在2011年东北9.0级地震的共地震滑动上方板块的控制
Dan Bassett1, David T Sandwell1, Yuri Fialko1
1Scripps Institution of Oceanography, La Jolla, California 92093, USA.
Nature
|March 4, 2016
概括
2011年东北地区地震
科学领域:
- 地质学
- 地震学
- 板块构造
背景情况:
- 2011年东北地震 (Mw ≥9.0) 提供了前所未有的地质数据.
- 了解控制巨型地震滑落和破裂程度的因素仍然是一个挑战.
研究的目的:
- 调查控制2011年东北地震破裂特征的地质结构.
- 在东北日本的巨型冲击地震行为上方板块结构相关联.
主要方法:
- 分析日本东北部的残余地形和重力异常.
- 重力建模,以确定重叠板的密度变化.
- 结构边界与历史地震和地震滑坡分布的相关性.
主要成果:
- 确定了一个离岸的结构边界, 很可能是中层构造线,
- 边界以北的巨大冲击被锁定,在2011年经历了显著的滑动 (> 40m).
- 边界以南的巨大冲击显示了地震间的爬行和2011年的小滑动.
结论:
- 上层板块的地质结构和推断的摩擦性质控制了巨型压力合.
- 中位构造线作为该地区地震行为的关键控制.
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