附近断层的变形是由1999年赫克多矿山地震引起的
Yuri Fialko1, David Sandwell, Duncan Agnew
1Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USA. fialko@radar.ucsd.edu
概括
交叉测量合成孔径雷达 (ISAR) 在1999年赫克托矿区地震期间揭示了断层运动. 断层区域表现出明显的机械性能,弹性地对地震应力变化作出反应.
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
- 遥感 遥感 遥感 遥感
背景情况:
- 1999年赫克托矿区地震造成了显著的表面变形.
- 了解地震事件期间的断层行为对于地震危险评估至关重要.
研究的目的:
- 分析与1999年赫克托矿山地震相关的表面变形模式,使用交叉测量合成孔径雷达 (ISAR).
- 调查在加利福尼亚州东部剪切区域内断层区域的机械特性.
主要方法:
- 使用交叉测量合成孔径雷达 (ISAR) 来观察表面移位.
- 分析了跨越千米宽的断层区域的垂直和水平运动.
主要成果:
- 观察到主要断裂附近多个断层的毫米到厘米的位移.
- 记录了一些断层部分的逆行运动,与长期的地质滑动相反.
- 在断层区域内推断降低了有效切割模量,这表明它们与周围地有机械区别.
结论:
- 断层区域表现出顺服的行为,弹性地响应共同地震应力变化.
- 观察到的位移表明,与周围地相比,断层区域是机械上独特的结构.
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