在断层断裂区域内明显的时间速度变化,以响应地球潮模式
Tenghui Sun1,2, Huajian Yao1,2,3,4, Hongfeng Yang5,6
1Laboratory of Seismology and Physics of the Earth's Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China.
National science review
|March 14, 2025
概括
在安宁赫断层区域附近的地震速度变化受到地球潮的显著影响. 这种潮效应在断层断裂区域更为明显,凸显了它在应力扰动中的作用.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造物理学 构造物理学
背景情况:
- 持续监测地震断层对于理解地震演变和改善预测至关重要.
- 地震速度变化提供了对地底过程和断层区域内的应力变化的洞察.
研究的目的:
- 为了研究中国西南部安宁河断层区域周围的地震速度变化.
- 为了确定潮力量对断层断裂区域内地震速度变化的影响.
主要方法:
- 使用地震干涉测量技术来分析地震速度.
- 数据分析的重点是确定与潮周期相关的地震速度的周期变化.
主要成果:
- 在安宁河断层断裂区内观察到潮力量对地震速度变化的显著影响.
- 周期性速度变化发生在白天,半白天和月度尺度上,直接与地球的潮有关.
- 与周围地区相比,断层断裂区域对地球潮的反应更加明显,这是由于断层密度更高.
结论:
- 潮力量在破坏地震断层区域内的压力方面发挥着至关重要的作用,特别是在富有断层的地区.
- 断层断裂区域对潮力量的敏感性强调了它们在地震前压力积累中的重要性.
- 这些发现有助于更好地了解断层区域动态和地震过程.
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