迷宫中的地震:压缩裂在2012年M(w) 8.6苏门答腊地震期间分支
1Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. lsmeng@gps.caltech.edu
概括
在2012年苏门答腊地震.
科学领域:
- 地震学 地震学
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
背景情况:
- 2012年苏门答腊发生的8.6级地震呈现出复杂的破裂动态.
- 之前的理解表明,沃顿盆地构造学被罢工滑动断层所主导.
研究的目的:
- 为了分析2012年苏门答腊地震的复杂破裂过程.
- 为了研究沃顿盆地的地震构造学.
主要方法:
- 地震学观察. 地震学观察.
- 背向投射源成像. 背向投射源成像.
- 动态库伦压力计算.
主要成果:
- 地震的大幅度是由深度,高压力下降和多个断层断裂造成的.
- 断裂发生在直角并联断层上,断裂速度缓慢.
- 断裂在东南东西西北方向传播,挑战了以前的模型.
- 断裂显示压缩分支与预测的方向相反.
结论:
- 破裂动态表明,深海石化层的压力不敏感强度控制了这种情况.
- 正角断层和不寻常的分支扩大了对沃顿盆地地震构造学的理解.
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