缓慢的地震缩放被重新考虑为突破传播的不同模式之间的边界
Satoshi Ide1, Gregory C Beroza2
1Department of Earth and Planetary Science, The University of Tokyo, Tokyo 113-0033, Japan.
概括
缓慢地震的缩放定律仍然有效作为时刻率的上限,这表明扩散传播的速度限制. 这与普通地震形成了鲜明对比,突出了地震事件中独特的物理过程.
科学领域:
- 地球科学 地球科学 地球科学
- 地震学 地震学
- 地质物理学 地质物理学
背景情况:
- 15年前,人们提出了缓慢地震的地震时刻和持续时间之间的线性缩放定律.
- 这引发了关于缓慢和快速 (普通) 地震之间的物理过程差异的争论.
研究的目的:
- 通过新的,广泛的观测,重新评估缓慢地震的缩放定律.
- 研究区分缓慢和快速地震的物理过程.
主要方法:
- 对跨越广泛时期范围的新地震观测结果的分析.
- 缓慢和快速地震类别之间的时刻率缩放的比较.
主要成果:
- 缓慢地震的线性缩放被证实为时刻速率 (~10^13 Nm/s) 的有效上限.
- 在缓慢和快速地震之间,瞬间速度仍然存在显著的差距.
- 观察到的趋势表明,无法观察到的缓慢地震的时刻率较低.
结论:
- 缓慢地震的缩放定律应该被视为扩散传播的"速度限制".
- 普通的地震包括合的地震波传播和断裂.
- 这种明显的缩放反映了缓慢和快速地震的物理传播机制的根本差异.
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