2011年东北地震后粘弹性放松的发生率
Tianhaozhe Sun1, Kelin Wang2, Takeshi Iinuma3
1School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia V8P 5C2, Canada.
Nature
|September 19, 2014
概括
大地震后的地震后变形主要是由粘弹性放松驱动的,而不仅仅是后滑. 新的海底GPS数据揭示了这种在短期运动中的主导作用,挑战了关于断层行为和地球的先前假设.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造物理学 构造物理学
背景情况:
- 俯冲地震后的地震后变形是复杂的,受粘弹性放松和后滑的影响.
- 之前的研究经常假设滑过后会主导短期变形,粘性弹性只在长期发挥作用.
- 通过传统的地质数据来测试这一假设是具有挑战性的.
研究的目的:
- 为了研究导致东北大震后短期地震后变形的主导机制.
- 为了评估粘弹性放松与后滑在重大沉降事件发生后的作用.
- 根据新的观测数据重新评估故障行为模型.
主要方法:
- 全球定位系统 (GPS) 在东北地震发生后立即获得的新海底观测结果的分析.
- 开发和应用数值模型模拟过渡粘弹性地幔形学.
- 观察到的变形模式与模型预测的比较.
主要成果:
- 对于粘弹性放松在短期地震后变形中发挥主导作用的明确证据.
- 观测到沟区域的快速向陆地移动,与陆地向海移动形成鲜明对比.
- 证明了陆地向上的运动是由于不对称的地震破裂而导致的应力放松的结果.
结论:
- 粘弹性放松是短期地震后变形的关键因素,与此前的假设相反.
- 这些发现需要对模型进行修订,这些模型高估了下降后滑动,低估了上升后滑动.
- 了解断层摩擦需要纳入粘弹性对变形模式的显著影响.
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