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基于Sentinel-1A数据反演2015年新疆皮山MW6.5地震断层滑动分布
引用本文:韩颖颖,曾浩炜,吴康良,韦 耐.基于Sentinel-1A数据反演2015年新疆皮山MW6.5地震断层滑动分布[J].大地测量与地球动力学,2017,37(6):590-593.
作者姓名:韩颖颖  曾浩炜  吴康良  韦 耐
摘    要:使用Sentinel-1A卫星观测的2015年新疆皮山地震震前震后一对SAR影像,提取该地震的同震形变场。结合Okada位错模型,在考虑渐变入射角和解缠基准偏差的情况下,反演本次地震的断层滑动分布。结果表明,皮山地震是小倾角逆冲型地震,断层破裂开始于地表以下约5 km处,最大滑动量为0.76 m,高滑区集中于深度9~14 km,累计释放地震矩达5.14×1018,相当于矩阵级MW6.47。

关 键 词:皮山地震  Sentinel-1A  同震形变场  断层滑动分布  

Fault Slip Distribution of 2015 MW6.5 Pishan,Xijiang Earthquake Inversed from Sentinel-1A Data
HAN Yingying,ZENG Haowei,WU Kangliang,WEI Nai.Fault Slip Distribution of 2015 MW6.5 Pishan,Xijiang Earthquake Inversed from Sentinel-1A Data[J].Journal of Geodesy and Geodynamics,2017,37(6):590-593.
Authors:HAN Yingying  ZENG Haowei  WU Kangliang  WEI Nai
Abstract:In this study, a pair of SAR imagestaken before and after the Pishan earthquake acquired from the Sentinel-1A satellite are used to extract the coseismic deformation field. Based on the above coseismic deformation field and the Okada model, considering the varying incidence angle and unwrapping datum error, we inverse the fault slip distribution of this earthquake. The inversion results indicate that the Pishan earthquake is a thrust earthquake with smaller dip, the fault ruptures 5 km under the surface, and the maximum slip is about 0.76 m, and the main slip area is at the depth of 9-14 km. The estimated seismic moment is 5.14×1018, approximately equivalent to the magnitude of MW6.47.
Keywords:Pishan earthquake  Sentinel-1A  coseismic deformation  fault slip distribution  
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