来自固的快速故障愈合控制了深度缓慢滑动和震的动态
Amanda M Thomas1, James M Watkins1, Nicholas Beeler2
1Department of Earth and Planetary Sciences, University of California, Davis, Davis, CA, USA.
Science advances
|November 19, 2025
概括
由凝聚力强度恢复驱动的快速断裂强化,可以控制深度慢滑事件 (SSEs). 这凸显了将凝聚力纳入断层行为地质物理模型的必要性.
科学领域:
- 地质物理学 地质物理学
- 构造物理学 构造物理学
- 地球科学 地球科学 地球科学
背景情况:
- 慢滑事件 (SSEs) 是重要的地质物理现象,但其潜在的物理机制仍然不清楚.
- 当前的模型往往忽略了SSEs期间断层形学中的凝聚力作用.
研究的目的:
- 调查凝聚力强度在卡斯卡迪亚俯冲区深缓滑事件 (SSEs) 动态中的作用.
- 通过模拟故障修复过程来证明凝聚力的重要性.
主要方法:
- 综合了来自卡斯卡迪亚降温区深层SSE的观测数据.
- 在现实的压力和温度条件下进行模拟断层愈合的石油学实验.
主要成果:
- 由于溶解-沉过程,在几个小时的时间尺度上观察到快速的凝聚力强度恢复.
- 在模拟故障条件下证明了显著的凝聚力强度恢复.
结论:
- 凝聚力是SSE期间控制断裂强度的关键因素.
- 未来的数值模型和研究断层滑动动态的实验应该包含凝聚力.
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