在实验室中,自我愈合的脉冲状剪切断裂发生在实验室中
George Lykotrafitis1, Ares J Rosakis, Guruswami Ravichandran
1Graduate Aeronautical Laboratories, California Institute of Technology, Pasadena, CA 91125, USA.
概括
研究人员可视化了地震断层破裂模式,观察了裂纹状和自我修复的滑动脉冲. 他们确定了影响这些动态剪切断裂行为的条件,进步了我们对地震事件的理解.
科学领域:
- 地质物理学 地质物理学
- 固体力学 固体力学是什么
- 实验物理实验物理学
背景情况:
- 地震断层模型预测了两个主要的动态剪切断裂模式:滑动裂和自我修复的滑动脉冲.
- 了解支配这些破裂模式的条件对于地震危险评估至关重要.
研究的目的:
- 通过实验可视化和描述裂纹状,脉冲状和混合动态剪切破裂模式.
- 确定在"不连贯"接口上发展不同的破裂模式的特定条件.
主要方法:
- 采用动态光弹性和激光干扰测量来进行同时测量.
- 在相同的固体之间的摩擦性"不连贯"接口上可视化破裂的传播.
主要成果:
- 在实验中观察并区分了裂纹状,脉冲状和混合破裂模式.
- 确定破裂模式类型,启动点,滑动速度历史和传播速度.
结论:
- 实验证据支持存在不同的类似裂和类似脉冲的动态剪切破裂模式.
- 该研究提供了一个框架,以理解基于接口属性和条件的不同破裂模式之间的过渡.
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