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Crustal Strain and Vertical Movement Characteristics of the Northeastern Margin of the Qinghai-Xizang Plateau Based on Continuous GNSS Observations
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Tao ZHANG1, Zhen TIAN1, 2, 3, *, Guofeng JI4, Jianyong LI1, Xin YU1
Journal of Geodesy and Geodynamics | 2025, 45(10) : 1006 - 1012
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Journal of Geodesy and Geodynamics | 2025, 45(10): 1006-1012
Crustal Strain and Vertical Movement Characteristics of the Northeastern Margin of the Qinghai-Xizang Plateau Based on Continuous GNSS Observations
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Tao ZHANG1, Zhen TIAN1, 2, 3, *, Guofeng JI4, Jianyong LI1, Xin YU1
Affiliations
  • 1 School of Geology and Geomatics, Chang'an University, 126 Yanta Road, Xi'an 710054, China
  • 2 State Key Laboratory of Loess Science, 126 Yanta Road, Xi'an 710054, China
  • 3 Generic Technical Development Platform of Shaanxi Province for Imaging Geodesy, 789 Third-Chanba Road, Xi'an 710016, China
  • 4 Qianxun Spatial Intelligence Inc, 38 Lane 1688 North-Guoquan Road, Shanghai 200438, China
  • HANG Tao, postgraduate, majors in GNSS crustal deformation monitoring, E-mail:

About Author:

HANG Tao, postgraduate, majors in GNSS crustal deformation monitoring, E-mail:

Published: 2025-10-15 doi: 10.14075/j.jgg.2024.09.447
Outline
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Based on continuous GNSS observation data, a relatively comprehensive three-dimensional GNSS velocity field for the northeastern margin of the Qinghai-Xizang plateau was established by fully considering random noise and regional environmental loading. This study characterizes crustal strain and vertical motion patterns in the research area. Results show that the region is dominated by compressive strain, with significant differences in principal strain rates between its southwestern and northeastern sectors. Notable distributions of maximum shear strain and principal strain are observed along the east Kunlun fault and Xianshuihe fault. Vertical uplift predominates across the northeastern Qinghai-Xizang plateau, suggesting that vertical tectonic forces may originate from intra-block compressional shortening or obstruction of deep lithospheric material flow. However, significant surface subsidence near the Lanzhou area is likely attributed to collapsible loess and soil erosion. Finally, estimates based on an incompressible Earth model indicate minimal vertical deformation caused by horizontal compression, implying that large-scale uplift in the northeastern Qinghai-Xizang plateau may primarily result from vertical tectonic factors such as lower crustal flow and lithospheric convective thinning, rather than horizontal crustal shortening.

3D velocity field  /  vertical deformation  /  GNSS imaging  /  horizontal strain  /  northeastern margin of Qinghai-Xizang plateau
张陶, 田镇, 计国锋, 黎建勇, 于鑫. 基于连续GNSS观测的青藏高原东北缘地壳应变与垂向运动特征研究. 大地测量与地球动力学, 2025 , 45 (10) : 1006 -1012 . DOI: 10.14075/j.jgg.2024.09.447
Tao ZHANG, Zhen TIAN, Guofeng JI, Jianyong LI, Xin YU. Crustal Strain and Vertical Movement Characteristics of the Northeastern Margin of the Qinghai-Xizang Plateau Based on Continuous GNSS Observations[J]. Journal of Geodesy and Geodynamics, 2025 , 45 (10) : 1006 -1012 . DOI: 10.14075/j.jgg.2024.09.447
  • Deep Earth Probe and Mineral Resources Exploration—National Science and Technology Major Project(2024ZD1000500)
  • China Postdoctoral Science Foundation(2022M710012)
  • China Postdoctoral Science Foundation(2023T160557)
  • State Key Laboratory of Earthquake Dynamics(LED2022B02)
  • Geoscience Big Data and Geohazard Prevention Innovation Team of Shaanxi Province(2022)
Year 2025 volume 45 Issue 10
35
16
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Article Info
doi: 10.14075/j.jgg.2024.09.447
  • Receive Date:2024-09-26
  • Online Date:2026-10-29
  • Published:2025-10-15
Article Data
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History
  • Received:2024-09-26
Funding
Deep Earth Probe and Mineral Resources Exploration—National Science and Technology Major Project(2024ZD1000500)
China Postdoctoral Science Foundation(2022M710012)
China Postdoctoral Science Foundation(2023T160557)
State Key Laboratory of Earthquake Dynamics(LED2022B02)
Geoscience Big Data and Geohazard Prevention Innovation Team of Shaanxi Province(2022)
Affiliations
    1 School of Geology and Geomatics, Chang'an University, 126 Yanta Road, Xi'an 710054, China
    2 State Key Laboratory of Loess Science, 126 Yanta Road, Xi'an 710054, China
    3 Generic Technical Development Platform of Shaanxi Province for Imaging Geodesy, 789 Third-Chanba Road, Xi'an 710016, China
    4 Qianxun Spatial Intelligence Inc, 38 Lane 1688 North-Guoquan Road, Shanghai 200438, 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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