2010年8月8日智利地震造成的土地水平变化
Marcelo Farías1, Gabriel Vargas, Andrés Tassara
1Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile. mfarias@dgf.uchile.cl
概括
2010年智利地震 (Mw 8.8) 在500公里的海岸线上造成了显著的陆地水平变化. 升起发生在一个链线的西部,而沉降发生在东部.
科学领域:
- 地质测量是指地质测量.
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 2010年智利地震 (Mw 8.8) 是一个具有重大地质后果的重大地震事件.
- 沿海和河流标记为地震造成的陆地水平变化提供了关键证据.
研究的目的:
- 为了记录和分析2010年智利地震后的地面水平的垂直变化.
- 为了确定共同地震移位的程度和模式.
- 为了模拟地震的破裂和能量释放.
主要方法:
- 垂直移位的沿海和河流标记物的现场观测.
- 分析大约500公里的土地水平变化.
- 应用一个简单的弹性脱位模型.
主要成果:
- 观察到标记物的垂直移位,范围从2.5到-1米.
- 确定了一个500公里长的段落作为最大长度的地震断裂.
- 位于距离沟沟120公里处的链线,将升起 (西部) 和下降 (东部) 的地区分开.
结论:
- 观察到的陆地平面变化与简单的弹性失位模型相一致.
- 模型参数表明,自1835年地震以来,有显著的弹性应变积累和释放.
- 2010年的事件可能释放了大部分储存的板块收能量.
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