The coseismic InSAR measurements of 2008 Yutian earthquake and its inversion for source parameters

被引:13
作者
Zhang Guo-Hong [1 ]
Qu Chun-Yan [1 ]
Shan Xin-Jian [1 ]
Zhang Gui-Fang [1 ]
Song Xiao-Gang [1 ]
Wang Rong-Jiang [2 ]
Li Zhen-Hong [3 ]
Hu Jyr-Ching [4 ]
机构
[1] China Earthquake Adm, Inst Geol, State Key Lab Earthquake Dynam, Beijing 100029, Peoples R China
[2] GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany
[3] Univ Glasgow, Dept Geog & Earth Sci, Glasgow G12 8QQ, Lanark, Scotland
[4] Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2011年 / 54卷 / 11期
关键词
Yutian earthquake; Co-seismic deformation derived from InSAR; Slip distribution inversion; Incidence angle of InSAR; Azimuth angle of InSAR; 7.1 HECTOR MINE; SLIP DISTRIBUTION; JOINT INVERSION; FAULT SLIP; DEFORMATION; GPS; RADAR; CALIFORNIA; MODEL; FIELD;
D O I
10.3969/j.issn.0001-5733.2011.11.005
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We have obtained the coseismic deformation along line of sight of the 2008 Yutian earthquake, using ALOS PALSAR images and SAR interferomety technique.. Based on the InSAR measurements and the constrained least square method, we studied the source parameters of this big normal event. Four schemes of inversion were constructed, with the emphasis on the effect to slip distribution inversion of the incidence angle and azimuth angle. Our inversion results show that the incidence angle has certain effect on the slip distribution, which means that a substitution of location-dependant incidence angle with constant mean incidence angle will lose some useful slip distribution on fault plane. Our inversion also shows the azimuth angle, however, has almost no obvious effect and it is an optimal choice to use the mean azimuth angle. Our most robust slip distribution can be obtained with the two parameters being location-dependant. In our favored inversion scheme using location dependant angles for both, the maximum slip reaches 3. 2m. Slip is mainly confined to 0 similar to 14 km depth and no evidence of shallow slip deficit. The inverted seismic moment M-0 is 3. 3 X 10(19) N . m, equivalent to an event of magnitude M(w)7. 0.
引用
收藏
页码:2753 / 2760
页数:8
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