潮和水力学地震性调制显示,在地震核化过程中孔液扩散
Zeyan Zhao1,2,3, Lian Xue2,3, Roland Bürgmann4
1State Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake Administration, Beijing 100029, China.
Science advances
|December 3, 2025
概括
地震是由周期性压力调节的. 普通地震 (OE) 和低频地震 (LFE) 对潮和水力压力有不同的反应,揭示了不同的核形成过程和断层特性.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造物理学 构造物理学
背景情况:
- 地震事件的发生受到外部周期性应力扰动的影响.
- 了解地震触发机制需要分析这些调制.
- 压力诱导的地震活动的物理基础仍然不完全理解.
研究的目的:
- 调查中央圣安德烈亚斯断层 (CSAF) 上的依赖频率的地震事件调制.
- 区分普通地震 (OE) 和低频地震 (LFE) 对潮和水力压力的反应.
- 阐明孔隙流体扩散和断层特性在地震核和滑动行为中的作用.
主要方法:
- 分析来自中央圣安德烈亚斯断层 (CSAF) 的地震事件数据.
- 地震发生与周期性应力变化 (潮和水文) 的相关性.
- 模拟不同深度的物理性质和流体含量分布.
主要成果:
- 普通的地震 (OE) 显示出对长期水文应激的敏感性.
- 低频地震 (LFEs) 对短时间的潮压力更敏感.
- 频率依赖调制表明OE和LFE的非瞬间核化和不同的核化时间.
- 流体含量和负载条件是控制缓慢到快速断层滑动的关键因素.
结论:
- 周期性地震性调制为地震核化过程提供了洞察力.
- 对OEs和LFE应力变化的明显反应突出了它们物理机制的差异.
- 这些发现适用于理解潜伏区的滑动行为过渡.
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