超低摩擦愈合解释了反复发生的缓慢滑动事件
Srisharan Shreedharan1,2, Demian Saffer1,3, Laura M Wallace1,4
1Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USA.
概括
浅浅的潜水区表现出各种各样的构造滑动模式. 这项研究揭示了Hikurangi边缘的近零摩擦愈合率,解释了频繁的小压力滴缓慢滑动事件 (SSEs).
科学领域:
- 地质学
- 构造学
- 地球科学
背景情况:
- 板块运动在浅层沉降巨潮上涉及各种构造滑动模式.
- 控制这些不同的滑动行为的摩擦性质尚未完全理解.
- 摩擦愈合,地震间断层的强化, 是一个关键特性.
研究的目的:
- 在北方的Hikurangi巨型岩石上研究材料的摩擦特性.
- 为了确定浅缓滑事件 (SSEs) 的区域的摩擦愈合率.
- 阐明浅层SSE低压力下降和短复发时间背后的机制.
主要方法:
- 岩石样本和物质的分析沿着北方的Hikurangi巨型岩石.
- 使用实验室实验或现场数据测量摩擦愈合率.
- 治愈率与观察到的滑动行为,压力下降和复发间隔的相关性.
主要成果:
- 在北方的Hikurangi巨型岩石上,材料的摩擦愈合率几乎为零 (每十年<0.0001).
- 这些低愈合率与潜水区常见的弱酸盐有关.
- 这些发现为浅层SSE的特征性低应力下降 (<50kPa) 和短复发时间 (1-2年) 提供了机制.
结论:
- 接近零的摩擦愈合率可以促进沟附近的频繁,小压力下降,缓慢的破裂.
- 薄弱的酸盐可能在潜水边缘的浅层SSE中发挥关键作用.
- 了解摩擦愈合对于理解板块构造和地震过程的动态至关重要.
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