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Dai ZH, Zhou LQ, Hu XH, Qu JH and Li X (2023). Generalization of PhaseNet in Shandong and its application to the Changqing M4.1 earthquake sequence. Earthq Sci 36(3): 212–227,. DOI: 10.1016/j.eqs.2023.04.003
Citation: Dai ZH, Zhou LQ, Hu XH, Qu JH and Li X (2023). Generalization of PhaseNet in Shandong and its application to the Changqing M4.1 earthquake sequence. Earthq Sci 36(3): 212–227,. DOI: 10.1016/j.eqs.2023.04.003

Generalization of PhaseNet in Shandong and its application to the Changqing M4.1 earthquake sequence

  • Waveforms of seismic events, extracted from January 2019 to December 2021 were used to construct a test dataset to investigate the generalizability of PhaseNet in the Shandong region. The results show that errors in the picking of seismic phases (P- and S-waves) had a broadly normal distribution, mainly concentrated in the ranges of −0.4–0.3 s and −0.4–0.8 s, respectively. These results were compared with those published in the original PhaseNet article and were found to be approximately 0.2–0.4 s larger. PhaseNet had a strong generalizability for P- and S-wave picking for epicentral distances of less than 120 km and 110 km, respectively. However, the phase recall rate decreased rapidly when these distances were exceeded. Furthermore, the generalizability of PhaseNet was essentially unaffected by magnitude. The M4.1 earthquake sequence in Changqing, Shandong province, China, that occurred on February 18, 2020, was adopted as a case study. PhaseNet detected more than twice the number of earthquakes in the manually obtained catalog. This further verified that PhaseNet has strong generalizability in the Shandong region, and a high-precision earthquake catalog was constructed. According to these precise positioning results, two earthquake sequences occurred in the study area, and the southern cluster may have been triggered by the northern cluster. The focal mechanism solution, regional stress field, and the location results of the northern earthquake sequence indicated that the seismic force of the earthquake was consistent with the regional stress field.
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