This research was funded by the Science for earthquake Resilience(No.XH24014YC),the Sixth Phase"169 Project"Scientific Research Project of Zhenjiang City(No.25),the Scientific Research Fund from Institute of Seismology,CEA and National Institute of Natural Hazards,Ministry of Emergency Management of China(No.IS202216316),and the Open Research Fund of the National Field Observation and Research Station for Gravity and Solid Tides,Wuhan(Nos.WHYMZ202113 and WHYWZ202301).The authors give special thanks to the Qinghai Basic Surveying and Mapping Institute and the Gansu Surveying and Mapping Engineering Institute for their provision of high-rate GNSS data.The authors gratefully appreciate the Incorporated Research Institutions for Seismology Data Management Center(IRIS-DMC,http://ds.iris.edu)for the far-field seismic wave data.In this study,high-rate GNSS data were resolved using GAMIT/TRACK jointly developed by MIT and SIO,PPP-AR developed by research team PRIDE at Wuhan University,and the velocity determination software created by the research team led by Rongxin Fang at Wuhan University.Several figures in this paper were drawn using GMT.We would like to thank Editage(www.editage.cn)for English language editing. （No.XH24014YC）