粘土中的摩擦不稳定性揭示了缓慢地震的起源
Giuseppe Volpe1, Cristiano Collettini1,2, Jacopo Taddeucci2
1Dipartimento di Scienze della Terra, La Sapienza Università di Roma, Rome, Italy.
Science advances
|June 28, 2024
概括
含有土壤丰富的断层的浅浅的俯冲区域可以表现出缓慢的无地震爬行和危险的缓慢滑动事件 (SSEs). 实验显示,这些断层内部的局部剪切区域使SSE核形成成为可能,这挑战了标准的摩擦理论.
科学领域:
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
- 构造物理学 构造物理学
背景情况:
- 浅层俯冲巨型冲击主要是无地震变形,但可以承载危险的慢滑事件 (SSEs) 和海地震.
- 富含粘土的浅层俯冲区的摩擦特性不太清楚,因为标准摩擦理论不能很容易地解释这些地区的地震滑动.
研究的目的:
- 调查使在富含粘土的断层中同时实现无地震爬行和缓慢滑动事件核化的机制.
- 挑战现有的摩擦理论,并提出一个替代的范式,以了解在浅沉降区的断层滑动行为.
主要方法:
- 分析了来自富含粘土的断层的实验数据,这些断层具有大量增强率的行为和零愈合率.
- 专注于由结构和应力异质性驱动的薄切割区内的缓慢断裂.
主要成果:
- 富含粘土的断层表现出大量增强速度的行为,可以同时在无地震上爬行并形成SSE的核.
- 在局部薄切割区域内观察到缓慢的断裂,由断层异质性驱动.
- 大量速率的增强促进了无地震爬行,而局部的剪切区域则促进了缓慢的破裂核和传播.
结论:
- 双摩擦行为模型解释了富含粘土的断层如何表现出无地震爬行和SSE.
- 在速率增强断层内的局部摩擦剪切为SSE和海地震提供了一种机制.
- 这项研究为浅层潜水带断层的复杂行为提供了新的视角.
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