在2011年MW 9.0东北奥基地震中,浅动态超速和能量深层破裂
Satoshi Ide1, Annemarie Baltay, Gregory C Beroza
1Department of Earth and Planetary Science, University of Tokyo, Hongo 7-3-1, Bunkyo-ku, Tokyo 113-0033, Japan. ide@eps.s.u-tokyo.ac.jp
概括
2011年东北奥基地区发生的地震.
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:
- 2011年东北奥基地震 (当时的9.0级) 造成了广泛的破坏.
- 了解其破裂特征对于地震危险评估至关重要.
研究的目的:
- 分析东北奥基地震的空间和时间断裂特征.
- 调查破裂行为,地震和海产生之间的关系.
主要方法:
- 使用了有限源成像技术.
- 对地震波形和余震分布的分析.
主要成果:
- 断裂呈现出显著的空间变化,具有明显的深层和浅层阶段.
- 在沟附近发生了很大的浅滑,可能是由于断层几何和悬挂墙的合规性.
- 正常的断层余震表明在高滑坡地区的动态超速.
- 高频辐射来自更深的破裂区域比较浅的区域更强.
结论:
- 断裂特征的空间变化直接影响了震动强度和海大小.
- 断层几何学和悬挂墙的特性在使大浅滑坡成为可能方面发挥了作用.
- 地震的破裂动态提供了关于巨型冲击地震行为和地震波辐射的见解.
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