缓慢的地震与偶发的震动和缓慢的滑动事件相吻合
Yoshihiro Ito1, Kazushige Obara, Katsuhiko Shiomi
1National Research Institute for Earth Science and Disaster Prevention, 3-1 Tennodai, Tsukuba 305-0006, Japan. yito@bosai.go.jp
概括
日本发生了非常低频的地震.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 板块构造学是一种板块构造学.
背景情况:
- 位于日本西南部的南开海潜水带是一个具有显著地震活动的地区.
- 了解缓慢地震对于评估地震危险至关重要.
研究的目的:
- 为了调查南开潜伏区的非常低频地震 (VLFEs).
- 分析VLFE,深度低频震动和缓慢滑动事件之间的关系.
主要方法:
- 来自VLFE的地震波的分析.
- 地震数据与深度低频震动和缓慢滑动事件的相关性.
主要成果:
- VLFE表现出具有大约20秒的主导周期的地震波.
- VLFE的地震性与深度低频震动和缓慢滑动事件密切相关,并与之迁移.
结论:
- 随着VLFE,震动和缓慢滑动事件的同时发生,有助于检测和描述缓慢地震.
- 这些缓慢的地震现象可能会增加邻近的巨大冲击地震断裂区域的压力.
相关概念视频
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