大震荡地震周期和板块收之间的反.
Juan Martin de Blas1, Giampiero Iaffaldano2,3, Andrés Tassara4
1Department of Geosciences and Natural Resource Management, University of Copenhagen, Copenhagen, Denmark. jmb@ign.ku.dk.
Scientific reports
|October 31, 2023
概括
在安第斯大地震发生之前,板块运动会减缓. 这项研究表明,在大型巨型冲击事件发生之前的十年里,构造板块收率下降,这挑战了以前的假设.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地震学 地震学
背景情况:
- 安第斯山脉的地质形成是纳斯卡和南美板块数百万年来趋同的结果.
- 巨大的地震周期运行在十年/百年时间尺度上.
- 板块收率在地震周期中被认为是恒定的,尽管有长期反.
研究的目的:
- 为了调查纳斯卡/南美板块运动是否在一年/十年期间有所变化.
- 为了确定巨冲压应力变化是否会在地震周期中影响板块运动.
主要方法:
- 对纳斯卡和南美板块运动的地质数据的分析.
- 专注于在安第斯大陆发生重大大地震之前的十年 (2010年,2014年,2015年).
- 观察到的板块运动减速与来自地震间应力积累的扭矩变化的比较.
主要成果:
- 在纳斯卡和南美洲的整个板块运动中观察到放缓.
- 减速超过数据不确定性和噪声.
- 减速所需的扭矩变化与地震间应力积累相一致.
结论:
- 当代纳斯卡/南美板块运动在巨型冲击地震周期中并不稳定.
- 大地震之前的地震间应力积累会导致板块收率的可测量变化.
- 确定了大型冲击应力和板块运动之间的短期反机制.
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