Scholarlink

<p>Catastrophic earthquakes have struck along the East Anatolian Fault (EAF), including the 2020 Elaziğ earthquake and the 2023 Kahramanmaraş earthquake doublet. We integrated ground velocity from 2015-2020, together with co- and post-seismic deformation from the 2020 and 2023 earthquakes to investigate the fault slip evolution of the EAF, aiming to reveal the potential future seismic hazards. The spatiotemporally continuous deformation field allows us to derive complete slip distribution models throughout the earthquake cycle, including an interseismic period, two distinct postseismic periods, and three coseismic events. The results demonstrate that the slip patterns exhibit complementary characteristics across the interseismic, coseismic, and postseismic phases. Additionally, by integrating historical earthquake records with the strain accumulated and released during the observation period and quantifying the corresponding slip deficits, we evaluated the seismic potential of the EAF. Among these, the Palu segment emerged as having particularly high seismic risk, emphasizing the need for close monitoring.</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

Slip complementarity and deficit of the East Anatolian Fault revealed by geodetic observations

  • 期刊论文

  • 出版模式：

    开放获取

  • 发表日期：

    2025年11月27日

查看全文
  • Bingquan Han,
  • Chen Yu,
  • Zhenhong Li,
  • Yosuke Aoki,
  • Zhenjiang Liu,
  • Chuang Song,
  • Xiaoning Hu,
  • Jianbing Peng

摘要

Catastrophic earthquakes have struck along the East Anatolian Fault (EAF), including the 2020 Elaziğ earthquake and the 2023 Kahramanmaraş earthquake doublet. We integrated ground velocity from 2015-2020, together with co- and post-seismic deformation from the 2020 and 2023 earthquakes to investigate the fault slip evolution of the EAF, aiming to reveal the potential future seismic hazards. The spatiotemporally continuous deformation field allows us to derive complete slip distribution models throughout the earthquake cycle, including an interseismic period, two distinct postseismic periods, and three coseismic events. The results demonstrate that the slip patterns exhibit complementary characteristics across the interseismic, coseismic, and postseismic phases. Additionally, by integrating historical earthquake records with the strain accumulated and released during the observation period and quantifying the corresponding slip deficits, we evaluated the seismic potential of the EAF. Among these, the Palu segment emerged as having particularly high seismic risk, emphasizing the need for close monitoring.