了地震辐射的指向性效应。在当前构造背景下,7.8级地震(主震)比预期的要大。近场记录显示,纳利侧向断裂早期向超剪切(~1.55Vs)破裂传播过渡,并在此发生断裂,然后传入东安纳托利亚断裂。早期过渡到超剪切阶段明显有助于东安纳托利亚断层破裂的进一步扩展和滑动的开始。建立了一个动态裂缝模型,该模型与不同作者获得的各种反演结果相匹配,并揭示了空间上不均匀的破裂传播速度。沿纳利侧向断裂和东安纳托利亚断裂西南端观测到超剪切速度超过横波速度Vs。自20世纪90年代末以来,地震学家一直致力于将扩展震源的破裂指向性效应纳入概率地震危险性分析程序,但迄今尚未达成共识,只有积累足够的观测数据,才能在这一领域取得进展。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Rupture Directivity Effects of Large Seismic Sources, Case of February 6th 2023 Catastrophic Earthquakes in Turkey

Rupture Directivity Effects of Large Seismic Sources, Case of February 6th 2023 Catastrophic Earthquakes in Turkey

An overview of the results obtained by foreign seismologists based on the records of Turkish seismic networks AFAD (State Agency for Disaster Management under the Ministry of Internal Affairs) is presented. The sequence of earthquakes began with the M7.8 main shock and includes thousands of aftershocks. The strongest events occurred in the first twelve hours, with the sources of two M7.0+ events located 100 km apart. Earthquakes have caused ground motions that are destructive to structures, the so-called “pulse-like waveforms,” and epicentral distances, as was previously noted, are not a good indicator of attenuation of waves from earthquakes with extended ruptures.The records of stations in the near-fault zones clearly revealed the directivity effects of seismic radiation. The M7.8 earthquake (main shock) was larger than expected in the current tectonic setting. The near-field records traced an early transition to the super-shear (~1.55Vs) rupture propagation on the Narli lateral fault, where the rupture originated and then passed into the East Anatolian fault. The early transition to the super-shear stage obviously contributed to the further propagation of the rupture and the initiation of slips on the East Anatolian fault. A dynamic fracture model has been constructed that matches the various results of inversions obtained by different authors and reveals spatially inhomogeneous rupture propagation velocities. Super-shear velocities exceeding the shear wave velocity Vs are observed along the Narli lateral fault and at the southwestern end of the East Anatolian fault. Since the late 1990s, seismologists have been working on incorporating the rupture directivity effects of extended sources into the probabilistic seismic hazard analysis procedures, but no consensus has been reached so far, and progress in this area can only be expected with the accumulation of a sufficient amount of observational data.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信