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Characteristics and Cause Analysis of Segmented Deformation of Coseismic Surface Rupture in Xizang Dingri MS6.8 Earthquake on January 7, 2025
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Yunxi DONG1, Wei ZHANG1, Mingjian LIANG1, *, Ling TAN1, Fupeng LI1, Shao LIU1, Jianyu LONG1, Xin TAN1, Cheng LIAO1, Hong ZUO1, Youlin DAI1, Benfu XIAO1, Yuwei WANG1, Zhiyi ZHANG2
Journal of Geodesy and Geodynamics | 2026, 46(7) : 895 - 902
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Journal of Geodesy and Geodynamics | 2026, 46(7): 895-902
Characteristics and Cause Analysis of Segmented Deformation of Coseismic Surface Rupture in Xizang Dingri MS6.8 Earthquake on January 7, 2025
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Yunxi DONG1, Wei ZHANG1, Mingjian LIANG1, *, Ling TAN1, Fupeng LI1, Shao LIU1, Jianyu LONG1, Xin TAN1, Cheng LIAO1, Hong ZUO1, Youlin DAI1, Benfu XIAO1, Yuwei WANG1, Zhiyi ZHANG2
Affiliations
  • 1 Sichuan Earthquake Agency, Chengdu 610000, China
  • 2 Sichuan Disaster Reduction Center, Chengdu 610000, China
Published: 2026-07-15 doi: 10.14075/j.jgg.2025.08.279
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On January 7, 2025, an earthquake of MS6.8 occurred in Dingri, Xizang, which produced a surface deformation zone about 35 km long. By means of high-resolution image interpretation, field geological survey and aerial photogrammetry of unmanned aerial vehicle, it is found that the northern part of the surface deformation zone of the Dingri earthquake is mainly a normal fault seismic fracture zone with vertical coseismic dislocation of 2 m to 3 m, and secondary rupture development of the nature of the strike-slip is also visible. However, the southern part of the deformation zone presents complex deformation characteristics, including both tensile deformation and extrusion deformation. Among them, the tensile deformation is mainly located on the west side of the linear fault scarp of the SN-trending Dengmocuo fault, and the deformation zone with the same strike as the fault may be a seismic surface fracture zone with structural significance. while the extrusion deformation zone is mainly distributed at the eastern boundary of lake-eroded shoal, located on the west side of the tensile deformation zone, with different directions. It is speculated that under a westward thrusting force, the surface frozen layer, as a rigid slider, slipped along the underlying saturated aquifer, cracked into multiple blocks, slipped westward and collided with each other, forming a multi-directional extrusion deformation zone.

Xizang plateau  /  Dingri MS6.8 earthquake  /  earthquake surface deformation zone  /  Dengmocuo fault
董芸希, 张威, 梁明剑, 谭凌, 李福鹏, 刘韶, 龙建宇, 谭鑫, 廖程, 左洪, 代友林, 肖本夫, 王余伟, 张智一. 2025年1月7日西藏定日MS6.8地震的同震地表破裂分段变形特征及成因分析. 大地测量与地球动力学, 2026 , 46 (7) : 895 -902 . DOI: 10.14075/j.jgg.2025.08.279
Yunxi DONG, Wei ZHANG, Mingjian LIANG, Ling TAN, Fupeng LI, Shao LIU, Jianyu LONG, Xin TAN, Cheng LIAO, Hong ZUO, Youlin DAI, Benfu XIAO, Yuwei WANG, Zhiyi ZHANG. Characteristics and Cause Analysis of Segmented Deformation of Coseismic Surface Rupture in Xizang Dingri MS6.8 Earthquake on January 7, 2025[J]. Journal of Geodesy and Geodynamics, 2026 , 46 (7) : 895 -902 . DOI: 10.14075/j.jgg.2025.08.279
Year 2026 volume 46 Issue 7
23
8
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doi: 10.14075/j.jgg.2025.08.279
  • Receive Date:2025-08-18
  • Online Date:2026-10-30
  • Published:2026-07-15
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  • Received:2025-08-18
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    1 Sichuan Earthquake Agency, Chengdu 610000, China
    2 Sichuan Disaster Reduction Center, Chengdu 610000, 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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