ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
玉树地震震前甘孜—玉树断裂局部应力场时空偏转特征的离散元模拟研究
  
关键词:Yushu earthquake  Ganzi–Yushu fault  discrete element  local stress field  deflection angle
基金项目:中央高校基本科研业务费研究生科技创新项目(编号: ZY20220319);国家自然科学基金项目(编号: 41807270);中央高校基本科研业务费专题研究重点项目(编号: ZY20215113)
作者单位E-mail
张涛 防灾科技学院地质工程学院 863841827@qq.com 
苏占东 防灾科技学院地质工程学院
河北省地震灾害防御与风险评价重点实验室 
szdchris@163.com 
孙进忠 中国地质大学(北京)工程技术学院  
张建勇 防灾科技学院地质工程学院  
唐磊 中国地震台网中心  
周剑 北京工业大学城市与工程安全减灾教育部重点实验室  
王磊 防灾科技学院地质工程学院
河北省地震灾害防御与风险评价重点实验室 
 
张明磊 防灾科技学院地质工程学院
河北省地震灾害防御与风险评价重点实验室 
 
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摘要:
Discrete Element Modeling of the Spatiotemporal Deflection Characteristics of the Local Stress Field of the Ganzi–Yushu Fault before the Yushu Earthquake
      Regional tectonic activities alter the stress state of the crust, and tectonic earthquakes are extreme regional tectonic activities. Therefore, understanding the change in the local stress field of seismogenic faults before earthquakes occur has great significance in the characterization of fault activities. This study used the particle discrete element package PFC2D and monitoring data of the YRY-4 borehole strain gauge at the Yushu Seismic Station to simulate the spatiotemporal deflection characteristics of the maximum principal stress direction in the local stress field before the Yushu MS7.1 earthquake on April 14, 2010, and the Ganzi–Yushu strike-slip fault. The results showed that the SH direction of the maximum horizontal principal stress at the Yushu station before the earthquake displayed counterclockwise deflection. The deflection gradually recovered after a certain amount of strain energy had accumulated. The change pattern of the simulated local stress direction was generally consistent with the field observation results. The variation pattern of SH differed at different positions of the fault, and the disturbance of local stress was more obvious with nearer proximity to the fault structure. The SHT located in the tensile stress concentration area and the SHP located in the compressive stress concentration area rotated simultaneously toward the boundary direction of the two areas. The deflection angle increased gradually with increasing time step. The degree of stress accumulation varied among different regions and increased with loading time. Fractures occurred at different times, with obvious spatiotemporal asynchronous effects.
ZHANG Tao,SU Zhandong,SUN Jinzhong,ZHANG Jianyong,TANG Lei,ZHOU Jian,WANG Lei,ZHANG Minglei.2024.Discrete Element Modeling of the Spatiotemporal Deflection Characteristics of the Local Stress Field of the Ganzi–Yushu Fault before the Yushu Earthquake[J].Acta Geoscientica Sinica,45(2):203-216.
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