1992年加利福尼亚州登陆器地震后,地下部的粘弹性流动
1Seismological Laboratory 252-21, California Institute of Technology, Pasadena, CA 91125, USA.
概括
1992年Landers地震后的地震后变形是使用空间地质学建模的. 下层地中的粘弹性流解释了变形,为地震危险和盆地和范围结构提供了洞察力.
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:
- 在1992年兰德斯地震之后观察到大规模的地震后变形.
- 了解后地震变形对于地震危险评估至关重要.
研究的目的:
- 调查1992年兰德斯地震后推动地震后变形的机制.
- 为了建模后滑和粘弹性流向观察到变形的贡献.
主要方法:
- 利用太空地理测量数据观察大规模的地震后变形.
- 开发了三维模型来模拟变形过程.
- 估计了下层地层的粘度.
主要成果:
- 仅靠后滑就无法解释所有观察到的水平和垂直移位.
- 10公里厚的下层地层中的粘弹性流成功地解释了水平和近垂直的后地震变形.
- 这个弱层的粘度被确定为大约10^18帕斯卡秒.
结论:
- 低地中的粘弹性流是大地震后地震后反弹的主要机制.
- 这种机制可以解释盆地和山脉省的延伸结构.
- 这些发现有助于改进地震危险分析.
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