在智利发生的2015年8.3兆瓦的伊拉佩尔地震之后,快速重新安置和后滑地震的演变
Joaquín Hormazábal1, Marcos Moreno2,3, Francisco Ortega-Culaciati1,4
1Department of Geophysics, Faculty of Physical and Mathematical Sciences, University of Chile, Santiago, Chile.
Scientific reports
|November 9, 2023
概括
在2015年伊拉佩尔地震之后,使用GNSS数据研究了后滑和重新锁定过程. 在主要破裂区的快速重新锁定表明持续的度,可能解释定期的地震复发.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 大型俯冲地震会导致复杂的地震后变形,因为后滑和粘弹性放松.
- 区分这些信号与板间重新锁定是具有挑战性的.
- 2015年伊拉佩尔地震为后地震过程提供了一个案例研究.
研究的目的:
- 为了研究2015年伊拉佩尔地震后的后滑,地震性和锁定的时空演变.
- 了解后滑,放松和重新锁定之间的相互作用.
- 确定特定度在地震复发中的作用.
主要方法:
- 对全球导航卫星系统 (GNSS) 连续6年测量 (2015-2021) 的分析.
- 来自地震后位移的余滑的逆转,以非线性粘弹性放松 (强度定律形学) 为准.
- 从GNSS站的线性趋势中确定锁定分布.
主要成果:
- 后滑集中的两个区域围绕主要的地震滑动区域,积累超过1.5米.
- 余震主要发生在余震区域的边界.
- 最大的地震滑动区域显示了快速的重新定位,作为持续的速度减弱度,没有观察到的余震或余震.
结论:
- 主破裂区的快速重新定位可能决定该地区大地震的定期复发间隔.
- 了解后地震变形对于地震危险评估至关重要.
- 这项研究强调了潜水带地震后果的复杂但可预测的性质.
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