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Anomaly Characteristics of Geoelectric Field before Jishishan MS6.2 Earthquake
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Liqiong ZHANG1, Shude GAO1, Na LI1
Journal of Geodesy and Geodynamics | 2025, 45(4) : 367 - 372
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Journal of Geodesy and Geodynamics | 2025, 45(4): 367-372
Anomaly Characteristics of Geoelectric Field before Jishishan MS6.2 Earthquake
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Liqiong ZHANG1, Shude GAO1, Na LI1
Affiliations
  • 1 Gansu Earthquake Agency, 450 West-Donggang Road, Lanzhou 730000, China
  • ZHANG Liqiong, senior engineer, majors in earthquake prediction and seismic electromagnetism, E-mail:

About Author:

ZHANG Liqiong, senior engineer, majors in earthquake prediction and seismic electromagnetism, E-mail:

Published: 2025-04-15 doi: 10.14075/j.jgg.2024.05.216
Outline
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By utilizing the method of dominant azimuth of the geoelectric field, an analysis of the dominant azimuth anomaly changes and characteristics was conducted on the geoelectric field data within a 400 km range of the epicenter of the 2023 Jishishan MS6.2 earthquake. The results show that the earliest anomaly before the earthquake occurred at the Guyuan station, which is located at the intersection of the Haiyuan fault and the Liupanshan fault. During the period of the anomaly, the Jingtai station, located in the middle section of the Haiyuan fault, also showed a rapid and significant deflection of the azimuth. The max azimuth α changes at both stations deviated from the normal background value by about 45°, which is considered a medium to short-term anomaly. The last anomaly to appear was at the Dawu station, located in the Bayan Har block, where the azimuth angle α showed a rapid deflection and jump, deviating from the normal background value by about 90°, which is considered a short-term anomaly. The number of three abnormal stations meets the prediction index system of the geoelectric field dominant azimuth. The evolution of the anomaly shows that the anomalies have quasi-synchronous characteristics in terms of appearance, duration, and end time. In terms of the distance from the epicenter, Guyuan station is the farthest, while Jingtai and Dawu stations are closer to the earthquake epicenter. Before the earthquake, due to the internal compression of the plate, the areas where the three geoelectric field stations are located and the surrounding stress compression changes were intense. When rocks were subjected to pressure and fracture, the fracture structure of the rock mass led to significant changes in the dominant azimuth of the geoelectric field in succession. The subsequent end of the three geoelectric fields anomaly after the earthquake also indirectly reflected the process of the gradual recovery of the rock mass fracture structure after stress release, indicating that the data changes of the three stations can truly reflect the changes in the underground medium.

geoelectric field  /  Jishishan MS6.2 earthquake  /  dominant azimuth  /  anomaly characteristics
张丽琼, 高曙德, 李娜. 积石山MS6.2地震前地电场异常特征. 大地测量与地球动力学, 2025 , 45 (4) : 367 -372 . DOI: 10.14075/j.jgg.2024.05.216
Liqiong ZHANG, Shude GAO, Na LI. Anomaly Characteristics of Geoelectric Field before Jishishan MS6.2 Earthquake[J]. Journal of Geodesy and Geodynamics, 2025 , 45 (4) : 367 -372 . DOI: 10.14075/j.jgg.2024.05.216
  • The Spark Program of Earthquake Technology of CEA(XH24047YA)
  • Joint Fund for Earthquake Science(U2039206)
  • Seismic Regime Tracking Project of CEA(CEA-ZQGZ-202501049)
  • The Key Project of Seismological Research Fund of Gansu Earthquake Agency(KY2203002)
Year 2025 volume 45 Issue 4
25
10
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Article Info
doi: 10.14075/j.jgg.2024.05.216
  • Receive Date:2024-05-09
  • Online Date:2026-10-30
  • Published:2025-04-15
Article Data
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History
  • Received:2024-05-09
Funding
The Spark Program of Earthquake Technology of CEA(XH24047YA)
Joint Fund for Earthquake Science(U2039206)
Seismic Regime Tracking Project of CEA(CEA-ZQGZ-202501049)
The Key Project of Seismological Research Fund of Gansu Earthquake Agency(KY2203002)
Affiliations
    1 Gansu Earthquake Agency, 450 West-Donggang Road, Lanzhou 730000, 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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