远距离的S波微震
Kiwamu Nishida1, Ryota Takagi2
1Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi 1, Bunkyo-ku, Tokyo 113-0032, Japan. knishida@eri.u-tokyo.ac.jp.
概括
研究人员使用地震阵列追踪远方风暴的微地震. 他们观察到P和S波,但水平偏振的S波 (SH波) 仍然无法通过当前的模型来解释,为地球提供了新的见解
科学领域:
- 地震学
- 海洋学
- 地质学
背景情况:
- 微震,地震波的振动是由海洋的膨胀产生的.
- 追踪微震源位置对于理解激发机制至关重要.
研究的目的:
- 研究来自微地震的地震波组件 (P和S波) 的源位置和能量分区.
- 了解远处风暴产生的微震的激发机制.
主要方法:
- 在日本使用地震阵列观察微地震.
- 分析了来自大西洋暴风雨的P波和S波微震.
主要成果:
- 观察到的P波和垂直极化S波 (SV波) 与非线性海洋膨胀强迫相一致.
- 观测到的水平极化S波 (SH波) 无法通过当前的单维地球模型来解释.
结论:
- 目前的模型充分解释了P和SV波微震,但未能解释SH波.
- 精确的微震源位置有可能为探索地球内部创造一个新的目录.
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