journal article·2024-11-28Open access

Deformation Distribution Characteristics and Seismic Hazard of the Xianshuihe Fault Zone Based on GNSS and InSAR Data

Junkai Yao, Changyun Chen, Jingwei Liang, Bingfeng Tao, Qingmeng Wei, Yongyan Du

Applied Sciences· Volume 14· Issue 23

Abstract

The spatial distribution characteristics and slip rate in the Xianshuihe Fault Zone (XSHFZ) are still subject to controversy, and the segments where creeping movement occurs within the fault remain unclear. In this paper, the three-dimensional deformation field of the XSHFZ and its neighboring areas is obtained by integrating InSAR and GNSS data. Subsequently, based on the three-dimensional deformation field, an elastic dislocation model is employed to analyze the slip rate, locking state, and creeping movement within the XSHFZ. The results show that the XSHFZ is a typical sinistral strike–slip fault with compressional characteristics. The slip rate of the XSHFZ ranges from 9.3 to 14.3 mm/yr. The average strike–slip rate of the Qianning and Kangding segments surpasses that of the eastern and western segments, while the Moxi segment exhibits the lowest slip rate. The locking depth of the XSHFZ is estimated to be between 13 and 26 km, with shallow creep movement predominantly concentrated in three segments: Daofu, Qianning, and Kangding, where the shallow creep rate ranges from 1.5 to 4.9 mm/yr. The XSHFZ is known for its short recurrence period of strong earthquakes and frequent seismic activities. A quantitative study of fault slip rates, locking depth, and creeping movement provides essential support for analyzing its seismic hazards. The seismic hazard of each segment of the Xianshuihe Fault Zone (XSHFZ) was analyzed based on the principle of seismic moment balance. The areas with high seismic hazards in the Xianshuihe Fault Zone correspond to the locations of seismic gaps along the fault. Specifically, the Qianning segment and the Yalahe and Selaha faults within the Kangding segment are associated with seismic gaps and are at risk of experiencing earthquakes with magnitudes of 6.9, 6.9, and 6.6, respectively. The results highlight the importance of continuous monitoring and preparedness measures to mitigate the seismic risks present in the XSHFZ.
Source: crossref · Quality: baseline

Research context

OpenAlex topics: earthquake and tectonic studies · Earthquake Detection and Analysis · Rock Mechanics and Modeling

SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.

Affiliations

State Key Laboratory of High-Speed Railway Track System, Beijing 100081, China

Railway Engineering Research Institute, China Academy of Railway Sciences Corporation Limited, Beijing 100081, China

China Academy of Railway Sciences Corporation Limited, Beijing 100081, China

The First Monitoring and Application Center, China Earthquake Administration, Tianjin 300180, China

School of Geology and Geomatics, Tianjin Chengjian University, Tianjin 300384, China

Funding

The Open Fund for National Innovation Platform of State Key laboratory of High-speed Railway Track System

References (81)

