粘弹性滑动块作为地震性断层的模型
Charlotte A Motuzas1,2, Robert Shcherbakov1,2
1Department of Earth Sciences, Western University, London, ON N6A 5B7, Canada.
Entropy (Basel, Switzerland)
|October 28, 2023
概括
这项研究引入了一种模拟地震事件的新模型,揭示了粘性弹性如何影响断层动态和余震模式. 这些发现表明,比在自然地震序列中观察到的更快的余震衰变.
科学领域:
- 地质物理学 地质物理学
- 计算地震学计算地震学
- 地震科学 地震科学 地震科学
背景情况:
- 了解地震生成和余震序列对于地震危险评估至关重要.
- 在断层动态中地粘弹性的作用仍然是活跃的研究领域.
- 地球地中的非线性过程显著影响地震事件模式.
研究的目的:
- 提出和检查一个模型,在模拟类似地震的事件中结合粘性弹性.
- 研究非线性地过程对地震触发和衰变的影响.
- 使用已建立的地震模型分析模拟的地震序列的行为.
主要方法:
- 用粘弹性标准线性固体 (SLS) 元素进行滑块故障模型的数值模拟.
- 对模拟的地震雪崩及其自我组织的关键性的分析.
- 应用流行型余震序列 (ETAS) 模型来分析模拟序列.
主要成果:
- 粘弹性滑块模型产生类似于自然地震序列的合成地震事件和雪崩.
- 流行型余震序列 (ETAS) 模型有效地表示模拟的触发和衰变模式.
- 模拟的余震序列的p值略大,表明衰变速度比自然序列更快.
结论:
- 在断裂模型中包含粘弹性类风学得到了现实的模拟频率大小分布和ETAS匹配的支持.
- 该模型提供了关于粘弹性特性如何影响地震序列动态的见解.
- 在ETAS参数估计中的偏差凸显了模拟和自然地震系统之间的潜在差异.
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