2010年,智利中部发生了8.8兆瓦的莫尔巨型地震,GPS监测
1Laboratoire de Géologie de l'Ecole Normale Supérieure, UMR CNRS 8538, Paris, France. vigny@biotite.ens.fr
概括
2010年马尔地震造成了显著的地变形,滑坡集中在断层度上,延伸到浅处. 后滑发生在低地震滑动的地方,这表明复杂的断裂动态.
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:
- 大规模的地震会产生地变形,可通过地测技术进行测量.
- 了解断层滑坡分布对于地震危险评估至关重要.
研究的目的:
- 使用GPS数据推断2010年8.8兆瓦马尔巨型地震的静态变形和动力学.
- 为了确定毛尔地震的滑动分布和破裂特征.
主要方法:
- 利用智利中部的全球定位系统 (GPS) 网络数据.
- 应用弹性建模来推断断裂滑落和变形.
- 使用低频数据重新定位了地震的低中心.
主要成果:
- 破裂延伸约500公里,滑坡高达15米,集中在两个度上.
- 破裂到达浅处,可能延伸到沟.
- 在低地震滑坡的地区观察到后滑坡;低震中心迁移40公里西南.
结论:
- 毛尔地震表现出复杂的破裂行为,其中含有浅滑和显著的后滑.
- 破裂以~3.1公里/秒的速度在双边传播,这表明了对巨型冲击地震动态的详细理解.
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