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Study on crustal deformation of the Ms6. 6 Damxung earthquake in 2008 by InSAR measurements

2010; KeAi; Volume: 1; Issue: 1 Linguagem: Inglês

10.3724/sp.j.1246.2010.00015

2589-0573

Xuejun Qiao, Shanjun Ren, Zhaosheng Nie, Yu Zhou, Qiang Shen, Shaomin Yang,

Earthquake Detection and Analysis

Three Envisat images from ESA were used to derive the pre – and co-seismic deformation interfereograms caused by the Damxung Ms6. 6 earthquake of Oct. 6, 2008, by using InSAR. The result shows no significant crustal motion more than 4 months before the earthquake, but a maximum co-seismic displacement of about 0.3 m in an epicentral area of 20 km × 20 km. The deformation field was symmetrically distributed about a NS axis, where the west side subsided and the east side uplifted. We used a linear elastic dislocation model in half space and a nonlinear constraint optimized algorithm to estimate the slip distribution along the fault. The results indicates that the epicenter is located at 90.374°E, 29.745°N with a moment magnitude of Mw6. 35. The earthquake is dominated by normal faulting with a maximum slip of 3 m on a 12 km × 11 km fault plane striking S189°W, dipping 60° to NW at a depth of 9.5 km, and is located at a sub-fault of the southeastern Piedmont of the Nyainqentanglha mountains. The relatively shallow depth of earthquake is related to relatively high heat flow in the area.