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Blast Quantification Using Hopkinson Pressure Bars
Published on: July 5, 2016
非火山性震动是由大暂时剪切应力驱动的
Justin L Rubinstein1, John E Vidale, Joan Gomberg
1Department of Earth and Space Science, University of Washington, Box 351310, Seattle, Washington, 98195, USA. justin@ess.washington.edu
Nature
|August 3, 2007
概括
在俯冲区附近的非火山震动可能是由远处地震产生的地震波引发的. 这表明震和缓慢滑动事件是由板面界面上的快速剪切应力增加引起的.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造物理学 构造物理学
背景情况:
- 在火山和俯冲区观察到非冲动性地震辐射或震动.
- 非火山震的确切原因尚不清楚,流体运动和板面接口滑动是主要假设.
- 之前在日本的研究将震与低频地震和潜水界面上的剪切滑动联系起来.
研究的目的:
- 为了调查在卡斯卡迪亚潜伏区的非火山震动的原因.
- 为了确定外部地震事件是否会引发震动.
- 了解震动,缓慢滑动事件和板接口应力之间的关系.
主要方法:
- 分析来自卡斯卡迪亚潜伏区的地震震动数据.
- 震荡爆发与2002年阿拉斯加德纳利地震的地震波到达的相关性.
- 基于Love波移位的板面接口上的剪切应力计算.
主要成果:
- 在卡斯卡迪亚被鉴定出地震爆发,由德纳利地震的爱情波引发.
- 震发生在特定的爱波移位期间,表明触发机制.
- 计算的切割应力约为40kPa,这表明板面接口的有效应力非常低.
结论:
- 震动和潜在的缓慢滑动事件可以通过在引接口上增加剪切应力即时诱导.
- 这种现象代表了对增加的驾驶压力的摩擦失效反应.
- 这些发现挑战了现有的模型,并突出了潜伏区对外部应力的敏感性.
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