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EARTHQUAKE ›› 2020, Vol. 40 ›› Issue (4): 76-89.doi: 10.12196/j.issn.1000-3274.2020.04.006

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Analysis of Coseismic Displacements due to the MW7.8 Nepal Earthquake Using InSAR Data and Inversion of Fault Slip Distribution

XU Xiao-bo1, MA Chao2, HONG Shun-ying3, LIAN Da-jun1, ZHANG Ying-feng4   

  1. 1. School of Environmental Science and Engineering, Suzhou University of Science and Technology, Suzhou 215009, China;
    2. School of Surveying and Land Information Engineering, Henan Polytechnic University, Jiaozuo 454000, China;
    3. Institute of Earthquake Forecasting, CEA, Beijing 100036, China;
    4. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • Received:2019-12-19 Online:2020-10-30 Published:2020-10-23

Abstract: The Nepal MW7.8 earthquake occurred on April 25, 2015. Based on Sentinel-1A SAR images before and after the earthquake, the coseismic deformation field was derived by D-InSAR method. InSAR observation results show that the coseismic deformation field was located near the Main Boundary Thrust Fault (MBT) and the Main Frontal Thrust Fault (MFT) in the Himalayan Orogenic Belt. The whole deformation field showed a spindle-shaped envelope extending about 150 km in length from northwest to southeast. The coseismic deformation is dominated by uplift in large area. The maximum uplift in line-of-sight (LOS) is 1.18m. There was a small subsidence area to the north of the uplift area. The maximum coseismic deformation center is obtained from InSAR deformation. Based on the Okada model and InSAR observations, we inverted the fault slip distribution. Inversion results show that the earthquake is a typical thrusting event. The main seismogenic fault is Main Himalayan Thrust Fault (MHT). And coseismic rupture is transmitted upward from Main Himalayan Thrust Fault (MHT) along Main Frontal Thrust Fault (MFT). In this paper, based on the details of InSAR coseismic deformation field, combined with the geological background, fault distribution and fault movement characteristics of the earthquake area, the preliminary interpretation and description of the pseudo coseismic fracture surface trace is completed.

Key words: 2015 Nepal MW7.8 earthquake, D-InSAR, Coseismic deformation field, Fault slip inversion

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