梁明^1,2,,
王武星^1,,,
张晶¹
1. 中国地震局地震预测重点实验室(中国地震局地震预测研究所), 北京 100036
2. 广东省地震局, 广州 510070

基金项目: 国家自然科学基金项目（41331066，41274098）和地震行业科研专项（201508010）资助


详细信息

作者简介: 梁明, 男, 1991年生, 硕士研究生, 从事GPS和卫星重力资料的地球动力学应用研究.E-mail:lm1324308612@163.com

通讯作者: 王武星, 男, 1975年生, 研究员, 主要从事大地测量资料的地球动力学应用研究.E-mail:bkwwx@seis.ac.cn

中图分类号: P228;P315

收稿日期:2017-06-11
修回日期:2017-11-28
上线日期:2018-07-05

Post-seismic deformation mechanism of the M_W9.0 Tohoku-Oki earthquake detected by GPS and GRACE observations

LIANG Ming^1,2,,
WANG WuXing^1,,,
ZHANG Jing¹
1. Key Laboratory of Earthquake Prediction, Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, China
2. Guangdong Earthquake Agency, Guangzhou 510070, China


More Information

Corresponding author: WANG WuXing,E-mail:bkwwx@seis.ac.cn

MSC: P228;P315

--> Received Date: 11 June 2017
Revised Date: 28 November 2017
Available Online: 05 July 2018


摘要
摘要:利用GPS和GRACE观测数据研究了日本M_W9.0地震的震后变形特征.GPS观测显示，区域震后位移呈现随指数函数变化特征，变化速率符合大森公式的衰减特性；近五年的震后水平位移累积已达到东向60~165 cm，南向20~65 cm的量值，距震中较远站点已超过同震变化量，且震后变形仍然持续.GRACE观测到显著的震后重力变化，地震破裂两侧的重力变化总体均呈上升趋势，但海洋侧的变化速率较快.联合震后余滑和黏弹性位错理论对震后变形进行了模拟，探索了GPS和GRACE观测的综合应用方法.研究发现，综合考虑震后余滑和黏滞性松弛效应可以对日本地震的震后变形做出较合理的解释，震后初期余滑起主要作用，1至2年以后逐渐减弱，黏滞性松弛作用逐渐增强.在震后变形模拟和区域黏滞性结构反演中形成GPS和GRACE观测结合应用的方法，先基于震后GPS形变估算区域黏滞性结构，而后利用GRACE观测修正深部的黏滞系数，并综合利用这两种观测微调浅层黏滞系数，最终确定区域黏滞性结构.基于该方法反演了日本震源区的地幔黏滞性结构，地震断层破裂两侧的流变参数存在差异，大陆侧的地幔顶层黏滞系数在1.0×10¹⁹ Pa·s量级，而海洋侧的则略小于大陆的，在6.0×10¹⁸ Pa·s量级.
关键词: GPS/
GRACE/
震后变形/
震后余滑/
黏滞性松弛

Abstract:Post-seismic deformation characteristics of the M_W9.0 Tohoku-Oki earthquake are studied by using GPS and GRACE observations. GPS continuous observations show that the regional post-seismic displacements are characterized by exponential function, and the rate of change accords with the attenuation characteristic of the Omori formula. Post-seismic horizontal displacements accumulated to 60~165 cm for the east components, and 20~65 cm for the south components, in nearly 5 years following the main shock, until December 2015. For GPS sites further away from the epicenter, post-seismic displacements have exceeded their co-seismic changes. Moreover, their post-seismic deformations are still continuing. Significant post-seismic gravity changes are detected by GRACE also, which shows that gravity rises on both sides of the seismic rupture. However, the rate of gravity change is faster on the ocean side. Here we combine the theories of afterslip and viscoelastic dislocation to simulate the post-seismic deformations and explore the comprehensive application of GPS and GRACE observations. The results demonstrate the combination of afterslip and viscoelastic relaxation theories can make a reasonable explanation for the post-seismic deformations of the M_W9.0 Tohoku-Oki earthquake. The contribution of afterslip plays a major role in the initial stage, and it gradually weakens one or two years later, while the contribution of viscoelastic relaxation increases with time. The method of combining GPS and GRACE observations is formed in the simulation. Firstly, determine a preliminary regional viscous structure by inversion of post-seismic GPS observation, then modify the viscosity of the deepest layer according to GRACE observation, and fine tune the viscosity of the shallower layer by synthetically using GPS and GRACE observations. Finally, determine the regional viscous structure. Based on this method, we estimated the mantle viscous structure in the region of the M_W9.0 Tohoku-Oki earthquake by GPS and GRACE observations. The simulation results show that the rheological parameters are different on the two sides of the fault. The viscosity of the top mantle on the continental side is of the order of 1.0×10¹⁹ Pa·s, while that on the ocean side is of the order of 6.0×10¹⁸ Pa·s.
Key words:GPS/
GRACE/
Post-seismic deformation/
Afterslip/
Viscoelastic relaxation



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