Rupture process of Jiashi,Xinjiang earthquake(M_S 6.5)of Feb. 24, 2003
Wei Wang
Abstract
Wei Wang
Abstract
The rupture process of Jiashi, Xinjiang earthquake of Feb. 24, 2003 was estimated by the finite fault model using far field broadband P wave records of CDSN and IRIS. The results indicate that the earthquake focus a north-dipped thrust fault with left-lateral strike slip. The fault plane has a strike of 300° and a dip of 28°. The focal depth is 7.5km.The focal mechanism of this earthquake is different from that of the earthquakes occurred in 1997 and 1998, but similar to that of Artux, Xinjiang earthquake of 1996.We proposed that this earthquake was caused by thrust fault due to the northward pushing of Tarim basin and orogeny of Tianshan Mountain.
OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
The rupture process of Jiashi, Xinjiang earthquake of Feb. 24, 2003 was estimated by the finite fault model using far field broadband P wave records of CDSN and IRIS. The results indicate that the earthquake focus a north-dipped thrust fault with left-lateral strike slip. The fault plane has a strike of 300° and a dip of 28°. The focal depth is 7.5km.The focal mechanism of this earthquake is different from that of the earthquakes occurred in 1997 and 1998, but similar to that of Artux, Xinjiang earthquake of 1996.We proposed that this earthquake was caused by thrust fault due to the northward pushing of Tarim basin and orogeny of Tianshan Mountain.
Key concepts: Seismology, Geology, Focal mechanism, Foreshock, Thrust fault, Fault plane, Thrust, Fault (geology)