杨君妍^1,,
孙文科³,
洪顺英¹,
苑争一²,
李瑜²,
陈伟¹,
孟国杰¹
1. 中国地震局地震预测研究所, 北京 100039
2. 中国地震台网中心, 北京 100045
3. 中国科学院大学地球与行星科学学院, 北京 100049

基金项目: 国家自然科学基金项目（41974093，41774088，41874024），中国地震局地震预测研究所基本科研业务费项目（2020IEF0508），大地测量与地球动力学国家重点实验室开放基金（SKLGED2021-5-3），国家重点研发计划（2019YFE0108900），中国地震科学实验场专项（2018CSES0207）联合资助


详细信息

作者简介: 杨君妍, 女, 1988年生, 副研究员, 从事GRACE和GNSS卫星在地球重力学中的应用.E-mail: yangjunyan1987@163.com

中图分类号: P315

收稿日期:2021-06-15
修回日期:2021-07-09
上线日期:2021-08-10

Coseismic deformation analysis of the 2021 Qinghai Madoi M7.4 earthquake

YANG JunYan^1,,
SUN WenKe³,
HONG ShunYing¹,
YUAN ZhengYi²,
LI Yu²,
CHEN Wei¹,
MENG GuoJie¹
1. Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100039, China
2. China Earthquake Networks Center, Beijing 100045, China
3. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China


MSC: P315

--> Received Date: 15 June 2021
Revised Date: 09 July 2021
Available Online: 10 August 2021


摘要
摘要:2021年5月22日，青海省玛多县发生了7.4级地震，该地震发生在巴颜喀拉地块北部边界东昆仑断裂带以南约70 km，属于块体内部断裂带地震.根据中国大陆构造环境监测网络提供资料，距离震源30多公里的玛多台站记录到东西向永久位移约25 cm.同时，InSAR也观测到明显的形变场，升轨和降轨的最大相对形变量分别约1.87 m和2.32 m.为了解释这些大地测量观测数据，本文利用该地震的三个断层滑动模型，基于不同地球模型的地震位错理论，计算同震变形场，并分别与GNSS观测数据和InSAR视线向形变量对比分析，结果显示基于InSAR数据反演的断层滑动模型产生的位移场与球形地球模型的理论计算结果最为吻合.进一步，利用较优断层模型计算2021年青海玛多7.4级地震的理论同震位移、大地水准面、重力和应变等变化，该结果为玛多地震的GNSS和重力观测的解释提供理论参考依据.
关键词: 玛多地震/
断层滑动模型/
同震变形/
位错理论/
地球模型

Abstract:The Madoi M7.4 earthquake occurred on May 22, 2021, in Madoi County, Qinghai Province. It is located at ~70 km south of the East Kunlun fault zone on the northern boundary of the Bayan Har block. So it belongs to the intra-block fault zone earthquake. According to the data provided by the China Continental Tectonic Environment Monitoring Network, ~25 cm permanent east-west displacement is recorded at the Madoi Station, which is more than 30 km away from the epicenter. Meanwhile, the InSAR also observes obvious deformation field, with the maximum relative LOS (Line of Sight) of ascending and descending about 1.87 m and 2.32 m, respectively. In order to interpret these geodetic observation data, we use seismic dislocation theory of different Earth models based on three fault slip models to calculate the coseismic deformation field and compare results with GNSS observation and InSAR LOS deformation. The result indicates the displacement field generated by the fault slip model which is inversed by InSAR data is good agreement with the theoretical calculation with the spherical earth model. Furthermore, we use the better fault model to calculate the theoretical coseismic displacement, geoid, gravity and strain changes of the 2021 Qinghai Madoi M7.4 earthquake. The results provide a theoretical basis for GNSS and gravity observation interpretation of Madoi earthquake.
Key words:Madoi earthquake/
Fault slip model/
Coseismic deformation/
Dislocation theory/
Earth model



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