在日本东北部,周期性缓慢滑落引发大震区地震
Naoki Uchida1, Takeshi Iinuma2, Robert M Nadeau3
1Graduate School of Science and International Research Institute of Disaster Science, Tohoku University, 6-6, Aramaki-aza-aoba, Aoba-ku, Sendai 980-8578, Japan.
概括
日本的近期缓慢滑动事件
科学领域:
- 地质学
- 构造学
- 地震学
背景情况:
- 板块边界断层通过地震和无地震滑动适应相对运动.
- 在日本东北部,无地震滑动包括未合的俯冲推力区域的后滑和稳定滑动.
研究的目的:
- 报告一个新发现的近期缓慢滑动行为在巨型冲击区.
- 调查慢滑事件与大地震之间的关系.
主要方法:
- 分析地质数据以确定缓慢滑动事件.
- 缓慢滑动事件与地震活动的相关性.
主要成果:
- 在巨型冲击区域中发现了一种广泛的,以前未被识别的近期缓慢滑动行为.
- 缓慢滑动事件每1到6年发生一次.
- 这些事件经常与大型地震 (M ≥ 5) 发生或发生之前,包括2011年M 9东北地震.
结论:
- 周期性缓慢滑动事件可能会导致周期性压力变化.
- 缓慢的滑动事件改变了更大的地震的时间.
- 缓慢滑动的周期性可以改善依赖时间的地震预测.
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