Scholarlink

<p>Coseismic off-fault deformation (OFD) measurements provide crucial insight into fault deformation behavior and shallow faulting damage. Although kinematic and dynamic characteristics of the causative faults associated with the 2023 Turkey-Syria earthquake doublet (Mw 7.8 and 7.6) were well determined, the OFD behavior and mechanism remain poorly constrained. Here we utilized high-resolution optical satellite geodesy to illuminate OFD distribution of the earthquake doublet. We found an average of ~80% and ~83% of coseismic fault deformation were localized on the primary fault planes of the Mw 7.8 and Mw 7.6 earthquakes, respectively; together, the remaining deformation manifested as OFD distributed within an average of 200-m- and 140-m-wide damage zones. Our observations revealed the OFD systematically increases in fault segments that have more complex geometry and slower coseismic rupture velocity, validating that both factors exhibit a significant facilitation on first-order variation of OFD during the earthquake doublet.</p>

错误：搜索内容不能为空，请输入英文关键词
错误：关键词超出字数限制，请精简
高级检索

Fault geometry and rupture speed as controls on off-fault deformation in the 2023 Turkey-Syria earthquakes

  • 期刊论文

  • 出版模式：

    开放获取

  • 发表日期：

    2025年2月12日

查看全文
  • Xi Xi,
  • Chenglong Li,
  • Tao Li,
  • Zhanyu Wei,
  • Zhangfeng Ma,
  • Guohong Zhang,
  • Chunyan Qu,
  • Honglin He,
  • Xinjian Shan

摘要

Coseismic off-fault deformation (OFD) measurements provide crucial insight into fault deformation behavior and shallow faulting damage. Although kinematic and dynamic characteristics of the causative faults associated with the 2023 Turkey-Syria earthquake doublet (Mw 7.8 and 7.6) were well determined, the OFD behavior and mechanism remain poorly constrained. Here we utilized high-resolution optical satellite geodesy to illuminate OFD distribution of the earthquake doublet. We found an average of ~80% and ~83% of coseismic fault deformation were localized on the primary fault planes of the Mw 7.8 and Mw 7.6 earthquakes, respectively; together, the remaining deformation manifested as OFD distributed within an average of 200-m- and 140-m-wide damage zones. Our observations revealed the OFD systematically increases in fault segments that have more complex geometry and slower coseismic rupture velocity, validating that both factors exhibit a significant facilitation on first-order variation of OFD during the earthquake doublet.