Teleseismic body wave traveltime tomography is used to inverse the three-dimensional seismic velocity structure beneath Shizigou in the western Qaidam basin. The travel time are picked from the continuous observation data on a small seismic array of stations deployed during 2004-2007. The tomographic results obtained indicate that a NW-trending low velocity anomaly just beneath the target region insert northeastwards with a high dip angle. In the north, northeast and east of the low velocity anomaly, some high-velocity anomalies distribute with the same strike and coverage as those of Shizigou anticline. © 2009 Seismological Society of China and Springer-Verlag GmbH.
CITATION STYLE
Xu, X., Ma, Y., Shi, D., Wang, X., & Yin, C. (2009). Application of teleseismic tomography to the study of shallow structure beneath Shizigou in the western Qaidam basin. Earthquake Science, 22(2), 189–195. https://doi.org/10.1007/s11589-009-0189-9
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