概括
一个缓慢的变形前体,相当于7.6级地震,在1989年麦奎里山脊地震之前发生. 这种缓慢的事件引发了主要冲击,这表明海洋上层地幔的复合破裂过程.
科学领域:
- 地震学 地震学
- 地震物理学的地震物理学
- 地质物理学 地质物理学
背景情况:
- 1989年马奎里山脊地震 (Mw 8.2) 是一个主要的地震事件.
- 了解地震前体对于地震危险评估至关重要.
研究的目的:
- 为了研究1989年麦考里山脊地震的低频地震光谱.
- 为了识别主要冲击之前的潜在前体现象.
主要方法:
- 分析来自1989年麦奎里山脊地震的低频地震光谱 (<6毫赫).
- 建模地震作为一个复合事件,涉及缓慢变形.
主要成果:
- 观察到的振幅增加和相延迟降低到6mHz以下表明短期缓慢的前体.
- 缓慢的前体释放了~3 x 10^20 Nm (Mw 7.6) 的时刻.
- 前体可能启动了主要破裂,这表明一个复合事件.
结论:
- 1989年麦奎里山脊地震之前发生了一次显著的缓慢变形事件.
- 这种缓慢的前体起源于海洋上层地幔,位于主要破裂区以下.
- 地震可以从缓慢的变形事件开始,挑战传统的破裂模型.
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