SEISMOLOGY AND GEOLOGY ›› 2016, Vol. 38 ›› Issue (2): 278-289.DOI: 10.3969/j.issn.0253-4967.2016.02.004

• Research Paper • Previous Articles     Next Articles

COSEISMIC DISPLACEMENT AND FAULT SLIP OF THE MW6.1 NAPA EARTHQUAKE IN AMERICA REVEALED BY SENTINEL-1A INSAR DATA

ZUO Rong-hu, QU Chun-yan, ZHANG Guo-hong, SHAN Xin-jian, SONG Xiao-gang, WEN Shao-yan, XU Xiao-bo   

  1. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • Received:2015-03-30 Revised:2015-11-04 Online:2016-06-20 Published:2016-08-11

基于Sentinel-1A数据获取美国纳帕MW6.1地震同震形变场及断层滑动反演

左荣虎, 屈春燕, 张国宏, 单新建, 宋小刚, 温少妍, 徐小波   

  1. 中国地震局地质研究所, 地震动力学国家重点实验室, 北京 100029
  • 作者简介:左荣虎,男,1989年生,在读硕士研究生,主要研究方向为InSAR地壳形变观测研究,电话:010-62009024,E-mail:rh_zuo@163.com。
  • 基金资助:

    国家自然科学基金(41374015,41411011073)和地震动力学国家重点实验室课题(LED2015A03,LED2013A02)共同资助。

Abstract:

We achieved the coseismic displacements of the Napa MW6.1 earthquake located in California US occurring on 24 August 2014 by using InSAR data from the newly launched ESA's Sentinel-1A satellite. The 30m×30m ASTER GDEM was used to remove the terrain effect, and phase unwrapping method of branch-cut algorithm was adopted. In order to obtain a better coseismic displacement field, we also tested 90m×90m SRTM data to remove the terrain effect and Minimum Cost Flow algorithm to unwrap the phase. Results showed that the earthquake caused a significant ground displacement with maximum uplift and subsidence of 0.1m and -0.09m in the satellite light of sight(LOS). Based on the Sentinel-1A dataset and sensitivity based iterative fitting(SBIF) method of restrictive least-squares algorithm, we obtained coseismic fault slip distribution and part of the earthquake source parameters. Inversion results show that the strike angle is 341.3°, the dip angle is 80°, rupture is given right-lateral fault, average rake angle is -176.38°, and the maximum slip is ~0.8m at a depth of 4.43km. The accumulative seismic moment is up to 1.6×1018N·m, equivalent to a magnitude of MW6.14.

Key words: Sentinel-1A, Napa earthquake, D-InSAR, coseismic displacement, inversion

摘要:

利用欧洲空间局新发射的Sentinel-1A卫星获取的第1对同震SAR影像,采用30m×30m分辨率的ASTER GDEM数据去除地形效应,应用枝切法解缠,得到了2014年8月24日美国加利福尼亚州纳帕地震的地表同震形变场。为了获取最优同震形变场,对比使用了90m×90m分辨率的SRTM数据去除地形相位,以及最小费用流方法进行相位解缠。结果显示此次地震造成形变场在LOS方向(Line Of Sight)的最大抬升量和最大沉降量分别达到了0.1m和0.09m。基于获取的同震形变场,采用限制性最小二乘算法进行敏感性迭代拟合,获取了此次地震的断层滑动分布及部分震源参数。反演结果表明发震断层的走向为341.3°,倾角为80°,破裂以右旋走滑为主,平均滑动角为-176.38°,最大滑动量达0.8m,位于地表下约4.43km处。此次地震累计释放地震矩1.6×1018N·m,约合矩震级MW6.14。

关键词: Sentinel-1A, 纳帕地震, D-InSAR, 同震形变, 反演

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