| 用钻孔应变数据探测2011年日本Tohoku大地震激发的低频地球环型自由振荡及其谱峰分裂 |
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| 引用本文： | 张赓, 徐建桥, 陈晓东, 张凌云, 孙和平, 龚立卓. 2024. 用钻孔应变数据探测2011年日本Tohoku大地震激发的低频地球环型自由振荡及其谱峰分裂. 地球物理学报, 67(4): 1383-1397, doi: 10.6038/cjg2023Q0551 |
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| 作者姓名： | 张赓 徐建桥 陈晓东 张凌云 孙和平 龚立卓 |
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| 作者单位： | 1. 中国科学院精密测量科学与技术创新研究院, 大地测量与地球动力学国家重点实验室, 武汉 430077; 2. 中国科学院大学, 地球与行星科学学院, 北京 100049; 3. 华北理工大学矿业工程学院, 河北唐山 063210 |
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| 基金项目： | 中国科学院战略性先导科技专项(B类)(XDB41000000), 国家自然科学基金(42174101, 42192535, 41974023, 42004075), 湖北珞珈实验室专项基金(S22H640201)资助 |
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| 摘 要： | 地震激发的地球自由振荡中, 环型自由振荡(特别是低频环型自由振荡)的精确探测相比于球型自由振荡更加困难. 环型自由振荡对SH波速度结构更加敏感, 能更好地监测走滑断层运动, 因此精确估算环型自由振荡的谱峰参数可为地球内部大尺度SH波速度结构和大地震的震源机制提供更强约束. 本研究利用2011年日本Tohoku地震后四分量钻孔应变仪的观测资料, 提取了该地震激发的1.3 mHz以下低频环型和球型自由振荡信号, 与STS-1宽频带地震仪的结果相比较, 发现四分量钻孔应变仪对1 mHz以下的环型自由振荡具有更强的探测能力. 本研究还采用频率域自回归方法精确估计了0T2—0T6的简并频率, 结果与PREM模型理论值相差非常小, 平均相对误差仅为2.52×10-4.此外还用钻孔应变仪观测资料探测到了0T2谱峰分裂现象. 研究结果表明, 钻孔应变仪能有效探测到大地震激发的低频地球环型自由振荡信号, 可为地幔大尺度各向异性结构研究提供高质量的基础数据.
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| 关 键 词： | 环型自由振荡 钻孔应变仪 Tohoku地震 简正模谱峰分裂 STS-1地震仪 |
| 收稿时间： | 2022-07-11 |
| 修稿时间： | 2023-02-19 |
Probing low-frequency toroidal free oscillations and their splitting excited by the 2011 Tohoku,Japan earthquake using observations of borehole strainmeters |
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| ZHANG Geng, XU JianQiao, CHEN XiaoDong, ZHANG LingYun, SUN HePing, GONG LiZhuo. 2024. Probing low-frequency toroidal free oscillations and their splitting excited by the 2011 Tohoku, Japan earthquake using observations of borehole strainmeters. Chinese Journal of Geophysics (in Chinese), 67(4): 1383-1397, doi: 10.6038/cjg2023Q0551 |
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| Authors: | ZHANG Geng XU JianQiao CHEN XiaoDong ZHANG LingYun SUN HePing GONG LiZhuo |
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| Affiliation: | 1. State Key Laboratory of Geodesy and Earth's Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430077, China; 2. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China; 3. Mining Engineering College, North China University of Science and Technology, Tangshan Hebei 063210, China |
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| Abstract: | Toroidal free oscillations (especially the low-frequency toroidal modes) excited by earthquakes are much more difficult to be detected comparing with the spheroidal modes. However, toroidal modes are sensitive to SH waves and can be used to monitor the lateral movement of faults. Therefore, the accurate estimation of toroidal modes provides more constraints on the large-scale SH-wave velocity structure of the earth's interior and the focal mechanism of large earthquakes. Using observations of 4-component borehole strainmeters, low-frequency toroidal modes and spheroidal modes below 1.3 mHz excited by the 2011 Tohoku, Japan earthquake are extracted in this study. The results indicate that the 4-component borehole strainmeters have better detectability for toroidal modes below 1 mHz compared to the STS-1 broadband seismometers. The degenerate frequencies of the low-frequency toroidal modes 0T2—0T6 are accurately estimated with the autoregressive method in frequency domain. The estimated values are close to the PREM theoretical values with an average relative error of 2.52×10-4. In addition, the mode splitting of 0T2 is detected using the borehole strainmeter data. Our results demonstrate that the borehole strainmeters can effectively detect signals of low-frequency toroidal modes excited by large earthquakes, and then provide high-quality basic data for the investigation of the large-scale anisotropic structure of the mantle. |
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| Keywords: | Toroidal free oscillations Borehole strainmeter Tohoku earthquake Normal mode splitting STS-1 seismometer |
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