非常远程的动态触发泥火山动荡和静默的6级断层滑动
Zaur Bayramov1,2, Renier Viltres1, Cécile Doubre1
1Institut Terre et Environnement de Strasbourg UMR 7063, Université de Strasbourg, CNRS, Strasbourg, France.
概括
大规模地震引发了泥火山爆发和1000公里远的库拉盆地断层滑坡. 地震波可能改变了深层孔隙压力,造成了这种广泛的地质变形事件.
科学领域:
- 地质学
- 构造学
- 地震学
背景情况:
- 大规模的地震可以远程触发地质事件,
- 需要进一步调查地震波与富含液体的盆地之间的相互作用.
研究的目的:
- 研究远方地震波对地质结构的触发机制.
- 分析2023年卡拉曼马拉斯地震对库拉盆地的影响.
主要方法:
- 使用干涉测量合成光圈雷达 (InSAR) 来绘制变形图.
- 综合当地地质和地震数据进行综合分析.
- 分析了库拉盆地的地震和后地震反应.
主要成果:
- 在56个泥火山观察到变形和/或喷发.
- 在几十公里的七个断层中检测到厘米级的无地震滑动.
- 在碳化合物田下发现局部通胀.
- 标志着相当于6.1级的短暂变形事件.
结论:
- 卡拉曼马拉斯地震的地震波导致库拉盆地发生了重大地质变形.
- 由地震波引发的深度孔压力变化是无地震滑落和泥火山活动的可能原因.
- 这项研究强调了遥远的地震事件与涉及流体的地质系统之间的复杂相互作用.
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