Show source-provided references
1. Field Study of a Highly Active Fault Zone: The Xianshuihe Fault of Southwestern China10.1130/0016-7606(1991)103<1178:FSOAHA>2.3.CO;2 ↗
2. Pattern of Latest Tectonic Motion and Its Dynamics for Active Blocks in Sichuan-Yunnan Region, China10.1360/03dz0017 ↗
3. A Review on Active Tectonics and Deep Crustal Processes of the Western Sichuan Region, Eastern Margin of the Tibetan Plateau10.1016/j.tecto.2012.02.021 ↗
4. Late Quaternary Slip-Rates and Slip Partitioning on the Southeastern Xianshuihe Fault System, Eastern Tibetan Plateau10.1111/1755-6724.12689 ↗
5. Holocene Activity and Paleoseismicity of the Selaha Fault, Southeastern Segment of the Strike-Slip Xianshuihe Fault Zone, Tibetan Plateau10.1016/j.tecto.2016.11.014 ↗
6. Cooling History of the Gongga Batholith: Implications for the Xianshuihe Fault and Miocene Kinematics of SE Tibet10.1016/j.epsl.2017.02.025 ↗
7. Southeastward Increase of the Late Quaternary Slip-Rate of the Xianshuihe Fault, Eastern Tibet. Geodynamic and Seismic Hazard Implications10.1016/j.epsl.2017.12.045 ↗
8. The Slip Rate and Strong Earthquake Recurrence Interval on the Qianning-Kangding Segment of the Xianshuihe Fault Zone10.1007/s11589-001-0004-8 ↗
9. Liang, M. (2019). Characteristics of the Late Quaternary Fault Activity of the Xianshuihe Fault. [Ph.D. Thesis, Institute of Geology, China Earthquake Administration].
10. Conditional Probabilities for the Recurrence of Earthquakes on the Xianshuihe Fault Zone within the Coming Three Decades
11. Wang, E. (1998). Late Cenozoic Xianshuihe-Xiaojiang, Red River, and Dali Fault Systems of Southwestern Sichuan and Central Yunnan, China, Geological Society of America.10.1130/0-8137-2327-2.1 ↗
12. Segmentation, geometric features, and their seismotectonic implications for the Holocene xianshuihe fault zone
13. Interseismic Slip Rate of the Northwestern Xianshuihe Fault from InSAR Data
14. Contemporary Crustal Deformation around the Southeast Borderland of the Tibetan Plateau10.1029/2004JB003421 ↗
15. Present-Day Crustal Motion within the Tibetan Plateau Inferred from GPS Measurements10.1029/2005JB004120 ↗
16. Geodetic Imaging of Potential Seismogenic Asperities on the Xianshuihe-Anninghe-Zemuhe Fault System, Southwest China, with a New 3-D Viscoelastic Interseismic Coupling Model10.1002/2014JB011492 ↗
17. Locking Depth, Slip Rate, and Seismicity Distribution along the Daofu–Kangding Segment of the Xianshuihe Fault System, Eastern Tibetan Plateau10.1016/j.jseaes.2020.104328 ↗
18. Block-like versus Distributed Crustal Deformation around the Northeastern Tibetan Plateau10.1016/j.jseaes.2017.02.040 ↗
19. Crustal Deformation in the India-Eurasia Collision Zone From 25 Years of GPS Measurements10.1002/2017JB014465 ↗
20. Present-Day Kinematics at the India-Asia Collision Zone10.1130/G22924A.1 ↗
21. Present-Day Crustal Deformation of Continental China Derived from GPS and Its Tectonic Implications10.1029/2019JB018774 ↗
22. Along-Strike Variation in Fault Structural Maturity and Seismic Moment Deficits on the Yushu-Ganzi-Xianshuihe Fault System Revealed by Strain Accumulation and Regional Seismicity10.1016/j.epsl.2022.117799 ↗
23. Present-Day Kinematics in Southeastern Tibet Inferred From GPS Measurements10.1029/2020JB021305 ↗
24. Block Motion, Slip Rates, and Earthquake Hazard Assessment of Boundary Faults in the Sichuan–Yunnan Region, China10.1007/s11600-024-01319-1 ↗
25. Interseismic Deformation in the Northwestern Sichuan-Yunnan Block Constrained by Sentinel-1 InSAR and GNSS10.1016/j.tecto.2024.230440 ↗
26. GPS Monitoring of Temporal Deformation of the Xianshuihe Fault10.1007/s11430-008-0095-3 ↗
27. Post-seismic slip deformation on the Luhuo segment of the Xianhuihe fault zone
28. Surface Creep and Slip-Behavior Segmentation along the Northwestern Xianshuihe Fault Zone of Southwestern China Determined from Decades of Fault-Crossing Short-Baseline and Short-Level Surveys10.1016/j.tecto.2017.11.002 ↗
29. Interseismic movement along the Luhuo-Daofu section of the Xianshuihe fault from InSAR and GPS observations
30. Geodetic Imaging of Shallow Creep along the Xianshuihe Fault and Its Frictional Properties10.1016/j.epsl.2021.117001 ↗
31. Interseismic slip rates and shallow creep along the northwestern segment of the Xianshuihe fault from InSAr data
32. Active Tectonic Blocks and Strong Earthquakes in the Continent of China10.1360/03dz0002 ↗
33. Xu, X., Han, Z., Yang, X., Zhang, S., Yu, G., Zhou, B., Li, F., Ma, B., Chen, G., and Ran, Y. (2016). Seismotectonic Map in China and Its Adjacent Regions, Seismological Press.
34. Department of Earthquake Disaster Prevention, State Seismological Bureau (1995). The Catalogue of Chinese Historical Strong Earthquakes, Seismological Press.
35. Spatial Distribution of Time-Independent Seismicity in China10.1007/s000240050223 ↗
36. Department of Earthquake Disaster Prevention, China Earthquake Administration (1999). The Catalogue of Chinese Modern Earthquakes, China Science and Technology Press.
37. Research on the completeness of earthquake data in the Chinese mainland (II)
38. The Working Group of M7 (2012). Study on the Mid- to Long-Term Potential of Large Earthquakes on the Chinese Continent, Seismological Press. [1st ed.].
