石富强^1,,
张辉²,
邵志刚^3,,,
徐晶⁴,
邵辉成¹,
李玉江⁵
1. 陕西省地震局, 西安 710068
2. 甘肃省地震局, 兰州 730000
3. 中国地震局地震预测研究所, 北京 100036
4. 中国地震局第二监测中心, 西安 710054
5. 应急管理部国家自然灾害防治研究院, 北京 100085

基金项目: 国家重点研发计划（2017YFC1500501），中国地震局地震科技星火计划（XH21032）和震情跟踪合同制任务（2019020501）以及中国大陆地震重点监视防御区任务共同资助


详细信息

作者简介: 石富强, 男, 1984年生, 高级工程师, 2011年硕士毕业于兰州大学, 主要从事地壳运动学及动力学方面的数值模拟工作.E-mail:shifuqiang121@163.com

通讯作者: 邵志刚, 男, 1977年生, 研究员, 2007年博士毕业于中国科学技术大学, 主要从事地球动力学与地震活动性方面的研究.E-mail:shaozg0911@126.com

中图分类号: P541;P315

收稿日期:2020-03-09
修回日期:2020-07-27
上线日期:2020-09-05

Coulomb stress evolution and stress interaction among strong earthquakes in North China

SHI FuQiang^1,,
ZHANG Hui²,
SHAO ZhiGang^3,,,
XU Jing⁴,
SHAO HuiCheng¹,
LI YuJiang⁵
1. Shaanxi Earthquake Agency, Xi'an 710068, China
2. Gansu Earthquake Agency, Lanzhou 730000, China
3. Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, China
4. The Second Crust Monitoring and Application Center, China Earthquake Administration, Xi'an 710054, China
5. National Institute of Natural Hazards, Ministry of Emergency Management, Beijing 100085, China


More Information

Corresponding author: SHAO ZhiGang,E-mail:shaozg0911@126.com

MSC: P541;P315

--> Received Date: 09 March 2020
Revised Date: 27 July 2020
Available Online: 05 September 2020


摘要
摘要:采用更加符合长期变形和震后短期变形的Burgers流变模型，模拟了华北地区1303年以来6.5级以上地震引起的同震和震后库仑应力演化.结合华北地区历史地震期幕活动特征，分析了不同活跃期之间、同一活跃期内不同地震之间的库仑应力加卸载效应.结果表明：华北地区不同活跃期的强震主体活动区受控于历史强震的库仑应力加载作用；每个活跃期内强震活动主体区在空间上的迁移与该活跃期内首个7.5级以上地震的触发作用有关；华北地区每个活跃期内强震活动在时间上表现出的"平静期—活跃警告期—高潮期—剩余释放期"应该是区域动力加载过程的一种表现.岩石圈流变松弛效应引起的库仑应力变化对华北地区强震活动时空演化有显著的促进作用.本研究讨论了库仑应力变化在华北地区历史地震活动时空演化过程中可能扮演的角色，为探索华北地区强震活动空间迁移和韵律特征蕴含的构造动力学过程，以及与之相关的地震危险性判定提供参考依据.
关键词: 地震活动/
时空演化/
库仑应力/
Burgers流变模型/
华北

Abstract:Using the Burgers rheological model which is more suitable for both long-term tectonic deformation and short-term postseismic deformation simulation, we simulated the coseismic and postseismic Coulomb stress evolution that caused by all M_S≥6.5 earthquakes since 1303 in North China. Then, the Coulomb stress change among earthquakes in the same seismic activity period and across different seismic activity periods, are discussed based on the historical strong earthquake activity in North China and its temporal rhythmic character. The results indicated that the major seismic active area in North China is controlled by the Coulomb stress loading of historical strong earthquakes, and its spatial migration in one seismic activity period should be driven by the Coulomb stress loading of the first M_S≥7.5 earthquake. The phenomenon of "Quiescence-Active warning-High activity-Surplus release" in the temporal seismic activity in North China could be interpreted as the dynamic response of the tectonic stress loading. Coulomb stress that associated with the rheological relaxation of the lithosphere contributes to the seismic activity in North China. The main purpose of this paper is to discuss the Coulomb stress changes and their effects on the strong earthquakes activity in North China, and then furnish some references on the mechanism exploring of the spatial migration and temporal rhythmic character of the seismic activity in North China, as well as the related seismic risk analysis.
Key words:Earthquake activity/
Spatio-temporal evolution/
Coulomb stress/
Burgers rheology/
North China



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