Source Parameters of the 2003–2004 Bange Earthquake Sequence, Central Tibet, China, Estimated from InSAR Data

Remote Sensing

Chengsheng Yang¹  Jing Xu²  Qiang Zhao²  Lingyun Ji² 

[1] College of Geology Engineering and Geomatics, Chang’an University, 126 Yanta Rd., Xi’an 710054, China;Second Monitoring and Application Center, China Earthquake Administration, 316 Xiying Rd., Xi’an 710054, China;

关键词: radar interferometry;    satellite geodesy;    earthquake source observations;    deformation;    earthquake sequence;    Bange earthquakes;   

DOI  :  10.3390/rs8060516

来源: DOAJ

【 摘 要 】

A sequence of Ms ≥ 5.0 earthquakes occurred in 2003 and 2004 in Bange County, Tibet, China, all with similar depths and focal mechanisms. However, the source parameters, kinematics and relationships between these earthquakes are poorly known because of their moderately-sized magnitude and the sparse distribution of seismic stations in the region. We utilize interferometric synthetic aperture radar (InSAR) data from the European Space Agency’s Envisat satellite to determine the location, fault geometry and slip distribution of three large events of the sequence that occurred on 7 July 2003 (Ms 6.0), 27 March 2004 (Ms 6.2), and 3 July 2004 (Ms 5.1). The modeling results indicate that the 7 July 2003 event was a normal-faulting event with a right-lateral slip component, the 27 March 2004 earthquake was associated with a normal fault striking northeast–southwest and dipping northwest with a moderately oblique right-lateral slip, and the 3 July 2004 event was caused by a normal fault. A calculation of the static stress changes on the fault planes demonstrates that the third earthquake may have been triggered by the previous ones.

【 授权许可】

Unknown