2019年加利福尼亚州里奇克雷斯特7.1级地震及其6.4级Foreshock序列之间的关系
Jianchang Zheng1,2, Zhengshuai Zhang2, Xiaohan Li2
1Department of Mathematics and Statistics, University of Otago, Dunedin 9054, New Zealand.
Entropy (Basel, Switzerland)
|January 24, 2025
概括
2019年里奇克雷斯特地震序列,包括其7.1级 (MW) 主震,主要是由西北冲击断层的活动驱动的. 一个较小的M4.0事件直接先于M6.4前震,揭示了复杂的断层相互作用.
科学领域:
- 地震学 地震学
- 地震科学 地震科学 地震科学
- 构造学 构造学 构造学 构造学
背景情况:
- 2019年里奇克雷斯特地震的序列包括一个复杂的M7.1主震和一个显著的M6.4前震.
- 了解强烈地震序列中的动态关系对于地震危险评估至关重要.
研究的目的:
- 分析2019年里奇克雷斯特地震的前震和余震序列.
- 阐明控制序列的复杂动态关系和断层结构.
主要方法:
- 使用移动的地震目录进行详细分析.
- 应用了最近邻近算法来识别地震序列中的链接和家族结构.
主要成果:
- 确定了7月6日发生的M{W}5.0事件,作为M{W}7.1主震动的直接前震,可能与断层障碍有关.
- 描述了7月4日发生的M(W)6.4事件,作为一个复杂的合破裂.
- 证实了M4.0事件在西北冲击断层作为直接的前冲击到M(W)6.4事件.
结论:
- 里奇克雷斯特地震序列主要受到西北冲击断层活动的影响.
- 这一序列在西北断层上引发了小破裂,在西南断层上引发了并联滑动,并在西北断层上达到更大的破裂.
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