由钻井观测站捕捉到的南开沟巨型冲击
Joshua R Edgington1, Demian M Saffer1, Charles A Williams2
1University of Texas Institute for Geophysics, Austin, TX, USA.
概括
在海上潜伏区域的研究显示,缓慢的滑落事件 (SSEs) 向海面迁移到沟. 高孔流体压力和SSE源区域的低应力提供了这些因素与浅地缓慢地震相关的证据.
科学领域:
- 地质学
- 构造学
- 地震学
背景情况:
- 了解潜伏区的压力积累和释放对于评估浅滑和海潜力至关重要.
- 这些过程的离岸模式仍然不太清楚.
研究的目的:
- 分析南开潜伏区缓慢滑动事件 (SSE) 的详细滑动时间历史.
- 研究孔隙液压,应力和浅层SSE之间的关系.
主要方法:
- 来自三个海上钻井观测站的形成孔压力记录的分析.
- 追踪滑动的开始,迁移和相关的地震现象.
主要成果:
- 记录了两个SSE,从沟向陆地30公里开始,以1-2公里/天的速度向海迁移.
- 滑坡距离沟几公里, 可能会破坏沟,
- 在SSE源区域呈现高孔液压和低应力.
结论:
- 提供了观察证据,将高孔液压和低应力与浅缓慢的地震联系起来.
- 证明SSEs可以传播到板边最浅的部分.
- 强调海上监测对于潜水区动态的重要性.
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