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一个超导重力计网络检测了微小的地震重力变化
Yuichi Imanishi1, Tadahiro Sato, Toshihiro Higashi
1Ocean Research Institute, University of Tokyo, 1-15-1, Minamidai, Nakano, Tokyo 164-8639, Japan. imanishi@ori.u-tokyo.ac.jp
高分辨率的重力记录在大地震后检测到重力加速度的永久变化. 这些使用超导引力计测量的发现与理论模型一致,并推进了对地构造过程的研究.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
背景情况:
- 地震引起的地变形会导致可测量的重力变化.
- 高精度的重力测量对于检测微妙的地球物理信号至关重要.
研究的目的:
- 在大地震后检测和量化永久性的重力加速度变化.
- 用精确的重力数据验证位移模型.
主要方法:
- 利用一个区域网络的高分辨率连续超导引力计.
- 分析了重力记录,以确定地震后的永久加速转移.
主要成果:
- 检测到的永久重力加速度变化小于10(-8) m/s2 (1微型利略).
- 观察到的重力变化与脱位建模中的理论值非常相匹配.
结论:
- 超导重力测量在检测地震引起的重力变化方面是有效的.
- 这种技术可以有助于理解构造过程中的世俗重力变化.
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