意大利中部一群地震造成的缓慢地震动态受到限制
1Dipartimento di Scienze della Terra, Universita di Camerino, Camerino (MC), Italy. Istituto Nazionale di Fision Nucleare-Laboratori Nazionali del Gran Sasso (LNGS), L'Aquila, Italy. Dipartimento di Fisica, Universita di L'Aqui.
概括
研究人员在意大利观察到缓慢的地震. 这些事件的地震时刻与它们的上升时间的平方根相比例,这表明类似于热扩散的缓慢破裂传播.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
背景情况:
- 缓慢的地震是地震事件,其特点是长时间的破裂时间.
- 了解它们的机制对于地震危险评估至关重要.
研究的目的:
- 分析意大利中部集群缓慢地震的特征.
- 调查地震时刻和这些事件的起伏时间之间的关系.
主要方法:
- 使用地质干扰仪记录地震数据.
- 分析了记录事件的应变升高时间和地震时刻.
主要成果:
- 记录了几次集群缓慢的地震.
- 观察到地震时刻与上升时间的平方根相成比例.
- 压力上升时间从几十秒到数千秒不等.
结论:
- 观察到的缩放定律挑战了传统的故障建模假设.
- 结果支持一种类似于热扩散的缓慢破裂传播模型.
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