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地震是由地震波引发的,其次是Landers和Hector矿山地震
J Gomberg1, P A Reasenberg, P Bodin
1US Geological Survey, Center for Earthquake Research and Information, 3876 Central Avenue Suite 2, Memphis, Tennessee 38152-3050, USA. gomberg@usgs.gov
Nature
|May 25, 2001
概括
大地震产生的暂时的地震波可以引发余震. 动态应力变化超过静态应力变化,在这种地震触发现象中起着关键作用,特别是在更远的距离上.
科学领域:
- 地震地震学 地震学
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
背景情况:
- 1992年的兰德斯地震和1999年的赫克托矿山地震为研究地震触发提供了独特的机会.
- 以前的研究表明,地震波的动态变形可以增加地震率.
研究的目的:
- 量化Landers和Hector矿山地震后地震率变化的空间和时间模式.
- 研究动态和静态应力变化在地震触发中的作用.
- 确定动态触发值及其与当地条件的关系.
主要方法:
- 对响应Landers和Hector矿山地震的地震率变化的分析.
- 观察到的地震性模式与地震波传播和应力变化模型的比较.
- 测量顶峰地震速度以推断动态触发值.
主要成果:
- 在Landers的北部和Hector Mine的南部观察到地震率的增加,与破裂的方向性一致.
- 动态和静态应力变化都有助于触发,动态应力在更远的距离上占主导地位.
- 据估计,动态触发值在十分之一到几MPa之间,明显高于静态值.
- 在动态变形减缓后,在一些地点观察到延迟触发.
结论:
- 作为地震波辐射的动态变形是触发地震性的重要因素.
- 断裂导向性影响动态应力和随后的地震性的空间分布.
- 这些发现支持地震触发过程中的液化或循环疲劳等物理机制.
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