超级剪切地震的余震签名超级剪切地震的余震签名
Michel Bouchon1, Hayrullah Karabulut
1Centre National de la Recherche Scientifique et Université Joseph Fourier, Grenoble, Laboratoire de Géophysique Interne et Tectonophysique, Boîte Postale 53, 38041 Grenoble, France. Michel.Bouchon@ujf-grenoble.fr
概括
超级听力地震,破裂速度快于地震波,产生冲击波,增加破坏. 这些地震显示安静的断层,但由于冲击波的冲击波,余震聚集在断层之外.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地震科学 地震科学 地震科学
背景情况:
- 地震断层可以以超过剪切波速度的速度破裂 (超剪切破裂).
- 超级剪切断裂产生地震冲击波,类似于声波爆炸,可能增加地震破坏.
- 超级剪切地震的地震行为和余震模式尚未完全理解.
研究的目的:
- 描述与超级剪切地震相关的余震模式.
- 为了研究超级剪切裂变动态和地震波辐射之间的关系.
- 了解超剪断破裂对地震危险评估的影响.
主要方法:
- 对地震数据的分析,以确定超级剪切裂变事件.
- 与主要断层平面相对应的余震分布的映射和统计分析.
- 对地震冲击波传播和周围岩石压力积累的建模.
主要成果:
- 超级震级地震表现出一个明显的余震模式:断层平面本身的静止.
- 余震主要集中在位于主断层之外的二次结构上.
- 观察到的模式表明,在超切断断段沿着均摩擦,以及在断层外的冲击波所产生的应力度.
结论:
- 超尖地震的特点是不寻常的地震特征:一个安静的断层平面与断层外的余震集群.
- 超级剪切破裂产生的地震冲击波在激活二次结构和影响余震分布方面发挥着至关重要的作用.
- 了解这些模式对于改善地震风险模型和预测地震影响至关重要.
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