HIGHLIGHTS
- who: Yefei Bai from the sampled with a time interval of , s. We hand-picked the P wave first arrivals, and a time window of , s was used for the joint inversion. Eight coseismic static displacements from GNSS sites processed by the Geodesy Laboratory at Central Washington University were used (Fig., ). Eight hr-GNSS time series which include both seismic arrivals and static offsets were also used, with data provided by the UNAVCO website (Supplementary Fig., ). have published the research work: Fast and slow intraplate ruptures during the 19 October 2020 magnitude 7.6 Shumagin earthquake, in . . .
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