39. Estimating recent activities of the Xianshuihe fault zone by earthquake activity parameters
40. Quasi-Time-Predictable Recurrence Behavior and Assessments of Earthquake Occurrence Probabilities on Segments of Fault Zone
41. Historical Pattern and Behavior of Earthquake Ruptures along the Eastern Boundary of the Sichuan-Yunnan Faulted-Block, Southwestern China10.1016/j.pepi.2008.04.013 ↗
42. Research on the Magnitude and Recurrence Interval of Characterized Earthquakes with Magnitude ≥ 6.7 along the Northwestern Portion of the Xianshuihe Fault Zone in Western Sichuan, China
43. Study on the potential strong-earthquake risk for the eastern boundary of the sichuan-yunnan active faulted-block, China
44. Earthquake Triggering along the Xianshuihe Fault Zone of Western Sichuan, China10.1007/s00024-003-2471-4 ↗
45. Evolution of Coulomb stress and stress interaction among strong earthquakes along the Xianshuihe fault zone
46. Coulomb Stress Evolution over the Past 200years and Seismic Hazard along the Xianshuihe Fault Zone of Sichuan, China10.1016/j.tecto.2015.12.018 ↗
47. Cenozoic Tectonics of Asia: Effects of a Continental Collision: Features of Recent Continental Tectonics in Asia Can Be Interpreted as Results of the India-Eurasia Collision10.1126/science.189.4201.419 ↗
48. Slip-Line Field Theory and Large-Scale Continental Tectonics10.1038/264319a0 ↗
49. Oblique Stepwise Rise and Growth of the Tibet Plateau10.1126/science.105978 ↗
50. Basic Characteristics of Active Tectonics of China10.1360/03yd9032 ↗
51. On the Mechanics of the Collision between India and Asia10.1144/GSL.SP.1986.019.01.07 ↗
52. Late Cenozoic Right-Lateral Strike-Slip Faulting in Southern Tibet10.1029/JB094iB03p02787 ↗
53. Tibet Uplift and Erosion10.1016/0040-1951(96)00076-5 ↗
54. An, Y. (2010). Boundary Features of the Seismic Rupture Segments Along the Xianshuihe Fault Zone. [Ph.D. Thesis, Institute of Geology, China Earthquake Administration].
55. Dynamic Deformation and Fault Locking of the Xianshuihe Fault Zone, Southeastern Tibetan Plateau: Implications for Seismic Hazards10.1186/s40623-022-01591-9 ↗
56. Aftershock Zones of Great Earthquakes, Seismicity Gaps, and Earthquake Prediction for Alaska and the Aleutians
57. High-Precision Vertical Movement and Three-Dimensional Deformation Pattern of the Tibetan Plateau10.1029/2021JB023202 ↗
58. Three-Dimensional Surface Displacements from InSAR and GPS Measurements with Variance Component Estimation10.1109/LGRS.2011.2181154 ↗
59. Influence of Different Data Fusion Methods on the Accuracy of Three-Dimensional Displacements Field10.1016/j.asr.2019.12.017 ↗
60. Analysis of the Fault Slip, Creep, and Coupling Characteristics of the Maomaoshan-Laohushan-Haiyuan Fault Using InSAR and GNSS Measurements10.1016/j.tecto.2023.229988 ↗
61. Geodetic Determination of Relative Plate Motion in Central California
62. Slip Rate and Locking Depth from GPS Profiles across the Southern Dead Sea Transform
63. Segall, P. (2010). Earthquake and Volcano Deformation. Earthquake and Volcano Deformation, Princeton University Press.10.1515/9781400833856 ↗
64. Along-Strike Variations of the Partitioning of Convergence across the Haiyuan Fault System Detected by InSAR10.1093/gji/ggw028 ↗
65. Geodetic Observations of Shallow Creep on the Laohushan-Haiyuan Fault, Northeastern Tibet10.1029/2020JB021576 ↗
66. He, L., Lv, H., Feng, G., Xiong, Z., Wang, Y., Gao, H., Wang, W., Yang, X., and Lv, L. (2024). Interseismic Kinematic Parameter Inversion and Seismic Hazard Assessment of the Xianshuihe Fault Zone Based on InSAR. J. Geod. Geodyn., 1–10.
67. Spatial Slip Rate Distribution Along the SE Xianshuihe Fault, Eastern Tibet, and Earthquake Hazard Assessment10.1029/2021TC006985 ↗
68. Aseismic Sliding of Active Faults by Pressure Solution Creep: Evidence from the San Andreas Fault Observatory at Depth10.1130/G32073.1 ↗
69. Large Earthquakes and Creeping Faults10.1002/2016RG000539 ↗
70. Creeping Faults: Good News, Bad News?10.1002/2017RG000565 ↗
71. Partial Coupling and Earthquake Potential Along the Xianshuihe Fault, China10.1029/2020JB021406 ↗
72. The California Earthquake of April 18, 1906
73. M ≧ 6 Earthquakes in Southern California during the Twentieth Century: No Evidence for a Seismicity or Moment Deficit10.1785/BSSA0880030635 ↗
74. The Relationship between Seismic and Aseismic Slip on the Philippine Fault on Leyte Island: Bayesian Modeling of Fault Slip and Geothermal Subsidence10.1029/2020JB020052 ↗
75. A Moment Magnitude Scale10.1029/JB084iB05p02348 ↗
76. Balance of Seismic Moment in the Songpan-Ganze Region, Eastern Tibet: Implications for the 2008 Great Wenchuan Earthquake10.1016/j.tecto.2009.09.022 ↗
77. Slip Rates and Seismic Moment Deficits on Major Active Faults in Mainland China
78. Comparison between Earthquake Magnitudes Determined by China Seismograph Network and US Seismograph Network (II): Surface Wave Magnitude
79. Research on the Completeness of Earthquake Data in the Chinese Mainland (I)—North China10.1007/BF02650672 ↗
80. Moment Budget and Seismic Potential of the Xianshuihe-Xiaojiang Fault System, Southeastern Tibetan Plateau10.1016/j.tecto.2023.229935 ↗
81. The Generic Mapping Tools Version 610.1029/2019GC008515 ↗