申文豪^1,,
李永生¹,
焦其松^1,,,
解全才²,
张景发¹
1. 中国地震局地壳应力研究所(地壳动力学重点实验室), 北京 100085
2. 中国地震局工程力学研究所(地震工程与工程振动重点实验室), 哈尔滨 150080

基金项目: 国家自然科学基金（41604041，41604040，41704051），中央级公益性科研院所基本科研业务专项（ZDJ2017-29，ZDJ2017-16，ZDJ2016-04）共同资助


详细信息

作者简介: 申文豪, 男, 助理研究员, 主要从事震源参数反演和强地面运动模拟等研究.E-mail:shenxiaoxi200212@163.com

通讯作者: 焦其松, 男, 助理研究员, 主要从事强震波形校正和地壳形变研究.E-mail:1985jqs@163.com

中图分类号: P315

收稿日期:2018-03-19
修回日期:2018-12-17
上线日期:2019-01-05

Joint inversion of strong motion and InSAR/GPS data for fault slip distribution of the Jiuzhaigou 7.0 earthquake and its application in seismology

SHEN WenHao^1,,
LI YongSheng¹,
JIAO QiSong^1,,,
XIE QuanCai²,
ZHANG JingFa¹
1. Key Laboratory of Crustal Dynamics, Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China
2. Key Laboratory of Earthquake Engineering and Engineering Vibration, Institute of Engineering Mechanics, China Earthquake Administration, Harbin 150080, China


More Information

Corresponding author: JIAO QiSong,E-mail:1985jqs@163.com

MSC: P315

--> Received Date: 19 March 2018
Revised Date: 17 December 2018
Available Online: 05 January 2019


摘要
摘要:2017年8月8日我国四川九寨沟发生里氏7.0级地震.本研究利用基线校正方法获得距震中100 km范围内9个强震台站同震位移，基于Sentinel-1卫星干涉SAR影像对获取了InSAR同震形变场.结合GPS形变数据，本研究进行了震源滑动模型联合反演，结果显示此次地震整体以走滑运动为主，释放地震矩约为7.60×10¹⁸N·m（~M_W6.52）.通过对比模拟形变场和观测值显示，联合反演结果优于单独基于InSAR形变场的反演结果.静态应力变化计算结果显示断层平均静态应力降为1.07 MPa.反演滑动模型沿走向和倾角方向拐角波数值分别为0.99×10^-4和1.10×10^-4.同震静态库仑应力变化计算结果显示共有83.6%的余震位于库仑应力增加的区域，被主震所触发的余震占总数的77.9%，主震对后续余震具有显著触发作用.强地面运动模拟结果显示模拟结果在烈度分布范围和等级方面与调查烈度符合度很高，模拟结果能够很好地反映断层破裂的方向性效应等特征.本研究计算结果显示九寨沟地震无论是平均静态应力降还是拐角波数均低于同类型地震的平均水平，这可能是造成本次地震强地震动水平相对不高的原因.
关键词: 九寨沟地震/
同震反演/
静态库仑应力变化/
强地面运动

Abstract:On August 8, 2017, an earthquake of M_S7.0 occurred at Jiuzhaigou, China. Based on the baseline correction method, coseismic displacement of 9 strong motion stations 100 km away from the epicenter are obtained. Also, the InSAR coseismic deformation field is derived from the Sentinel-1 satellite interference SAR images. Combined with GPS data, a joint inversion for the slip model of the source fault is carried out. Results show that the fault is dominated by strike slip, and the total released seismic moment is about 7.60×10¹⁸N·m, equivalent to an earthquake of M_W6.52. Results also demonstrate the joint inversion is better than the inversion from InSAR deformation alone comparing the simulated and the observed deformation field. Static stress calculation shows that the average static stress drop is 1.07 MPa, and corner wavenumbers of the slip model are 0.99×10^-4 and 1.10×10^-4 in strike and dip directions, respectively. Coulomb stress change calculation reveals that 83.6% of aftershocks are located in the positive Coulomb stress zone, 77.9% of total aftershocks may be triggered by the mainshock, indicating that the mainshock has a significant triggering effect on the subsequent aftershocks. The strong motion simulations permit to display basic features associated with the ground motion patterns. Moreover, the simulated results reflect the obvious rupture directivity effect. Both the average stress drop and corner wavenumber are at low levels which may be responsible for relatively weaker ground motion during the Jiuzhaigou earthquake.
Key words:Jiuzhaigou earthquake/
Coseismic inversion/
Static Coulomb stress change/
Strong ground motion



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