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Current Crustal Horizontal Deformation Characteristics and Stress-Strain Coupling Relationship of Ordos Block and Its Periphery
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Hui YANG1, Kang JI1, Yangyang GUO1
Journal of Geodesy and Geodynamics | 2025, 45(2) : 157 - 162, 176
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Journal of Geodesy and Geodynamics | 2025, 45(2): 157-162, 176
Current Crustal Horizontal Deformation Characteristics and Stress-Strain Coupling Relationship of Ordos Block and Its Periphery
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Hui YANG1, Kang JI1, Yangyang GUO1
Affiliations
  • 1 Xi'an Coal Transparent Geology Technology Co Ltd, Second-Nengyuan Road, Xianyan 712028, China
  • YANG Hui, associate researcher, majors in precision geodesy and dynamic deformation monitoring and analysis, E-mail:

About Author:

YANG Hui, associate researcher, majors in precision geodesy and dynamic deformation monitoring and analysis, E-mail:

Published: 2025-02-15 doi: 10.14075/j.jgg.2024.04.154
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Addressing the under-quantified crustal deformation characteristics and the unclear stress-strain coupling relationship of the Ordos block, this study employs a spherical least squares collocation model to calculate the characteristic strain field of the study area's crust and inverts the principal stress distribution using seismic source mechanism data. The results indicate that crustal deformation is primarily concentrated along plate boundaries and within fault basins, with less deformation within the Ordos block itself. Notably, at the junction of the northeastern Tibetan plateau and the Alxa block, the crustal deformation is particularly intense, characterized by strong compression along the plate boundary, with the main deformation mechanism being a coexistence of NW-SE compression and NE-SW extension, with a maximum principal compressive strain rate exceeding 0.05 μstrain. The crust in the study area is under a relatively uniform tensile stress environment, with the direction of the maximum principal stress being nearly horizontal and pointing towards SEE, aligning with the direction of the principal strain in the corresponding area. The minimum principal stress direction is closer to the direction of the principal compressive strain.

Ordos block  /  crustal deformation  /  spherical least squares collocation  /  focal mechanism solution  /  strain field  /  principal stress direction
杨辉, 冀康, 郭泱泱. 鄂尔多斯块体及其周缘现今地壳水平形变特征及应力应变耦合关系. 大地测量与地球动力学, 2025 , 45 (2) : 157 -162, 176 . DOI: 10.14075/j.jgg.2024.04.154
Hui YANG, Kang JI, Yangyang GUO. Current Crustal Horizontal Deformation Characteristics and Stress-Strain Coupling Relationship of Ordos Block and Its Periphery[J]. Journal of Geodesy and Geodynamics, 2025 , 45 (2) : 157 -162, 176 . DOI: 10.14075/j.jgg.2024.04.154
Year 2025 volume 45 Issue 2
22
8
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doi: 10.14075/j.jgg.2024.04.154
  • Receive Date:2024-04-07
  • Online Date:2026-10-30
  • Published:2025-02-15
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  • Received:2024-04-07
Affiliations
    1 Xi'an Coal Transparent Geology Technology Co Ltd, Second-Nengyuan Road, Xianyan 712028, 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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