Abstract
A detail three-dimensional P wave velocity structure of Beijing, Tianjin and Tangshan area (BTT area) was determined by inverting local earthquake data. In total 16 048 P wave first arrival times from 16048 shallow and mid-depth crustal earthquakes, which occurred in and around the BTT area from 1992 to 1999 were used. The first arrival times are recorded by Northern China United Telemetry Seismic Network and Yanqing-Huailai Digital Seismic Network. Hypocentral parameters of 1 132 earthquakes with magnitude M L=1.7–6.2 and the three-dimensional P wave velocity structure were obtained simultaneously. The inversion result reveals the complicated lateral heterogeneity of P wave velocity structure around BTT area. The tomographic images obtained are also found to explain other seismological observations well.
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Foundation item: Climbing Project “Continental Dynamics of East Asia” (95-S-05) from Ministry of Science and Technology, P. R. China.
Contribution No. 03FE1001, Institute of Geophysics, China Seismological Bureau.
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Yu, Xw., Chen, Yt. & Wang, Pd. Three-dimensional P velocity structure in Beijing area. Acta Seimol. Sin. 16, 1–15 (2003). https://doi.org/10.1007/s11589-003-0001-1
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DOI: https://doi.org/10.1007/s11589-003-0001-1
Key words
- tomography
- three-dimensional velocity structure
- seismic activity
- high velocity anomalies
- low velocity anomalies
- lateral heterogeneity