南开地下推力流与浅地缓慢地震之间的联系
Jin-Oh Park1, Ehsan Jamali Hondori2,3
1Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, Japan. jopark@aori.u-tokyo.ac.jp.
Scientific reports
|July 10, 2023
概括
在南开峡谷的推下流可能会通过改变孔液压和沿着脱落的应力来抑制缓慢的地震. 这一发现为俯冲区地震动态提供了新的见解.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地震学 地震学
背景情况:
- 巨型冲击断层对于理解大型地震至关重要.
- 沟沉积物在断层行为中的作用受到争议.
- 对缓慢地震发生的控制仍然不太了解.
研究的目的:
- 调查岩分布和浅地缓慢地震之间的相关性.
- 分析缓慢地震和滑落赤字率的沿冲击变化.
- 了解压力下的流对潜伏区地震性的影响.
主要方法:
- 从南开沟的地震反射数据的分析.
- 绘制了米欧纪低推力流石的区域分布.
- 将流分布与浅地缓慢地震和滑动缺陷率数据进行比较.
主要成果:
- 在南开积累镜下,创建了一个独特的三种离散的米奥森流石的地图.
- 推力下的流与浅地缓慢地震和滑动缺陷率的变化相关.
- 流石似乎会影响孔液过压和有效的垂直应力.
结论:
- 推力下的流可以通过创建低孔流体过压和高有效垂直应力来抑制缓慢地震的发生.
- 这项研究提供了新的见解,关于在潜伏区的浅地缓慢地震下推力流的作用.
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