复杂的多断层断裂和触发在东南土耳其2023年地震双重期间
Chengli Liu1, Thorne Lay2, Rongjiang Wang3,4
1School of Geophysics and Geomatics, China University of Geosciences, Wuhan, Hubei, China. liuchengli@cug.edu.cn.
Nature communications
|September 9, 2023
概括
在土耳其发生的两次大地震中,使用地震和地质数据进行了分析. 动力学模型揭示了断裂细节和应力变化,这表明第一次地震可能引发了第二次地震.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 2023年2月6日,东安纳托利亚断层区 (EAFZ) 的地震 (MW 7.8和MW 7.7) 造成了灾难性的破坏和死亡.
- 亚非贸易区是一个主要的左侧冲滑断层系统,位于地震活跃地区.
研究的目的:
- 为了获得两个主要地震的动力破裂模型.
- 了解断裂动态,包括速度,滑动分布和断裂相互作用.
- 评估应力转移在触发地震双倍的作用.
主要方法:
- 对广泛的地震和地质观测的反转.
- 开发复杂的5-6段故障模型.
- 限制模型与卫星观测和转移的余震.
主要成果:
- 这场MW 7.8事件始于分裂断层,沿EAFZ主链延伸约350公里,滑行速度高达8.1米,速度为2.5-4.5公里/秒.
- MW 7.7事件沿北EAFZ链破裂了约160公里,显示出初始的超切割破裂速度 (>4公里/秒),随后的速度较慢 (~3公里/秒).
- 库伦应力分析表明,第一个事件可能触发了第二个,并加载了相邻的断层.
结论:
- 详细的动力学模型提供了对EAFZ地震复杂破裂过程的见解.
- 这些发现突出了静态应力变化在连续的大地震触发中的重要作用.
- 了解这些断裂动态对于评估该地区的地震危险至关重要.
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