断层材料的异质性控制深层交叉板地震地震.
Yihe Huang1, Satoshi Ide2, Aitaro Kato3
1Department of Earth and Environment Sciences, University of Michigan, Ann Arbor, MI 48104, USA.
Science advances
|February 26, 2025
概括
地震集群与局部断层损伤和流体丰富有关. 这些条件造成了压力变化,促进了日本潜伏区频繁的深度地震.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 地震通常集中在特定区域,这表明由断层特性和应力变化控制.
- 了解断层材料和应力异质性对于地震危险评估至关重要.
研究的目的:
- 调查日本潜伏区的断层材料和应力异质性.
- 为了将局部结构与地震集群发生的情况相关联.
主要方法:
- 断层材料和地震源的高分辨率成像.
- 材料和源影像与数值模拟的整合.
- 来自日本潜伏区的地震数据的分析.
主要成果:
- 在地震集群周围确定了局部化的,具有接近零的波桑比率的异型结构.
- 这些结构表明受损,叶状和富含液体的断层介质.
- 局部结构导致应力扰动,有利于深层交层地震 (深度60-70公里).
结论:
- 断层材料的异质性显著影响地震的发生.
- 识别断层属性是改善地震危险评估的关键.
- 这些发现为深层交叉板地震的机制提供了洞察力.
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