| 2008年MS7.1于田地震InSAR同震形变场及其震源滑动反演 |
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| 引用本文： | 张国宏,屈春燕,单新建,张桂芳,宋小刚,汪荣江,李振洪,胡植庆.2008年MS7.1于田地震InSAR同震形变场及其震源滑动反演[J].地球物理学报,2011,54(11):2753-2760. |
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| 作者姓名： | 张国宏 屈春燕 单新建 张桂芳 宋小刚 汪荣江 李振洪 胡植庆 |
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| 作者单位： | 1. 地震动力学国家重点实验室,中国地震局地质研究所,北京 100029;
2. GFZ German Research Centre for Geosciences, Telegrafenberg, D-14473 Potsdam, Germany;
3. Department of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, United Kingdom;
4. 台湾大学地质科学系,台北 10617 |
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| 基金项目： | 中国地震局地质研究所基本科研业务专项(IGCEA0908、LED2008A06)、国家科技支撑计划(2008BAC35B04)、国家自然科学基金(40874006)项目共同资助. |
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| 摘 要： | 本研究利用InSAR技术与ALOS PALSAR雷达数据,获取了2008年3月20日于田MS7.1地震视线向同震形变场,并基于该数据集和限制性最小二乘算法反演了此次地震的断层滑动分布;通过构造四大类反演方案,详细分析了InSAR观测系统中的入射角与方位角对反演结果的影响.结果表明:入射角随点位变化对反演结果有较大影响,...
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| 关 键 词： | 于田地震 InSAR同震形变场 滑动分布反演 InSAR入射角 InSAR方位角 |
| 收稿时间： | 2011-01-31 |
The coseismic InSAR measurements of 2008 Yutian earthquake and its inversion for source parameters |
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| ZHANG Guo-Hong,QU Chun-Yan,SHAN Xin-Jian,ZHANG Gui-Fang,SONG Xiao-Gang,WANG Rong-Jiang,LI Zhen-Hong,HU Jyr-Ching.The coseismic InSAR measurements of 2008 Yutian earthquake and its inversion for source parameters[J].Chinese Journal of Geophysics,2011,54(11):2753-2760. |
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| Authors: | ZHANG Guo-Hong QU Chun-Yan SHAN Xin-Jian ZHANG Gui-Fang SONG Xiao-Gang WANG Rong-Jiang LI Zhen-Hong HU Jyr-Ching |
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| Institution: | 1. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
2. GFZ German Research Centre for Geosciences, Telegrafenberg, D-14473 Potsdam, Germany;
3. Department of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, United Kingdom;
4. Department of Geosciences, National Taiwan University, Taipei 10617, China |
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| Abstract: | 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 0~14 km depth and no evidence of shallow slip deficit. The inverted seismic moment M0 is 3.3×1019 N·m, equivalent to an event of magnitude MW7.0. |
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| Keywords: | Yutian earthquake Co-seismic deformation derived from InSAR Slip distribution inversion Incidence angle of InSAR Azimuth angle of InSAR |
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