实验室地震:Rayleigh下部到supershear的断裂过渡
Kaiwen Xia1, Ares J Rosakis, Hiroo Kanamori
1Seismological Laboratory, MC 252-21, California Institute of Technology (Caltech), Pasadena, CA 91125, USA.
概括
研究人员观察到超级剪切裂变,在实验室中模仿地震. 这些发现表明,在特定条件下的大自然地震中,可能会发生超级剪切传播.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 材料科学 材料科学 材料科学
背景情况:
- 地震涉及断层破裂,可以以不同的速度传播.
- 超级破裂,超过地震波的速度,是大地震中的一个关键现象.
- 了解破裂动态对于地震危险评估至关重要.
研究的目的:
- 为了实验地观察自发核化超级剪切裂变.
- 为了可视化从子雷利到超剪切裂变速度的过渡.
- 在实验室环境中调查促进超剪断破裂的条件.
主要方法:
- 实验室实验使用摩擦持有接口.
- 高速成像可视化破裂传播.
- 破裂动态和过渡机制的分析.
主要成果:
- 成功的实验观察了自发核化的超级剪切裂变.
- 从子雷利到超剪切破裂速度的过渡的可视化.
- 确定促进超剪裂传播的条件.
结论:
- 实验室实验可以复制复杂的地震破裂现象.
- 超剪切断裂过渡是可以观察到的,可以自发启动.
- 研究结果表明,超级剪切裂变可能发生在大型自然地震中.
相关概念视频
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The average shearing stress can be calculated by dividing the shear by the area of the cross-section.
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