上板管道与板边界相连,该板边界是缓慢地震的所在地
Ryuta Arai1, Seiichi Miura2, Yasuyuki Nakamura2
1Research Institute for Marine Geodynamics, Japan Agency for Marine-Earth Science and Technology, 3173-25 Showa-machi, Kanazawa-ku, Yokohama, Kanagawa, 236-0001, Japan. ryuta@jamstec.go.jp.
Nature communications
|September 20, 2023
概括
流体迁移通过受损的区域在俯冲区域的影响地震活动. 这项研究揭示了海底沉降如何产生管道,控制流体流动和Hyuga-nada地区缓慢地震的滑动模式.
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:
- 潜水区的流体行为对于地力学过程至关重要,如滑动行为和泥火山形成.
- 了解控制流体转移的结构和缓慢地震源断层在覆盖板块中的物理性质仍然具有挑战性.
研究的目的:
- 为了研究在Hyuga-nada潜水带中超越板块内的控制流体转移的结构.
- 了解缓慢地震源断层的物理特性.
主要方法:
- 获取和分析高分辨率的地震速度模型.
- 解释地震反射图像以识别地下结构.
主要成果:
- 在上层板块中识别出明显的,宽一公里,低速度的柱子,从海底延伸到10-13公里深.
- 将这些柱子解释为海底浮沉造成的受损区域,作为垂直流体迁移的管道.
- 上板速度/反射率的横向变化与缓慢地震的分布之间的相关性.
结论:
- 海底浮沉可以在覆盖板块内创建显著的流体通道.
- 这些上层板块的流体管道在调节在俯冲板边界观察到的复杂的地震滑动模式方面发挥着至关重要的作用.
- 已识别的排水系统提供了一种机制,将流体迁移与减缓地震行为联系起来.
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