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Source Model of the 2025 Dingri MW7.1 Earthquake Based on InSAR and Pixel Offset Tracking Observations
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Jin XU1, 2, Shijie GE2, Xinyi PAN2, Xixuan BAI3, *, Jianfeng GU3, Bingqiang ZHANG3
Journal of Geodesy and Geodynamics | 2026, 46(9) : 1147 - 1155
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Journal of Geodesy and Geodynamics | 2026, 46(9): 1147-1155
Source Model of the 2025 Dingri MW7.1 Earthquake Based on InSAR and Pixel Offset Tracking Observations
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Jin XU1, 2, Shijie GE2, Xinyi PAN2, Xixuan BAI3, *, Jianfeng GU3, Bingqiang ZHANG3
Affiliations
  • 1 School of Humanities and International Communication, Ningbo University of Technology, Ningbo 315600, China
  • 2 Emergency Management Research Center of Ninghai County, Ningbo 315600, China
  • 3 School of Civil Engineering and Architecture, Wuhan Institute of Technology, Wuhan 430074, China
Published: 2026-09-15 doi: 10.14075/j.jgg.2025.11.403
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Based on Sentinel-1A ascending and descending SAR data, the co-seismic InSAR deformation field and range-direction pixel offset of the January 7, 2025, MW7.1 Dingri earthquake were obtained. Combined with elastic half-space dislocation theory, the particle swarm optimization (PSO) algorithm and the Akaike-Bayesian information criterion (ABIC) were used to invert single- and double-fault slip distribution models. Static Coulomb stress changes at depths of 5 km, 10 km, and 15 km were also calculated. The results show that although the double-fault model, constrained by surface rupture traces identified via the pixel offset tracking (POT) method, exhibits higher roughness, it more accurately reproduces the surface rupture trajectory at fault strike variations. The double-fault model achieved fitting accuracies of 97.2% and 96.5% for ascending and descending InSAR data, respectively, outperforming the single-fault model (96.8%/95.9%). The inverted seismogenic fault has a strike of 186° and a dip angle of 55°, with co-seismic slip mainly concentrated in the northern section and a secondary slip core between the two fault strands. The total seismic moment released was 6.12×1019 Nm (MW7.1). Coulomb stress perturbations generally decreased on both sides of the fault, while stress increased at a depth of 15 km in the southern segment, showing strong spatial correlation with aftershock distribution, indicating that stress in this region is prone to release through aftershocks. Local stress increases were also observed at different depths near the northern and southern ends of the fault, which should be key areas for future research.

Dingri earthquake  /  InSAR  /  POT  /  source model inversion  /  Coulomb stress change
徐瑾, 葛诗杰, 潘欣怡, 白希选, 顾箭峰, 张兵强. 融合InSAR与POT观测的定日MW7.1地震震源模型研究. 大地测量与地球动力学, 2026 , 46 (9) : 1147 -1155 . DOI: 10.14075/j.jgg.2025.11.403
Jin XU, Shijie GE, Xinyi PAN, Xixuan BAI, Jianfeng GU, Bingqiang ZHANG. Source Model of the 2025 Dingri MW7.1 Earthquake Based on InSAR and Pixel Offset Tracking Observations[J]. Journal of Geodesy and Geodynamics, 2026 , 46 (9) : 1147 -1155 . DOI: 10.14075/j.jgg.2025.11.403
Year 2026 volume 46 Issue 9
32
12
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doi: 10.14075/j.jgg.2025.11.403
  • Receive Date:2025-11-20
  • Online Date:2026-10-30
  • Published:2026-09-15
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  • Received:2025-11-20
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    1 School of Humanities and International Communication, Ningbo University of Technology, Ningbo 315600, China
    2 Emergency Management Research Center of Ninghai County, Ningbo 315600, China
    3 School of Civil Engineering and Architecture, Wuhan Institute of Technology, Wuhan 430074, 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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