关于犹他州克兰德尔峡谷矿井倒塌的来源分析
Douglas S Dreger1, Sean R Ford, William R Walter
1Berkeley Seismological Laboratory, University of California, Berkeley, CA 94720, USA. dreger@seismo.berkeley.edu
概括
2007年犹他州的一次地震事件显示出了不寻常的辐射模式,表明了浅层地下崩而不是典型的构造地震. 地震时刻张量分析可以区分不同的地震源,如崩和地震.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
背景情况:
- 地震事件可以来自各种来源,包括构造地震和地下崩.
- 区分这些来源对于地震危险评估和监测至关重要.
研究的目的:
- 为了分析犹他州中部发生的3.9级地震的地震辐射模式.
- 为了确定地震事件的源机制.
- 评估地震动量张量分析对源类型歧视的实用性.
主要方法:
- 从3.9级地震事件的地震图分析.
- 使用地震时刻张量分析对地震事件进行建模.
- 将地震时刻张量结果与已知的核爆炸,矿山崩和构造地震的结果进行比较.
主要成果:
- 这次地震事件呈现出一种异常的辐射模式,其中占主导地位的是爆炸性成分,与构造地震不一致.
- 这一事件最好以浅层地下崩为模型.
- 确定了一个较小的非崩源组件,可能与断层或周围介质变形有关.
- 对于不同类型的源,观察到不同的地震时刻张量结果的不同种群.
结论:
- 地震时刻张量是一个有价值的工具,用于区分地震源类型,包括地下崩和构造地震.
- 分析的事件很可能是由浅层地下崩引起的,可能与相关的轻微断层有关.
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