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Surface Deformation and Seismogenic Fault Model of Zaduo MW5.7 Earthquake Revealed by InSAR Observations
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Jiayu HAO1, 2, 3, Chuang SONG1, 2, 4, *, Yihan NAI1, 2, 3, Zhenjiang LIU1, 2, 3, Chen YU1, 2, 4, Zhenhong LI1, 2, 4
Journal of Geodesy and Geodynamics | 2026, 46(4) : 435 - 442
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Journal of Geodesy and Geodynamics | 2026, 46(4): 435-442
Surface Deformation and Seismogenic Fault Model of Zaduo MW5.7 Earthquake Revealed by InSAR Observations
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Jiayu HAO1, 2, 3, Chuang SONG1, 2, 4, *, Yihan NAI1, 2, 3, Zhenjiang LIU1, 2, 3, Chen YU1, 2, 4, Zhenhong LI1, 2, 4
Affiliations
  • 1 School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, China
  • 2 State Key Laboratory of Loess Science, Xi'an 710054, China
  • 3 Big Data Center for Geosciences and Satellites, Chang'an University, Xi'an 710054, China
  • 4 Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Xi'an 710054, China
Published: 2026-04-15 doi: 10.14075/j.jgg.2025.03.108
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Abstract: Using ascending and descending SAR images from Sentinel-1A satellite, the co-seismic deformation of the MW5.7 earthquake in Zaduo county, Yushu city on March 7, 2024, was obtained. The geometry parameters and slip distribution of the seismogenic fault were inverted. Finally, based on the Coulomb stress changes induced by the earthquake, the impact on surrounding faults was analyzed and the regional seismic hazard was assessed. The results show that the main deformation areas of the co-seismic deformation fields from both ascending and descending orbits exhibit a four-quadrant distribution, with maximum LOS displacements of approximately 3.1 cm and 3.6 cm for ascending and descending orbits, respectively. Fault inversion experiments indicate that both the northeast-dipping fault model and the northwest-dipping fault model can reasonably explain the surface deformation caused by this earthquake. However, after a comprehensive analysis of co-seismic fitting residuals, regional active fault distribution, and geomorphic features, this study leans towards the conclusion that the seismogenic fault of this earthquake is a northeast-dipping strike-slip fault with a northwest-southeast trend. Co-seismic slip is concentrated at depths of 1.5 to 6.0 km, reaching a peak slip of 1.0 m at a depth of 3.7 km. Additionally, the static Coulomb stress changes reveal that the 2024 Zaduo earthquake has increased the risk of future earthquakes in the Yanshiping fault zone.

2024 Zaduo MW5.7 earthquake  /  InSAR  /  co-seismic deformation  /  fault slip distribution  /  Coulomb stress change
郝嘉宇, 宋闯, 能懿菡, 刘振江, 余琛, 李振洪. InSAR观测揭示的杂多MW5.7地震地表形变及发震断层模型. 大地测量与地球动力学, 2026 , 46 (4) : 435 -442 . DOI: 10.14075/j.jgg.2025.03.108
Jiayu HAO, Chuang SONG, Yihan NAI, Zhenjiang LIU, Chen YU, Zhenhong LI. Surface Deformation and Seismogenic Fault Model of Zaduo MW5.7 Earthquake Revealed by InSAR Observations[J]. Journal of Geodesy and Geodynamics, 2026 , 46 (4) : 435 -442 . DOI: 10.14075/j.jgg.2025.03.108
Year 2026 volume 46 Issue 4
41
17
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doi: 10.14075/j.jgg.2025.03.108
  • Receive Date:2025-03-31
  • Online Date:2026-10-29
  • Published:2026-04-15
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  • Received:2025-03-31
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Affiliations
    1 School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, China
    2 State Key Laboratory of Loess Science, Xi'an 710054, China
    3 Big Data Center for Geosciences and Satellites, Chang'an University, Xi'an 710054, China
    4 Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Xi'an 710054, China
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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