大喜马拉雅地震和西藏高原的地震
1CIRES and Department of Geological Sciences, University of Colorado, Boulder, Colorado 80309, USA.
Nature
|November 10, 2006
概括
喜马拉雅地震是由西藏高原的压缩应变驱动的,而不仅仅是大喜马拉雅. 这一发现有助于估计地震更新时间,并了解断裂模式.
科学领域:
- * 地震学 关于地震的研究
- * * 地质物理学
- * 构造学 构造学 构造学
背景情况:
- * 传统模型将喜马拉雅地震归因于大喜马拉雅附近的压缩应变.
- *最近的地震成像揭示了印度亚洲碰撞区的复杂地表几何结构.
研究的目的:
- * 调查西藏高原在推动喜马拉雅大地震中的作用.
- * 改进对地震断裂动态和复发间隔的理解.
主要方法:
- * 印度-亚洲碰撞弹性模型的开发和应用.
- *最近成像的地下界面几何体的整合.
- * 模型预测与最近喜马拉雅地震数据的比较.
主要成果:
- * 西藏南部高原的很大一部分有助于推动喜马拉雅山脉的巨大破裂.
- * 西藏弹性应变能量释放与喜马拉雅断裂长度成比例.
- *地震滑动和强度与断裂区域相关,这表明更新时间为500年.
- *模型解释了重裂事件和发生长时间的超级地震的发生.
结论:
- * 西藏南部高原是推动喜马拉雅地震的应变能量的一个关键储存库.
- *这些发现为了解该地区地震复发和断裂行为提供了新的框架.
- *弹性模型提供了对板块边界令人费解的地震性模式的见解.
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