地震学:地震的动态触发
1US Geological Survey, Suite 2, Memphis, Tennessee 38152, USA. gomberg@usgs.gov
Nature
|October 7, 2005
概括
来自大地震的地震波可以触发几英里外的小地震. 这项研究表明,动态变形的幅度,而不是频率,是触发后续地震事件的关键,无论距离如何.
科学领域:
- 地震学 地震学
- 地震物理学 地震物理学
- 地质物理学 地质物理学
背景情况:
- 地震会引发较小的余震,通常发生在主要断层破裂附近.
- 地震波引发的地震的机制和距离缩放尚未完全理解.
研究的目的:
- 为了分析动态变形与触发地震的距离和强度的缩放.
- 为了确定地震波在哪些条件下可以在不同距离引起进一步的地震.
主要方法:
- 与地震波相关的动态变形 (应力和应变) 的分析.
- 触发要求与实验室诱导的动态弹性非线性行为的比较.
主要成果:
- 动态变形可以触发任何距离的地震,如果它们的振幅超过几微波列.
- 地震波的频率含量不会显著影响它们引发地震的能力.
- 触发要求与实验室实验中观察到的动态弹性非线性行为的触发要求一致.
结论:
- 地震波引起的动态变形的幅度是触发地震的主要因素,无论距离如何.
- 控制远程地震触发的物理似乎与动态弹性非线性行为的实验室观测一致.
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