HR: 1340h
AN: S43C-1024 [Abstracts]
TI: Studying the Sequence of the April 17, 2003 Delingha Earthquake ($M_L$=6.7) by Regional Moment Tensor
Inversion
AU: * Jiao, W
EM: wjiao@multimax.com
AF: Multimax Inc., 1441 McCormick Drive, Largo, MD 20774
AU: Qian, R
EM: ryqian@vip.sina.com
AF: Dept. of Geophysical Exploration, China University of Geosciences, 29 Xue Yuan Lu, Beijing, 100083
China
AU: Chan, W
EM: winston@multimax.com
AF: Multimax Inc., 1441 McCormick Drive, Largo, MD 20774
AU: Zeng, X
AF: Dept. of Geophysical Exploration, China University of Geosciences, 29 Xue Yuan Lu, Beijing, 100083
China
AU: Zhang, M
AF: Dept. of Geophysical Exploration, China University of Geosciences, 29 Xue Yuan Lu, Beijing, 100083
China
AB:
On April 17, 2003, a strong earthquake of $M_L$ = 6.7 occurred to the northwest of the Delingha City, Qinghai Province,
northwest China. The epicenter (37$^{\circ}$33_N, 96$^{\circ}$27_E) lies in the Zongwulong Mountain, where the
Dachaidan-Zongwulong Mountain fault (DZMF) zone runs through. In this study, we analyzed the focal mechanism of the main
shock and several strong immediate aftershocks by regional waveform moment tensor inversion. We collected a comprehensive
regional waveform data set that includes the broadband waveforms from the China Digital Seismic Network, the GSN, and a
portable broadband seismic network deployed in the near regional distance to the earthquake at the time. One very broadband
station equipped with the STS-2 seismometer and 24-bit digital data logger was only 80km from the epicenter, which gave
tremendous constraint on the mechanism of the aftershock sequence (Fan and Wallace, 1991; Dreger and Helmberger, 1993). Our
results show the dominance of the high angle thrust faulting striking NWW-NW. The distribution of the fault plane solutions
reflects the turning and/or branching of the DZMF zone in the area, which has been confirmed by the field geological survey.
DE: 7230 Seismicity and seismotectonics
DE: 7215 Earthquake parameters
SC: Seismology [S]
MN: 2004 AGU Fall Meeting