缓慢滑落和流体诱导的地震群的平行动态
Philippe Danré1, Louis De Barros2, Frédéric Cappa2
1Université Côte d'Azur, CNRS, Observatoire de la Côte d'Azur, IRD, Géoazur, Sophia Antipolis, Valbonne, France. philippe.danre@geoazur.unice.fr.
Nature communications
|October 16, 2024
概括
地震群是由液体或缓慢滑动驱动的. 分析迁移的地震序列揭示了不同的缩放规律,有助于区分流体诱导和缓慢滑动驱动的地震活动.
科学领域:
- * 地震学 关于地震的研究
- * 构造物理学 构造物理学
- * 地质系统中的流体动力学
背景情况:
- *地震群是地震事件的序列,通常缺乏明确的主震.
- * 低中心迁移是群体中常见的特征,可能表明潜在的物理过程.
- * 区分液体诱导和无地震滑动作为群体驱动器对于危险评估至关重要.
研究的目的:
- * 分析移动地震序列的全球数据.
- * 识别和比较迁移速度,时刻和持续时间的缩放规律.
- * 为了区分液体诱导和缓慢滑动驱动的地震群.
主要方法:
- *编制和分析移动地震序列的全球数据集.
- *对低中心迁移模式的统计分析.
- *确定迁移速度,地震时刻和事件持续时间之间的缩放关系.
主要成果:
- * 在迁移序列中发现了两种不同的行为模式.
- * 与缓慢滑动事件相比,液体诱导的群体的迁移速度和时刻较低.
- * 在流体驱动和缓慢滑动驱动的地震序列之间,缩放规律显著不同.
结论:
- *这项研究提供了衡量标准,以区分地震群的驱动机制.
- * 已识别的缩放定律为断层滑动瞬态的物理提供了洞察力.
- *这些发现促使重新评估已建立的缩放规律,特别是对于群体地震性.
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